Climate of Minnesota
Minnesota has a humid continental climate, with hot summers and cold winters. Minnesota's location in the Upper Midwest allows it to experience some of the widest variety of weather in the United States, with each of the four seasons having its own distinct characteristics. The area near Lake Superior in the Minnesota Arrowhead region experiences weather unique from the rest of the state. The moderating effect of Lake Superior keeps the surrounding area relatively cooler in the summer and warmer in the winter, giving that region a smaller yearly temperature variation. On the Köppen climate classification , much of the southern third of Minnesota—roughly from the Twin Cities region southward—falls in the hot summer zone ("Dfa"), and the northern two-thirds of Minnesota falls in the warm summer zone ("Dfb"). Winter in Minnesota is characterized by cold (below freezing) temperatures. Snow is the main form of winter precipitation, but freezing rain, sleet, and occasionally rain are all possible during the winter months. Common storm systems include Alberta clippers or Panhandle hooks; some of which develop into blizzards. Annual snowfall extremes have ranged from over in the rugged Superior Highlands of the North Shore to as  little as in southern Minnesota. Temperatures as low as have occurred during Minnesota winters. Spring is a time of major transition in Minnesota. Snowstorms are common early in the spring, but by late-spring as temperatures begin to moderate, the state can experience tornado outbreaks, a risk which diminishes but does not cease through the summer and into the autumn. In summer, heat and humidity predominate in the south, while warm and less humid conditions are generally present in the north. These humid conditions initiate thunderstorm activity 30–40 days per year. Summer high temperatures in Minnesota average in the mid-80s  F (30 °C) in the south to the upper-70s F (25 °C) in the north, with temperatures as hot as possible. The growing season in Minnesota varies from 90 days per year in the Iron Range to 160 days in southeastern Minnesota. Tornadoes are possible in Minnesota from March through November, but the peak tornado month is June, followed by July, May, and August. The state averages 27 tornadoes per year. Average annual precipitation across the state ranges from approximately in the southeast to in the northwest. Autumn weather in Minnesota is largely the reverse of spring weather . The jet stream—which tends to weaken in summer—begins to revive, leading to a quicker changing of weather patterns and an increased variability of temperatures. By late October and November, these storm systems become strong enough to form major winter storms. Autumn and spring are the windiest times of the year in Minnesota. General climatology. Because of its location in North America, Minnesota experiences temperature extremes characteristic of a continental climate, with cold winters and mild to hot summers in the south and frigid winters and generally cool summers in the north. Each season has distinctive upper air patterns  which bring different weather conditions with them. The state is nearly from any large body of water (with the exception of Lake Superior), and temperatures and precipitation vary widely. It is far enough north to experience temperatures and blizzards during the winter months, but far enough south to have temperatures and tornado outbreaks in the summer. The variation between Minnesota's highest and lowest temperature is the eleventh largest variation of any U.S. state, and 3rd largest of any state east of the Rocky Mountains behind North Dakota and South Dakota. Minnesota is far from major sources of moisture and  is in the transition zone between the moist East and the semi-arid Great Plains. Annual average precipitation across the state ranges from around in the southeast to in the northwest. Snow is the main form of precipitation from November through March, while rain is the most common the rest of the year. Annual snowfall extremes have ranged from over in the rugged Superior Highlands of the North Shore to as little as in southern Minnesota. It has snowed in Minnesota during every month with the exception of July, and the state averages 110 days per year with snow cover  of an inch (2.5 cm) or greater. Lake Superior. Lake Superior moderates the climate of those parts of Minnesota's Arrowhead Region near the shore. The lake acts as a heat sink, keeping the state's North Shore area relatively cooler in the summer and warmer in the winter. While this effect is marked near the lake, it does not reach very far inland. For example, Grand Marais on the lakeshore has an average July high temperature of , while Virginia, at about the same latitude but inland about to the west, has an average July high of . Virginia's average  high temperature in January is , while Grand Marais’ is . Just a few miles inland from Lake Superior are the Sawtooth Mountains, which almost completely confine the marine air masses and associated precipitation to lower elevations near the lake. The prevailing northwest winter winds also limit the lake's influence. Places near the shoreline can receive lake-effect snow, but because the state lies north and west of the lake, snowfall amounts are not nearly as large as they are in locations like Wisconsin and Michigan that lie downwind to the south. Even so, the single largest snowstorm in Minnesota history  was a lake effect event. On January 6, 1994, Finland, Minnesota, received of lake effect snow in 24 hours, and over a three-day period. Both are Minnesota records. At per year, the port city of Duluth has the highest average snowfall total of any city in Minnesota. At , Grand Marais has the lowest average summer temperature of any city in the state. The climatological effects of Lake Superior tend to stifle convection, thus limiting the potential for tornadoes. Although Cook and Lake counties are two of the largest counties in the state, they have experienced only seven tornadoes in  the past 56 years. One of those tornadoes was a large F3 that occurred in the Tornado outbreak of August 6, 1969. Seasons. Winter. Even though winter does not officially start until late December, Minnesota usually begins experiencing winter-like conditions in November, sometimes in October. As with many other Midwestern states, winter in Minnesota is characterized by cold (below freezing) temperatures and snowfall. Weather systems can move in from the north, west, or south, with the majority of the weather being driven in from the north. A vigorous jet stream brings high and low-pressure systems through in quick  succession, which can cause large temperature variations over a short period of time. Winter temperature. As the last remnants of summertime air in the southern U.S. start to lose their grip, cold polar air building up in northern Canada starts to push farther south, eventually spreading into Minnesota. By the time December and January arrive, Minnesota is fully engulfed in the polar air and is then subjected to outbreaks of arctic air masses. Because there are no natural barriers north or northwest of Minnesota to block arctic air from pouring south, Minnesota gets regular shots of the arctic air through  the winter. High pressure systems which descend south from the Canadian plains behind the fronts bring light winds, clear skies, and bitterly cold temperatures. The northern part of Minnesota gets the brunt of the cold air. International Falls, sometimes called the "Icebox of the nation", has the coldest average annual temperature of any National Weather Service first-order station in the contiguous United States at . Tower, Minnesota, sinks below on an average of seventy-one days per year, while the ten coldest counties in the contiguous US, based on January minimums, are all located in Minnesota. The air mass then  slowly moderates as it moves south into the rest of the state. Alberta clippers alternate with these high-pressure systems, bringing high winds and some snowfall with them. Minnesota occasionally gets breaks from the polar and arctic air when a zonal flow takes hold. This means that the jet stream will move in a west to east motion—rather than north to south—and warmer air from the western United States is pushed into the region. In Minnesota this pattern commonly leads to a prolonged period of above freezing high temperatures that gives Minnesotans a break from the winter freeze . Storms that move into Minnesota from a more westerly direction generally do not bring significant amounts of precipitation with them. This pattern becomes especially common when El Niño is present, as the jet stream is weakened and pushed further north into Canada, therefore arctic air is often blocked from entering Minnesota. