Question: What type of cloud deck is formed when cool air is trapped under warm air?

Answer: Stratus

The dew point is the temperature to which a parcel must be cooled in order to become saturated, and (unless super-saturation occurs) condenses to water. Water vapour normally begins to condense on condensation nuclei such as dust, ice, and salt in order to form clouds. An elevated portion of a frontal zone forces broad areas of lift, which form clouds decks such as altostratus or cirrostratus. <hl> Stratus is a stable cloud deck which tends to form when a cool, stable air mass is trapped underneath a warm air mass. <hl> It can also form due to the lifting of advection fog during breezy conditions.

The dew point is the temperature to which a parcel must be cooled in order to become saturated, and (unless super-saturation occurs) condenses to water. Water vapour normally begins to condense on condensation nuclei such as dust, ice, and salt in order to form clouds. An elevated portion of a frontal zone forces broad areas of lift, which form clouds decks such as altostratus or cirrostratus. <hl> Stratus <hl> is a stable cloud deck which tends to form when a cool, stable air mass is trapped underneath a warm air mass. It can also form due to the lifting of advection fog during breezy conditions.


Question: What are two types of cloud decks that are formed by lift due to frontal zone forces?

The dew point is the temperature to which a parcel must be cooled in order to become saturated, and (unless super-saturation occurs) condenses to water.  Water vapour normally begins to condense on condensation nuclei such as dust, ice, and salt in order to form clouds.  An elevated portion of a frontal zone forces broad areas of lift, which form clouds decks such as altostratus or cirrostratus.  Stratus is a stable cloud deck which tends to form when a cool, stable air mass is trapped underneath a warm air mass.  It can also form due to the lifting of advection fog during breezy conditions.

Answer: altostratus or cirrostratus

The dew point is the temperature to which a parcel must be cooled in order to become saturated, and (unless super-saturation occurs) condenses to water. Water vapour normally begins to condense on condensation nuclei such as dust, ice, and salt in order to form clouds. <hl> An elevated portion of a frontal zone forces broad areas of lift, which form clouds decks such as altostratus or cirrostratus . <hl> Stratus is a stable cloud deck which tends to form when a cool, stable air mass is trapped underneath a warm air mass. It can also form due to the lifting of advection fog during breezy conditions.

The dew point is the temperature to which a parcel must be cooled in order to become saturated, and (unless super-saturation occurs) condenses to water. Water vapour normally begins to condense on condensation nuclei such as dust, ice, and salt in order to form clouds. An elevated portion of a frontal zone forces broad areas of lift, which form clouds decks such as <hl> altostratus or cirrostratus <hl>. Stratus is a stable cloud deck which tends to form when a cool, stable air mass is trapped underneath a warm air mass. It can also form due to the lifting of advection fog during breezy conditions.

An elevated portion of a frontal zone forces broad areas of lift, which form clouds decks such as <hl> altostratus or cirrostratus <hl> .


Question: How many different main mechanisms are there for cooling air?

There are four main mechanisms for cooling the air to its dew point: adiabatic cooling, conductive cooling, radiational cooling, and evaporative cooling. Adiabatic cooling occurs when air rises and expands. The air can rise due to convection, large-scale atmospheric motions, or a physical barrier such as a mountain (orographic lift). Conductive cooling occurs when the air comes into contact with a colder surface, usually by being blown from one surface to another, for example from a liquid water surface to colder land.  Radiational cooling occurs due to the emission of infrared radiation, either by the air or by the surface underneath.  Evaporative cooling occurs when moisture is added to the air through evaporation, which forces the air temperature to cool to its wet-bulb temperature, or until it reaches saturation.

Answer: four

<hl> There are four main mechanisms for cooling the air to its dew point: adiabatic cooling, conductive cooling, radiational cooling, and evaporative cooling. <hl> Adiabatic cooling occurs when air rises and expands. The air can rise due to convection, large-scale atmospheric motions, or a physical barrier such as a mountain (orographic lift). Conductive cooling occurs when the air comes into contact with a colder surface, usually by being blown from one surface to another, for example from a liquid water surface to colder land. Radiational cooling occurs due to the emission of infrared radiation, either by the air or by the surface underneath. Evaporative cooling occurs when moisture is added to the air through evaporation, which forces the air temperature to cool to its wet-bulb temperature, or until it reaches saturation.

There are <hl> four <hl> main mechanisms for cooling the air to its dew point: adiabatic cooling, conductive cooling, radiational cooling, and evaporative cooling. Adiabatic cooling occurs when air rises and expands. The air can rise due to convection, large-scale atmospheric motions, or a physical barrier such as a mountain (orographic lift). Conductive cooling occurs when the air comes into contact with a colder surface, usually by being blown from one surface to another, for example from a liquid water surface to colder land. Radiational cooling occurs due to the emission of infrared radiation, either by the air or by the surface underneath. Evaporative cooling occurs when moisture is added to the air through evaporation, which forces the air temperature to cool to its wet-bulb temperature, or until it reaches saturation.


Question: What type of cooling happens when air rises and expands?

Answer: Adiabatic

There are four main mechanisms for cooling the air to its dew point: adiabatic cooling, conductive cooling, radiational cooling, and evaporative cooling. <hl> Adiabatic cooling occurs when air rises and expands. <hl> The air can rise due to convection, large-scale atmospheric motions, or a physical barrier such as a mountain (orographic lift). Conductive cooling occurs when the air comes into contact with a colder surface, usually by being blown from one surface to another, for example from a liquid water surface to colder land. Radiational cooling occurs due to the emission of infrared radiation, either by the air or by the surface underneath. Evaporative cooling occurs when moisture is added to the air through evaporation, which forces the air temperature to cool to its wet-bulb temperature, or until it reaches saturation.

There are four main mechanisms for cooling the air to its dew point: adiabatic cooling, conductive cooling, radiational cooling, and evaporative cooling. <hl> Adiabatic <hl> cooling occurs when air rises and expands. The air can rise due to convection, large-scale atmospheric motions, or a physical barrier such as a mountain (orographic lift). Conductive cooling occurs when the air comes into contact with a colder surface, usually by being blown from one surface to another, for example from a liquid water surface to colder land. Radiational cooling occurs due to the emission of infrared radiation, either by the air or by the surface underneath. Evaporative cooling occurs when moisture is added to the air through evaporation, which forces the air temperature to cool to its wet-bulb temperature, or until it reaches saturation.


Question: What type of cooling occurs when the air comes into contact with cold surfaces?

Answer: Conductive

There are four main mechanisms for cooling the air to its dew point: adiabatic cooling, conductive cooling, radiational cooling, and evaporative cooling. Adiabatic cooling occurs when air rises and expands. The air can rise due to convection, large-scale atmospheric motions, or a physical barrier such as a mountain (orographic lift). <hl> Conductive cooling occurs when the air comes into contact with a colder surface, usually by being blown from one surface to another, for example from a liquid water surface to colder land. <hl> Radiational cooling occurs due to the emission of infrared radiation, either by the air or by the surface underneath. Evaporative cooling occurs when moisture is added to the air through evaporation, which forces the air temperature to cool to its wet-bulb temperature, or until it reaches saturation.

There are four main mechanisms for cooling the air to its dew point: adiabatic cooling, conductive cooling, radiational cooling, and evaporative cooling. Adiabatic cooling occurs when air rises and expands. The air can rise due to convection, large-scale atmospheric motions, or a physical barrier such as a mountain (orographic lift). <hl> Conductive <hl> cooling occurs when the air comes into contact with a colder surface, usually by being blown from one surface to another, for example from a liquid water surface to colder land. Radiational cooling occurs due to the emission of infrared radiation, either by the air or by the surface underneath. Evaporative cooling occurs when moisture is added to the air through evaporation, which forces the air temperature to cool to its wet-bulb temperature, or until it reaches saturation.


Question: What is it called when cooling happens because of the emission of infrared radiation?

Answer: Radiational

There are four main mechanisms for cooling the air to its dew point: adiabatic cooling, conductive cooling, radiational cooling, and evaporative cooling. Adiabatic cooling occurs when air rises and expands. The air can rise due to convection, large-scale atmospheric motions, or a physical barrier such as a mountain (orographic lift). Conductive cooling occurs when the air comes into contact with a colder surface, usually by being blown from one surface to another, for example from a liquid water surface to colder land. <hl> Radiational cooling occurs due to the emission of infrared radiation, either by the air or by the surface underneath. <hl> Evaporative cooling occurs when moisture is added to the air through evaporation, which forces the air temperature to cool to its wet-bulb temperature, or until it reaches saturation.

There are four main mechanisms for cooling the air to its dew point: adiabatic cooling, conductive cooling, radiational cooling, and evaporative cooling. Adiabatic cooling occurs when air rises and expands. The air can rise due to convection, large-scale atmospheric motions, or a physical barrier such as a mountain (orographic lift). Conductive cooling occurs when the air comes into contact with a colder surface, usually by being blown from one surface to another, for example from a liquid water surface to colder land. <hl> Radiational <hl> cooling occurs due to the emission of infrared radiation, either by the air or by the surface underneath. Evaporative cooling occurs when moisture is added to the air through evaporation, which forces the air temperature to cool to its wet-bulb temperature, or until it reaches saturation.


Question: What kind of cooling happens when moisture is added to the air due to evaporation?

Answer: Evaporative

There are four main mechanisms for cooling the air to its dew point: adiabatic cooling, conductive cooling, radiational cooling, and evaporative cooling. Adiabatic cooling occurs when air rises and expands. The air can rise due to convection, large-scale atmospheric motions, or a physical barrier such as a mountain (orographic lift). Conductive cooling occurs when the air comes into contact with a colder surface, usually by being blown from one surface to another, for example from a liquid water surface to colder land. Radiational cooling occurs due to the emission of infrared radiation, either by the air or by the surface underneath. <hl> Evaporative cooling occurs when moisture is added to the air through evaporation, which forces the air temperature to cool to its wet-bulb temperature, or until it reaches saturation. <hl>

There are four main mechanisms for cooling the air to its dew point: adiabatic cooling, conductive cooling, radiational cooling, and evaporative cooling. Adiabatic cooling occurs when air rises and expands. The air can rise due to convection, large-scale atmospheric motions, or a physical barrier such as a mountain (orographic lift). Conductive cooling occurs when the air comes into contact with a colder surface, usually by being blown from one surface to another, for example from a liquid water surface to colder land. Radiational cooling occurs due to the emission of infrared radiation, either by the air or by the surface underneath. <hl> Evaporative <hl> cooling occurs when moisture is added to the air through evaporation, which forces the air temperature to cool to its wet-bulb temperature, or until it reaches saturation.


Question: What happens when droplets of water fuse and become larger or when they freeze?

Coalescence occurs when water droplets fuse to create larger water droplets, or when water droplets freeze onto an ice crystal, which is known as the Bergeron process. The fall rate of very small droplets is negligible, hence clouds do not fall out of the sky; precipitation will only occur when these coalesce into larger drops.  When air turbulence occurs, water droplets collide, producing larger droplets. As these larger water droplets descend, coalescence continues, so that drops become heavy enough to overcome air resistance and fall as rain.

Answer: Coalescence

<hl> Coalescence occurs when water droplets fuse to create larger water droplets, or when water droplets freeze onto an ice crystal, which is known as the Bergeron process. <hl> The fall rate of very small droplets is negligible, hence clouds do not fall out of the sky; precipitation will only occur when these coalesce into larger drops. When air turbulence occurs, water droplets collide, producing larger droplets. As these larger water droplets descend, coalescence continues, so that drops become heavy enough to overcome air resistance and fall as rain.

<hl> Coalescence <hl> occurs when water droplets fuse to create larger water droplets, or when water droplets freeze onto an ice crystal, which is known as the Bergeron process. The fall rate of very small droplets is negligible, hence clouds do not fall out of the sky; precipitation will only occur when these coalesce into larger drops. When air turbulence occurs, water droplets collide, producing larger droplets. As these larger water droplets descend, coalescence continues, so that drops become heavy enough to overcome air resistance and fall as rain.


Question: When droplets freeze and form ice crystal what is that called?

Answer: Bergeron process

<hl> Coalescence occurs when water droplets fuse to create larger water droplets, or when water droplets freeze onto an ice crystal, which is known as the Bergeron process . <hl> The fall rate of very small droplets is negligible, hence clouds do not fall out of the sky; precipitation will only occur when these coalesce into larger drops. When air turbulence occurs, water droplets collide, producing larger droplets. As these larger water droplets descend, coalescence continues, so that drops become heavy enough to overcome air resistance and fall as rain.

Coalescence occurs when water droplets fuse to create larger water droplets, or when water droplets freeze onto an ice crystal, which is known as the <hl> Bergeron process <hl>. The fall rate of very small droplets is negligible, hence clouds do not fall out of the sky; precipitation will only occur when these coalesce into larger drops. When air turbulence occurs, water droplets collide, producing larger droplets. As these larger water droplets descend, coalescence continues, so that drops become heavy enough to overcome air resistance and fall as rain.

Coalescence occurs when water droplets fuse to create larger water droplets, or when water droplets freeze onto an ice crystal, which is known as the <hl> Bergeron process <hl> .


Question: What happens when air turbulence causes droplets to collide?

Answer: producing larger droplets

Coalescence occurs when water droplets fuse to create larger water droplets, or when water droplets freeze onto an ice crystal, which is known as the Bergeron process. The fall rate of very small droplets is negligible, hence clouds do not fall out of the sky; precipitation will only occur when these coalesce into larger drops. <hl> When air turbulence occurs, water droplets collide, producing larger droplets . <hl> As these larger water droplets descend, coalescence continues, so that drops become heavy enough to overcome air resistance and fall as rain.

Coalescence occurs when water droplets fuse to create larger water droplets, or when water droplets freeze onto an ice crystal, which is known as the Bergeron process. The fall rate of very small droplets is negligible, hence clouds do not fall out of the sky; precipitation will only occur when these coalesce into larger drops. When air turbulence occurs, water droplets collide, <hl> producing larger droplets <hl>. As these larger water droplets descend, coalescence continues, so that drops become heavy enough to overcome air resistance and fall as rain.

When air turbulence occurs, water droplets collide, <hl> producing larger droplets <hl> .


Question: When coalescence continues and drops become heavy enough to overcome air resistance?

Answer: rain

Coalescence occurs when water droplets fuse to create larger water droplets, or when water droplets freeze onto an ice crystal, which is known as the Bergeron process. The fall rate of very small droplets is negligible, hence clouds do not fall out of the sky; precipitation will only occur when these coalesce into larger drops. When air turbulence occurs, water droplets collide, producing larger droplets. <hl> As these larger water droplets descend, coalescence continues, so that drops become heavy enough to overcome air resistance and fall as rain . <hl>

Coalescence occurs when water droplets fuse to create larger water droplets, or when water droplets freeze onto an ice crystal, which is known as the Bergeron process. The fall rate of very small droplets is negligible, hence clouds do not fall out of the sky; precipitation will only occur when these coalesce into larger drops. When air turbulence occurs, water droplets collide, producing larger droplets. As these larger water droplets descend, coalescence continues, so that drops become heavy enough to overcome air resistance and fall as <hl> rain <hl>.

As these larger water droplets descend, coalescence continues, so that drops become heavy enough to overcome air resistance and fall as <hl> rain <hl> .


Question: How large is the fall rate of very small water droplets?

Answer: negligible

Coalescence occurs when water droplets fuse to create larger water droplets, or when water droplets freeze onto an ice crystal, which is known as the Bergeron process. <hl> The fall rate of very small droplets is negligible , hence clouds do not fall out of the sky; precipitation will only occur when these coalesce into larger drops. <hl> When air turbulence occurs, water droplets collide, producing larger droplets. As these larger water droplets descend, coalescence continues, so that drops become heavy enough to overcome air resistance and fall as rain.

Coalescence occurs when water droplets fuse to create larger water droplets, or when water droplets freeze onto an ice crystal, which is known as the Bergeron process. The fall rate of very small droplets is <hl> negligible <hl>, hence clouds do not fall out of the sky; precipitation will only occur when these coalesce into larger drops. When air turbulence occurs, water droplets collide, producing larger droplets. As these larger water droplets descend, coalescence continues, so that drops become heavy enough to overcome air resistance and fall as rain.

The fall rate of very small droplets is <hl> negligible <hl> , hence clouds do not fall out of the sky; precipitation will only occur when these coalesce into larger drops.


Question: What size are raindrops?

Raindrops have sizes ranging from 0.1 millimetres (0.0039 in) to 9 millimetres (0.35 in) mean diameter, above which they tend to break up. Smaller drops are called cloud droplets, and their shape is spherical. As a raindrop increases in size, its shape becomes more oblate, with its largest cross-section facing the oncoming airflow. Contrary to the cartoon pictures of raindrops, their shape does not resemble a teardrop. Intensity and duration of rainfall are usually inversely related, i.e., high intensity storms are likely to be of short duration and low intensity storms can have a long duration.  Rain drops associated with melting hail tend to be larger than other rain drops.  The METAR code for rain is RA, while the coding for rain showers is SHRA.

Answer: 0.1 millimetres (0.0039 in) to 9 millimetres

<hl> Raindrops have sizes ranging from 0.1 millimetres (0.0039 in) to 9 millimetres (0.35 in) mean diameter, above which they tend to break up. <hl> Smaller drops are called cloud droplets, and their shape is spherical. As a raindrop increases in size, its shape becomes more oblate, with its largest cross-section facing the oncoming airflow. Contrary to the cartoon pictures of raindrops, their shape does not resemble a teardrop. Intensity and duration of rainfall are usually inversely related, i.e., high intensity storms are likely to be of short duration and low intensity storms can have a long duration. Rain drops associated with melting hail tend to be larger than other rain drops. The METAR code for rain is RA, while the coding for rain showers is SHRA.

Raindrops have sizes ranging from <hl> 0.1 millimetres (0.0039 in) to 9 millimetres <hl> (0.35 in) mean diameter, above which they tend to break up. Smaller drops are called cloud droplets, and their shape is spherical. As a raindrop increases in size, its shape becomes more oblate, with its largest cross-section facing the oncoming airflow. Contrary to the cartoon pictures of raindrops, their shape does not resemble a teardrop. Intensity and duration of rainfall are usually inversely related, i.e., high intensity storms are likely to be of short duration and low intensity storms can have a long duration. Rain drops associated with melting hail tend to be larger than other rain drops. The METAR code for rain is RA, while the coding for rain showers is SHRA.


Question: What happens when drops get larger than 9 millimetres?

Answer: they tend to break up

<hl> Raindrops have sizes ranging from 0.1 millimetres (0.0039 in) to 9 millimetres (0.35 in) mean diameter, above which they tend to break up . <hl> Smaller drops are called cloud droplets, and their shape is spherical. As a raindrop increases in size, its shape becomes more oblate, with its largest cross-section facing the oncoming airflow. Contrary to the cartoon pictures of raindrops, their shape does not resemble a teardrop. Intensity and duration of rainfall are usually inversely related, i.e., high intensity storms are likely to be of short duration and low intensity storms can have a long duration. Rain drops associated with melting hail tend to be larger than other rain drops. The METAR code for rain is RA, while the coding for rain showers is SHRA.

Raindrops have sizes ranging from 0.1 millimetres (0.0039 in) to 9 millimetres (0.35 in) mean diameter, above which <hl> they tend to break up <hl>. Smaller drops are called cloud droplets, and their shape is spherical. As a raindrop increases in size, its shape becomes more oblate, with its largest cross-section facing the oncoming airflow. Contrary to the cartoon pictures of raindrops, their shape does not resemble a teardrop. Intensity and duration of rainfall are usually inversely related, i.e., high intensity storms are likely to be of short duration and low intensity storms can have a long duration. Rain drops associated with melting hail tend to be larger than other rain drops. The METAR code for rain is RA, while the coding for rain showers is SHRA.

Raindrops have sizes ranging from 0.1 millimetres (0.0039 in) to 9 millimetres (0.35 in) mean diameter, above which <hl> they tend to break up <hl> .


Question: What are smaller drop masses called?

Answer: cloud droplets

Raindrops have sizes ranging from 0.1 millimetres (0.0039 in) to 9 millimetres (0.35 in) mean diameter, above which they tend to break up. <hl> Smaller drops are called cloud droplets , and their shape is spherical. <hl> As a raindrop increases in size, its shape becomes more oblate, with its largest cross-section facing the oncoming airflow. Contrary to the cartoon pictures of raindrops, their shape does not resemble a teardrop. Intensity and duration of rainfall are usually inversely related, i.e., high intensity storms are likely to be of short duration and low intensity storms can have a long duration. Rain drops associated with melting hail tend to be larger than other rain drops. The METAR code for rain is RA, while the coding for rain showers is SHRA.

Raindrops have sizes ranging from 0.1 millimetres (0.0039 in) to 9 millimetres (0.35 in) mean diameter, above which they tend to break up. Smaller drops are called <hl> cloud droplets <hl>, and their shape is spherical. As a raindrop increases in size, its shape becomes more oblate, with its largest cross-section facing the oncoming airflow. Contrary to the cartoon pictures of raindrops, their shape does not resemble a teardrop. Intensity and duration of rainfall are usually inversely related, i.e., high intensity storms are likely to be of short duration and low intensity storms can have a long duration. Rain drops associated with melting hail tend to be larger than other rain drops. The METAR code for rain is RA, while the coding for rain showers is SHRA.

Smaller drops are called <hl> cloud droplets <hl> , and their shape is spherical.


Question: When the size of raindrops enlarge what shape do they take?

Answer: more oblate

Raindrops have sizes ranging from 0.1 millimetres (0.0039 in) to 9 millimetres (0.35 in) mean diameter, above which they tend to break up. Smaller drops are called cloud droplets, and their shape is spherical. <hl> As a raindrop increases in size, its shape becomes more oblate , with its largest cross-section facing the oncoming airflow. <hl> Contrary to the cartoon pictures of raindrops, their shape does not resemble a teardrop. Intensity and duration of rainfall are usually inversely related, i.e., high intensity storms are likely to be of short duration and low intensity storms can have a long duration. Rain drops associated with melting hail tend to be larger than other rain drops. The METAR code for rain is RA, while the coding for rain showers is SHRA.

Raindrops have sizes ranging from 0.1 millimetres (0.0039 in) to 9 millimetres (0.35 in) mean diameter, above which they tend to break up. Smaller drops are called cloud droplets, and their shape is spherical. As a raindrop increases in size, its shape becomes <hl> more oblate <hl>, with its largest cross-section facing the oncoming airflow. Contrary to the cartoon pictures of raindrops, their shape does not resemble a teardrop. Intensity and duration of rainfall are usually inversely related, i.e., high intensity storms are likely to be of short duration and low intensity storms can have a long duration. Rain drops associated with melting hail tend to be larger than other rain drops. The METAR code for rain is RA, while the coding for rain showers is SHRA.

As a raindrop increases in size, its shape becomes <hl> more oblate <hl> , with its largest cross-section facing the oncoming airflow.


Question: Of what size are raindrops associated with melting hail?

Answer: larger

Raindrops have sizes ranging from 0.1 millimetres (0.0039 in) to 9 millimetres (0.35 in) mean diameter, above which they tend to break up. Smaller drops are called cloud droplets, and their shape is spherical. As a raindrop increases in size, its shape becomes more oblate, with its largest cross-section facing the oncoming airflow. Contrary to the cartoon pictures of raindrops, their shape does not resemble a teardrop. Intensity and duration of rainfall are usually inversely related, i.e., high intensity storms are likely to be of short duration and low intensity storms can have a long duration. <hl> Rain drops associated with melting hail tend to be larger than other rain drops. <hl> The METAR code for rain is RA, while the coding for rain showers is SHRA.

Raindrops have sizes ranging from 0.1 millimetres (0.0039 in) to 9 millimetres (0.35 in) mean diameter, above which they tend to break up. Smaller drops are called cloud droplets, and their shape is spherical. As a raindrop increases in size, its shape becomes more oblate, with its largest cross-section facing the oncoming airflow. Contrary to the cartoon pictures of raindrops, their shape does not resemble a teardrop. Intensity and duration of rainfall are usually inversely related, i.e., high intensity storms are likely to be of short duration and low intensity storms can have a long duration. Rain drops associated with melting hail tend to be <hl> larger <hl> than other rain drops. The METAR code for rain is RA, while the coding for rain showers is SHRA.


Question: What forms when a layer of above freezing air is sandwiched between layers of sub-freezing air?

Ice pellets form when a layer of above-freezing air exists with sub-freezing air both above and below.  This causes the partial or complete melting of any snowflakes falling through the warm layer.  As they fall back into the sub-freezing layer closer to the surface, they re-freeze into ice pellets.  However, if the sub-freezing layer beneath the warm layer is too small, the precipitation will not have time to re-freeze, and freezing rain will be the result at the surface.  A temperature profile showing a warm layer above the ground is most likely to be found in advance of a warm front during the cold season, but can occasionally be found behind a passing cold front.

Answer: Ice pellets

<hl> Ice pellets form when a layer of above-freezing air exists with sub-freezing air both above and below. <hl> This causes the partial or complete melting of any snowflakes falling through the warm layer. As they fall back into the sub-freezing layer closer to the surface, they re-freeze into ice pellets. However, if the sub-freezing layer beneath the warm layer is too small, the precipitation will not have time to re-freeze, and freezing rain will be the result at the surface. A temperature profile showing a warm layer above the ground is most likely to be found in advance of a warm front during the cold season, but can occasionally be found behind a passing cold front.

<hl> Ice pellets <hl> form when a layer of above-freezing air exists with sub-freezing air both above and below. This causes the partial or complete melting of any snowflakes falling through the warm layer. As they fall back into the sub-freezing layer closer to the surface, they re-freeze into ice pellets. However, if the sub-freezing layer beneath the warm layer is too small, the precipitation will not have time to re-freeze, and freezing rain will be the result at the surface. A temperature profile showing a warm layer above the ground is most likely to be found in advance of a warm front during the cold season, but can occasionally be found behind a passing cold front.


Question: what happens if sub freezing air is layered too thinly below falling precipitation doesn't give time to refreeze?

Answer: freezing rain

Ice pellets form when a layer of above-freezing air exists with sub-freezing air both above and below. This causes the partial or complete melting of any snowflakes falling through the warm layer. As they fall back into the sub-freezing layer closer to the surface, they re-freeze into ice pellets. <hl> However, if the sub-freezing layer beneath the warm layer is too small, the precipitation will not have time to re-freeze, and freezing rain will be the result at the surface. <hl> A temperature profile showing a warm layer above the ground is most likely to be found in advance of a warm front during the cold season, but can occasionally be found behind a passing cold front.

Ice pellets form when a layer of above-freezing air exists with sub-freezing air both above and below. This causes the partial or complete melting of any snowflakes falling through the warm layer. As they fall back into the sub-freezing layer closer to the surface, they re-freeze into ice pellets. However, if the sub-freezing layer beneath the warm layer is too small, the precipitation will not have time to re-freeze, and <hl> freezing rain <hl> will be the result at the surface. A temperature profile showing a warm layer above the ground is most likely to be found in advance of a warm front during the cold season, but can occasionally be found behind a passing cold front.


Question: What happens when snowflakes fall through a warm air layer?

Answer: partial or complete melting

Ice pellets form when a layer of above-freezing air exists with sub-freezing air both above and below. <hl> This causes the partial or complete melting of any snowflakes falling through the warm layer. <hl> As they fall back into the sub-freezing layer closer to the surface, they re-freeze into ice pellets. However, if the sub-freezing layer beneath the warm layer is too small, the precipitation will not have time to re-freeze, and freezing rain will be the result at the surface. A temperature profile showing a warm layer above the ground is most likely to be found in advance of a warm front during the cold season, but can occasionally be found behind a passing cold front.

Ice pellets form when a layer of above-freezing air exists with sub-freezing air both above and below. This causes the <hl> partial or complete melting <hl> of any snowflakes falling through the warm layer. As they fall back into the sub-freezing layer closer to the surface, they re-freeze into ice pellets. However, if the sub-freezing layer beneath the warm layer is too small, the precipitation will not have time to re-freeze, and freezing rain will be the result at the surface. A temperature profile showing a warm layer above the ground is most likely to be found in advance of a warm front during the cold season, but can occasionally be found behind a passing cold front.


Question: What is most likely to be found in advance of a warm front during a cold season?

Answer: a warm layer

Ice pellets form when a layer of above-freezing air exists with sub-freezing air both above and below. This causes the partial or complete melting of any snowflakes falling through the warm layer. As they fall back into the sub-freezing layer closer to the surface, they re-freeze into ice pellets. However, if the sub-freezing layer beneath the warm layer is too small, the precipitation will not have time to re-freeze, and freezing rain will be the result at the surface. <hl> A temperature profile showing a warm layer above the ground is most likely to be found in advance of a warm front during the cold season, but can occasionally be found behind a passing cold front. <hl>

Ice pellets form when a layer of above-freezing air exists with sub-freezing air both above and below. This causes the partial or complete melting of any snowflakes falling through the warm layer. As they fall back into the sub-freezing layer closer to the surface, they re-freeze into ice pellets. However, if the sub-freezing layer beneath the warm layer is too small, the precipitation will not have time to re-freeze, and freezing rain will be the result at the surface. A temperature profile showing <hl> a warm layer <hl> above the ground is most likely to be found in advance of a warm front during the cold season, but can occasionally be found behind a passing cold front.


Question: What happens when snowflakes fall through a warm layer of air?

Answer: partial or complete melting

Ice pellets form when a layer of above-freezing air exists with sub-freezing air both above and below. <hl> This causes the partial or complete melting of any snowflakes falling through the warm layer. <hl> As they fall back into the sub-freezing layer closer to the surface, they re-freeze into ice pellets. However, if the sub-freezing layer beneath the warm layer is too small, the precipitation will not have time to re-freeze, and freezing rain will be the result at the surface. A temperature profile showing a warm layer above the ground is most likely to be found in advance of a warm front during the cold season, but can occasionally be found behind a passing cold front.

Ice pellets form when a layer of above-freezing air exists with sub-freezing air both above and below. This causes the <hl> partial or complete melting <hl> of any snowflakes falling through the warm layer. As they fall back into the sub-freezing layer closer to the surface, they re-freeze into ice pellets. However, if the sub-freezing layer beneath the warm layer is too small, the precipitation will not have time to re-freeze, and freezing rain will be the result at the surface. A temperature profile showing a warm layer above the ground is most likely to be found in advance of a warm front during the cold season, but can occasionally be found behind a passing cold front.


Question: What forms in clouds when supercooled water droplets freeze on contact with condensation nuclei (Like dust/dirt)?

Like other precipitation, hail forms in storm clouds when supercooled water droplets freeze on contact with condensation nuclei, such as dust or dirt.  The storm's updraft blows the hailstones to the upper part of the cloud.  The updraft dissipates and the hailstones fall down, back into the updraft, and are lifted again.  Hail has a diameter of 5 millimetres (0.20 in) or more.  Within METAR code, GR is used to indicate larger hail, of a diameter of at least 6.4 millimetres (0.25 in).  GR is derived from the French word grêle.  Smaller-sized hail, as well as snow pellets, use the coding of GS, which is short for the French word grésil.  Stones just larger than golf ball-sized are one of the most frequently reported hail sizes.  Hailstones can grow to 15 centimetres (6 in) and weigh more than 500 grams (1 lb).  In large hailstones, latent heat released by further freezing may melt the outer shell of the hailstone.  The hailstone then may undergo 'wet growth', where the liquid outer shell collects other smaller hailstones.  The hailstone gains an ice layer and grows increasingly larger with each ascent. Once a hailstone becomes too heavy to be supported by the storm's updraft, it falls from the cloud.

Answer: hail

<hl> Like other precipitation, hail forms in storm clouds when supercooled water droplets freeze on contact with condensation nuclei, such as dust or dirt. <hl> The storm's updraft blows the hailstones to the upper part of the cloud. The updraft dissipates and the hailstones fall down, back into the updraft, and are lifted again. Hail has a diameter of 5 millimetres (0.20 in) or more. Within METAR code, GR is used to indicate larger hail, of a diameter of at least 6.4 millimetres (0.25 in). GR is derived from the French word grêle. Smaller-sized hail, as well as snow pellets, use the coding of GS, which is short for the French word grésil. Stones just larger than golf ball-sized are one of the most frequently reported hail sizes. Hailstones can grow to 15 centimetres (6 in) and weigh more than 500 grams (1 lb). In large hailstones, latent heat released by further freezing may melt the outer shell of the hailstone. The hailstone then may undergo 'wet growth', where the liquid outer shell collects other smaller hailstones. The hailstone gains an ice layer and grows increasingly larger with each ascent. Once a hailstone becomes too heavy to be supported by the storm's updraft, it falls from the cloud.

Like other precipitation, <hl> hail <hl> forms in storm clouds when supercooled water droplets freeze on contact with condensation nuclei, such as dust or dirt. The storm's updraft blows the hailstones to the upper part of the cloud. The updraft dissipates and the hailstones fall down, back into the updraft, and are lifted again. Hail has a diameter of 5 millimetres (0.20 in) or more. Within METAR code, GR is used to indicate larger hail, of a diameter of at least 6.4 millimetres (0.25 in). GR is derived from the French word grêle. Smaller-sized hail, as well as snow pellets, use the coding of GS, which is short for the French word grésil. Stones just larger than golf ball-sized are one of the most frequently reported hail sizes. Hailstones can grow to 15 centimetres (6 in) and weigh more than 500 grams (1 lb). In large hailstones, latent heat released by further freezing may melt the outer shell of the hailstone. The hailstone then may undergo 'wet growth', where the liquid outer shell collects other smaller hailstones. The hailstone gains an ice layer and grows increasingly larger with each ascent. Once a hailstone becomes too heavy to be supported by the storm's updraft, it falls from the cloud.


Question: To which part of a cloud is hail blown into?

Answer: upper part

Like other precipitation, hail forms in storm clouds when supercooled water droplets freeze on contact with condensation nuclei, such as dust or dirt. <hl> The storm's updraft blows the hailstones to the upper part of the cloud. <hl> The updraft dissipates and the hailstones fall down, back into the updraft, and are lifted again. Hail has a diameter of 5 millimetres (0.20 in) or more. Within METAR code, GR is used to indicate larger hail, of a diameter of at least 6.4 millimetres (0.25 in). GR is derived from the French word grêle. Smaller-sized hail, as well as snow pellets, use the coding of GS, which is short for the French word grésil. Stones just larger than golf ball-sized are one of the most frequently reported hail sizes. Hailstones can grow to 15 centimetres (6 in) and weigh more than 500 grams (1 lb). In large hailstones, latent heat released by further freezing may melt the outer shell of the hailstone. The hailstone then may undergo 'wet growth', where the liquid outer shell collects other smaller hailstones. The hailstone gains an ice layer and grows increasingly larger with each ascent. Once a hailstone becomes too heavy to be supported by the storm's updraft, it falls from the cloud.

Like other precipitation, hail forms in storm clouds when supercooled water droplets freeze on contact with condensation nuclei, such as dust or dirt. The storm's updraft blows the hailstones to the <hl> upper part <hl> of the cloud. The updraft dissipates and the hailstones fall down, back into the updraft, and are lifted again. Hail has a diameter of 5 millimetres (0.20 in) or more. Within METAR code, GR is used to indicate larger hail, of a diameter of at least 6.4 millimetres (0.25 in). GR is derived from the French word grêle. Smaller-sized hail, as well as snow pellets, use the coding of GS, which is short for the French word grésil. Stones just larger than golf ball-sized are one of the most frequently reported hail sizes. Hailstones can grow to 15 centimetres (6 in) and weigh more than 500 grams (1 lb). In large hailstones, latent heat released by further freezing may melt the outer shell of the hailstone. The hailstone then may undergo 'wet growth', where the liquid outer shell collects other smaller hailstones. The hailstone gains an ice layer and grows increasingly larger with each ascent. Once a hailstone becomes too heavy to be supported by the storm's updraft, it falls from the cloud.


Question: What is the minimum size of hail?

Answer: 5 millimetres (0.20 in)

Like other precipitation, hail forms in storm clouds when supercooled water droplets freeze on contact with condensation nuclei, such as dust or dirt. The storm's updraft blows the hailstones to the upper part of the cloud. The updraft dissipates and the hailstones fall down, back into the updraft, and are lifted again. <hl> Hail has a diameter of 5 millimetres (0.20 in) or more. <hl> Within METAR code, GR is used to indicate larger hail, of a diameter of at least 6.4 millimetres (0.25 in). GR is derived from the French word grêle. Smaller-sized hail, as well as snow pellets, use the coding of GS, which is short for the French word grésil. Stones just larger than golf ball-sized are one of the most frequently reported hail sizes. Hailstones can grow to 15 centimetres (6 in) and weigh more than 500 grams (1 lb). In large hailstones, latent heat released by further freezing may melt the outer shell of the hailstone. The hailstone then may undergo 'wet growth', where the liquid outer shell collects other smaller hailstones. The hailstone gains an ice layer and grows increasingly larger with each ascent. Once a hailstone becomes too heavy to be supported by the storm's updraft, it falls from the cloud.

Like other precipitation, hail forms in storm clouds when supercooled water droplets freeze on contact with condensation nuclei, such as dust or dirt. The storm's updraft blows the hailstones to the upper part of the cloud. The updraft dissipates and the hailstones fall down, back into the updraft, and are lifted again. Hail has a diameter of <hl> 5 millimetres (0.20 in) <hl> or more. Within METAR code, GR is used to indicate larger hail, of a diameter of at least 6.4 millimetres (0.25 in). GR is derived from the French word grêle. Smaller-sized hail, as well as snow pellets, use the coding of GS, which is short for the French word grésil. Stones just larger than golf ball-sized are one of the most frequently reported hail sizes. Hailstones can grow to 15 centimetres (6 in) and weigh more than 500 grams (1 lb). In large hailstones, latent heat released by further freezing may melt the outer shell of the hailstone. The hailstone then may undergo 'wet growth', where the liquid outer shell collects other smaller hailstones. The hailstone gains an ice layer and grows increasingly larger with each ascent. Once a hailstone becomes too heavy to be supported by the storm's updraft, it falls from the cloud.


Question: From what French word is GR derived?

Answer: grêle

Like other precipitation, hail forms in storm clouds when supercooled water droplets freeze on contact with condensation nuclei, such as dust or dirt. The storm's updraft blows the hailstones to the upper part of the cloud. The updraft dissipates and the hailstones fall down, back into the updraft, and are lifted again. Hail has a diameter of 5 millimetres (0.20 in) or more. Within METAR code, GR is used to indicate larger hail, of a diameter of at least 6.4 millimetres (0.25 in). <hl> GR is derived from the French word grêle . <hl> Smaller-sized hail, as well as snow pellets, use the coding of GS, which is short for the French word grésil. Stones just larger than golf ball-sized are one of the most frequently reported hail sizes. Hailstones can grow to 15 centimetres (6 in) and weigh more than 500 grams (1 lb). In large hailstones, latent heat released by further freezing may melt the outer shell of the hailstone. The hailstone then may undergo 'wet growth', where the liquid outer shell collects other smaller hailstones. The hailstone gains an ice layer and grows increasingly larger with each ascent. Once a hailstone becomes too heavy to be supported by the storm's updraft, it falls from the cloud.

Like other precipitation, hail forms in storm clouds when supercooled water droplets freeze on contact with condensation nuclei, such as dust or dirt. The storm's updraft blows the hailstones to the upper part of the cloud. The updraft dissipates and the hailstones fall down, back into the updraft, and are lifted again. Hail has a diameter of 5 millimetres (0.20 in) or more. Within METAR code, GR is used to indicate larger hail, of a diameter of at least 6.4 millimetres (0.25 in). GR is derived from the French word <hl> grêle <hl>. Smaller-sized hail, as well as snow pellets, use the coding of GS, which is short for the French word grésil. Stones just larger than golf ball-sized are one of the most frequently reported hail sizes. Hailstones can grow to 15 centimetres (6 in) and weigh more than 500 grams (1 lb). In large hailstones, latent heat released by further freezing may melt the outer shell of the hailstone. The hailstone then may undergo 'wet growth', where the liquid outer shell collects other smaller hailstones. The hailstone gains an ice layer and grows increasingly larger with each ascent. Once a hailstone becomes too heavy to be supported by the storm's updraft, it falls from the cloud.

GR is derived from the French word <hl> grêle <hl> .


Question: What is it called when hail gets larger as the liquid outer shell of hail collects other smaller hailstones?

Answer: wet growth

Like other precipitation, hail forms in storm clouds when supercooled water droplets freeze on contact with condensation nuclei, such as dust or dirt. The storm's updraft blows the hailstones to the upper part of the cloud. The updraft dissipates and the hailstones fall down, back into the updraft, and are lifted again. Hail has a diameter of 5 millimetres (0.20 in) or more. Within METAR code, GR is used to indicate larger hail, of a diameter of at least 6.4 millimetres (0.25 in). GR is derived from the French word grêle. Smaller-sized hail, as well as snow pellets, use the coding of GS, which is short for the French word grésil. Stones just larger than golf ball-sized are one of the most frequently reported hail sizes. Hailstones can grow to 15 centimetres (6 in) and weigh more than 500 grams (1 lb). In large hailstones, latent heat released by further freezing may melt the outer shell of the hailstone. <hl> The hailstone then may undergo ' wet growth ', where the liquid outer shell collects other smaller hailstones. <hl> The hailstone gains an ice layer and grows increasingly larger with each ascent. Once a hailstone becomes too heavy to be supported by the storm's updraft, it falls from the cloud.

Like other precipitation, hail forms in storm clouds when supercooled water droplets freeze on contact with condensation nuclei, such as dust or dirt. The storm's updraft blows the hailstones to the upper part of the cloud. The updraft dissipates and the hailstones fall down, back into the updraft, and are lifted again. Hail has a diameter of 5 millimetres (0.20 in) or more. Within METAR code, GR is used to indicate larger hail, of a diameter of at least 6.4 millimetres (0.25 in). GR is derived from the French word grêle. Smaller-sized hail, as well as snow pellets, use the coding of GS, which is short for the French word grésil. Stones just larger than golf ball-sized are one of the most frequently reported hail sizes. Hailstones can grow to 15 centimetres (6 in) and weigh more than 500 grams (1 lb). In large hailstones, latent heat released by further freezing may melt the outer shell of the hailstone. The hailstone then may undergo '<hl> wet growth <hl>', where the liquid outer shell collects other smaller hailstones. The hailstone gains an ice layer and grows increasingly larger with each ascent. Once a hailstone becomes too heavy to be supported by the storm's updraft, it falls from the cloud.

The hailstone then may undergo ' <hl> wet growth <hl> ', where the liquid outer shell collects other smaller hailstones.


Question: When did the British begin sending large quantities of arms to Yugoslavia?

One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ), the Yugoslav wartime deliberative assembly, was to fight the occupying forces. Until British supplies began to arrive in appreciable quantities in 1944, the occupiers were the only source of arms. The other objective was to create a federal multi-ethnic communist state in Yugoslavia. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.

Answer: 1944

One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ), the Yugoslav wartime deliberative assembly, was to fight the occupying forces. <hl> Until British supplies began to arrive in appreciable quantities in 1944 , the occupiers were the only source of arms. <hl> The other objective was to create a federal multi-ethnic communist state in Yugoslavia. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.

One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ), the Yugoslav wartime deliberative assembly, was to fight the occupying forces. Until British supplies began to arrive in appreciable quantities in <hl> 1944 <hl>, the occupiers were the only source of arms. The other objective was to create a federal multi-ethnic communist state in Yugoslavia. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.

Until British supplies began to arrive in appreciable quantities in <hl> 1944 <hl> , the occupiers were the only source of arms.


Question: What organization took on the role of Yugoslav wartime deliberative assembly?

Answer: Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ)

<hl> One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ) , the Yugoslav wartime deliberative assembly, was to fight the occupying forces. <hl> Until British supplies began to arrive in appreciable quantities in 1944, the occupiers were the only source of arms. The other objective was to create a federal multi-ethnic communist state in Yugoslavia. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.

One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the <hl> Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ) <hl>, the Yugoslav wartime deliberative assembly, was to fight the occupying forces. Until British supplies began to arrive in appreciable quantities in 1944, the occupiers were the only source of arms. The other objective was to create a federal multi-ethnic communist state in Yugoslavia. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.

One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the <hl> Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ) <hl> , the Yugoslav wartime deliberative assembly, was to fight the occupying forces.


Question: Who led the UNOF coalition?

Answer: Communist Party of Yugoslavia (KPJ)

<hl> One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ), the Yugoslav wartime deliberative assembly, was to fight the occupying forces. <hl> Until British supplies began to arrive in appreciable quantities in 1944, the occupiers were the only source of arms. The other objective was to create a federal multi-ethnic communist state in Yugoslavia. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.

One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the <hl> Communist Party of Yugoslavia (KPJ) <hl> and represented by the Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ), the Yugoslav wartime deliberative assembly, was to fight the occupying forces. Until British supplies began to arrive in appreciable quantities in 1944, the occupiers were the only source of arms. The other objective was to create a federal multi-ethnic communist state in Yugoslavia. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.


Question: Besides fighting occupying forces, what was the other objective of the UNOF coalition?

Answer: to create a federal multi-ethnic communist state in Yugoslavia

One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ), the Yugoslav wartime deliberative assembly, was to fight the occupying forces. Until British supplies began to arrive in appreciable quantities in 1944, the occupiers were the only source of arms. <hl> The other objective was to create a federal multi-ethnic communist state in Yugoslavia . <hl> To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.

One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ), the Yugoslav wartime deliberative assembly, was to fight the occupying forces. Until British supplies began to arrive in appreciable quantities in 1944, the occupiers were the only source of arms. The other objective was <hl> to create a federal multi-ethnic communist state in Yugoslavia <hl>. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.

The other objective was <hl> to create a federal multi-ethnic communist state in Yugoslavia <hl> .


Question: What does KPJ stand for within the context of Yugoslavia?

Answer: Communist Party of Yugoslavia

<hl> One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ), the Yugoslav wartime deliberative assembly, was to fight the occupying forces. <hl> Until British supplies began to arrive in appreciable quantities in 1944, the occupiers were the only source of arms. The other objective was to create a federal multi-ethnic communist state in Yugoslavia. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.

One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the <hl> Communist Party of Yugoslavia <hl> (KPJ) and represented by the Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ), the Yugoslav wartime deliberative assembly, was to fight the occupying forces. Until British supplies began to arrive in appreciable quantities in 1944, the occupiers were the only source of arms. The other objective was to create a federal multi-ethnic communist state in Yugoslavia. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.


Question: What was the movement that the Partisans were part of, on the military side?

Answer: Unitary National Liberation Front (UNOF)

<hl> One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ), the Yugoslav wartime deliberative assembly, was to fight the occupying forces. <hl> Until British supplies began to arrive in appreciable quantities in 1944, the occupiers were the only source of arms. The other objective was to create a federal multi-ethnic communist state in Yugoslavia. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.

One of two objectives of the movement, which was the military arm of the <hl> Unitary National Liberation Front (UNOF) <hl> coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ), the Yugoslav wartime deliberative assembly, was to fight the occupying forces. Until British supplies began to arrive in appreciable quantities in 1944, the occupiers were the only source of arms. The other objective was to create a federal multi-ethnic communist state in Yugoslavia. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.


Question: Who was in charge of the UNOF?

Answer: Communist Party of Yugoslavia (KPJ)

<hl> One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ), the Yugoslav wartime deliberative assembly, was to fight the occupying forces. <hl> Until British supplies began to arrive in appreciable quantities in 1944, the occupiers were the only source of arms. The other objective was to create a federal multi-ethnic communist state in Yugoslavia. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.

One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the <hl> Communist Party of Yugoslavia (KPJ) <hl> and represented by the Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ), the Yugoslav wartime deliberative assembly, was to fight the occupying forces. Until British supplies began to arrive in appreciable quantities in 1944, the occupiers were the only source of arms. The other objective was to create a federal multi-ethnic communist state in Yugoslavia. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.


Question: What was the name of the Yugoslav wartime deliberative assembly?

Answer: Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ)

<hl> One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ) , the Yugoslav wartime deliberative assembly, was to fight the occupying forces. <hl> Until British supplies began to arrive in appreciable quantities in 1944, the occupiers were the only source of arms. The other objective was to create a federal multi-ethnic communist state in Yugoslavia. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.

One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the <hl> Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ) <hl>, the Yugoslav wartime deliberative assembly, was to fight the occupying forces. Until British supplies began to arrive in appreciable quantities in 1944, the occupiers were the only source of arms. The other objective was to create a federal multi-ethnic communist state in Yugoslavia. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.

One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the <hl> Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ) <hl> , the Yugoslav wartime deliberative assembly, was to fight the occupying forces.


Question: When did British supplies start to arrive to help the AVNNOJ?

Answer: 1944

One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ), the Yugoslav wartime deliberative assembly, was to fight the occupying forces. <hl> Until British supplies began to arrive in appreciable quantities in 1944 , the occupiers were the only source of arms. <hl> The other objective was to create a federal multi-ethnic communist state in Yugoslavia. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.

One of two objectives of the movement, which was the military arm of the Unitary National Liberation Front (UNOF) coalition, led by the Communist Party of Yugoslavia (KPJ) and represented by the Anti-Fascist Council for the National Liberation of Yugoslavia (AVNNOJ), the Yugoslav wartime deliberative assembly, was to fight the occupying forces. Until British supplies began to arrive in appreciable quantities in <hl> 1944 <hl>, the occupiers were the only source of arms. The other objective was to create a federal multi-ethnic communist state in Yugoslavia. To this end, the KPJ attempted to appeal to all the various ethnic groups within Yugoslavia, by preserving the rights of each group.

Until British supplies began to arrive in appreciable quantities in <hl> 1944 <hl> , the occupiers were the only source of arms.


Question: What group wanted to perform an ethnic cleansing of non-Serbs from what they considered to be Serbian territories?

The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

Answer: Chetniks

<hl> The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks , were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. <hl> Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

The objectives of the rival resistance movement which emerged some weeks earlier, the <hl> Chetniks <hl>, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

The objectives of the rival resistance movement which emerged some weeks earlier, the <hl> Chetniks <hl> , were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian.


Question: Where did the April 1942 murders of Muslim women and children occur?

Answer: Herzegovina

The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. <hl> In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina ). <hl> In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in <hl> Herzegovina <hl>). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in <hl> Herzegovina <hl> ).


Question: What group of people were persecuted by the Partisan forces?

Answer: Muslims

The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. <hl> In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). <hl> In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of <hl> Muslims <hl> (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.


Question: What month and year marked the start of the conflict between the Chetnik's and the Partisan forces?

Answer: October 1941

The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. <hl> Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. <hl> To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. Relations between the two movements were uneasy from the start, but from <hl> October 1941 <hl> they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.


Question: What was the name of the group working to preserve the Yugoslav monarchy?

Answer: Chetniks

<hl> The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks , were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. <hl> Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

The objectives of the rival resistance movement which emerged some weeks earlier, the <hl> Chetniks <hl>, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

The objectives of the rival resistance movement which emerged some weeks earlier, the <hl> Chetniks <hl> , were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian.


Question: Which group thought that Tito's pan-ethnic policies were anti-Serbian?

Answer: Chetniks

<hl> The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks , were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. <hl> Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

The objectives of the rival resistance movement which emerged some weeks earlier, the <hl> Chetniks <hl>, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

The objectives of the rival resistance movement which emerged some weeks earlier, the <hl> Chetniks <hl> , were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian.


Question: Which group had their Muslim and Croat commanders' names changed to protect them?

Answer: Partisan forces

The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. <hl> In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). <hl> In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war <hl> Partisan forces <hl> were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.


Question: When did the full-scale war start between the Chetniks and Partisan groups?

Answer: October 1941

The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. <hl> Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. <hl> To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. Relations between the two movements were uneasy from the start, but from <hl> October 1941 <hl> they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.


Question: What was the name of the group working to preserve the Yugoslav monarchy?

Answer: Chetniks

<hl> The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks , were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. <hl> Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

The objectives of the rival resistance movement which emerged some weeks earlier, the <hl> Chetniks <hl>, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

The objectives of the rival resistance movement which emerged some weeks earlier, the <hl> Chetniks <hl> , were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian.


Question: When did the full-scale war start between the Chetniks and Partisan groups?

Answer: October 1941

The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. <hl> Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. <hl> To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. Relations between the two movements were uneasy from the start, but from <hl> October 1941 <hl> they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.


Question: Which group thought that Tito's pan-ethnic policies were anti-Serbian?

Answer: Chetniks

<hl> The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks , were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. <hl> Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

The objectives of the rival resistance movement which emerged some weeks earlier, the <hl> Chetniks <hl>, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

The objectives of the rival resistance movement which emerged some weeks earlier, the <hl> Chetniks <hl> , were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian.


Question: Which group had their Muslim and Croat commanders' names changed to protect them?

Answer: Partisan forces

The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. <hl> In the early part of the war Partisan forces were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). <hl> In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.

The objectives of the rival resistance movement which emerged some weeks earlier, the Chetniks, were the retention of the Yugoslav monarchy, ensuring the safety of ethnic Serbian populations, and the establishment of a Greater Serbia through the ethnic cleansing of non-Serbs from territories they considered rightfully and historically Serbian. Relations between the two movements were uneasy from the start, but from October 1941 they degenerated into full-scale conflict. To the Chetniks, Tito's pan-ethnic policies seemed anti-Serbian, whereas the Chetniks' royalism was anathema to the communists. In the early part of the war <hl> Partisan forces <hl> were predominantly composed of Serbs and given to the persecution of Muslims (e.g. the slaughter of Muslim women and children in April 1942 in Herzegovina). In that period names of Muslim and Croat commanders of Partisan forces had to be changed to protect them from their predominantly Serb colleagues.


Question: Who was killed at Gala?

The Chetniks were a mainly Serb-oriented group and their Serb nationalism resulted in an inability to recruit or appeal to many non-Serbs. The Partisans played down communism in favour of a Popular Front approach which appealed to all Yugoslavs. In Bosnia, the Partisan rallying cry was for a country which was to be neither Serbian nor Croatian nor Muslim, but instead to be free and brotherly in which full equality of all groups would be ensured. Nevertheless, Serbs remained the dominant ethnic group in the Yugoslav Partisans throughout the war.  Chetnik ethnic cleansing policies against the Muslims in Eastern Bosnia, and Dalmatia alienated Croats and Muslims from joining the Chetniks. Italian collaboration with Chetniks in northern Dalmatia resulted in atrocities which further galvanized support for the Partisans among Dalmatian Croats. Chetnik attacks on Gala, near Split, resulted in the slaughter of some 200 Croatian civilians.

Answer: 200 Croatian civilians

The Chetniks were a mainly Serb-oriented group and their Serb nationalism resulted in an inability to recruit or appeal to many non-Serbs. The Partisans played down communism in favour of a Popular Front approach which appealed to all Yugoslavs. In Bosnia, the Partisan rallying cry was for a country which was to be neither Serbian nor Croatian nor Muslim, but instead to be free and brotherly in which full equality of all groups would be ensured. Nevertheless, Serbs remained the dominant ethnic group in the Yugoslav Partisans throughout the war. Chetnik ethnic cleansing policies against the Muslims in Eastern Bosnia, and Dalmatia alienated Croats and Muslims from joining the Chetniks. Italian collaboration with Chetniks in northern Dalmatia resulted in atrocities which further galvanized support for the Partisans among Dalmatian Croats. <hl> Chetnik attacks on Gala, near Split, resulted in the slaughter of some 200 Croatian civilians . <hl>

The Chetniks were a mainly Serb-oriented group and their Serb nationalism resulted in an inability to recruit or appeal to many non-Serbs. The Partisans played down communism in favour of a Popular Front approach which appealed to all Yugoslavs. In Bosnia, the Partisan rallying cry was for a country which was to be neither Serbian nor Croatian nor Muslim, but instead to be free and brotherly in which full equality of all groups would be ensured. Nevertheless, Serbs remained the dominant ethnic group in the Yugoslav Partisans throughout the war. Chetnik ethnic cleansing policies against the Muslims in Eastern Bosnia, and Dalmatia alienated Croats and Muslims from joining the Chetniks. Italian collaboration with Chetniks in northern Dalmatia resulted in atrocities which further galvanized support for the Partisans among Dalmatian Croats. Chetnik attacks on Gala, near Split, resulted in the slaughter of some <hl> 200 Croatian civilians <hl>.

Chetnik attacks on Gala, near Split, resulted in the slaughter of some <hl> 200 Croatian civilians <hl> .


Question: What group did the Chetnik seek to ethnically cleanse?

Answer: Muslims

The Chetniks were a mainly Serb-oriented group and their Serb nationalism resulted in an inability to recruit or appeal to many non-Serbs. The Partisans played down communism in favour of a Popular Front approach which appealed to all Yugoslavs. In Bosnia, the Partisan rallying cry was for a country which was to be neither Serbian nor Croatian nor Muslim, but instead to be free and brotherly in which full equality of all groups would be ensured. Nevertheless, Serbs remained the dominant ethnic group in the Yugoslav Partisans throughout the war. <hl> Chetnik ethnic cleansing policies against the Muslims in Eastern Bosnia, and Dalmatia alienated Croats and Muslims from joining the Chetniks. <hl> Italian collaboration with Chetniks in northern Dalmatia resulted in atrocities which further galvanized support for the Partisans among Dalmatian Croats. Chetnik attacks on Gala, near Split, resulted in the slaughter of some 200 Croatian civilians.

The Chetniks were a mainly Serb-oriented group and their Serb nationalism resulted in an inability to recruit or appeal to many non-Serbs. The Partisans played down communism in favour of a Popular Front approach which appealed to all Yugoslavs. In Bosnia, the Partisan rallying cry was for a country which was to be neither Serbian nor Croatian nor Muslim, but instead to be free and brotherly in which full equality of all groups would be ensured. Nevertheless, Serbs remained the dominant ethnic group in the Yugoslav Partisans throughout the war. Chetnik ethnic cleansing policies against the <hl> Muslims <hl> in Eastern Bosnia, and Dalmatia alienated Croats and Muslims from joining the Chetniks. Italian collaboration with Chetniks in northern Dalmatia resulted in atrocities which further galvanized support for the Partisans among Dalmatian Croats. Chetnik attacks on Gala, near Split, resulted in the slaughter of some 200 Croatian civilians.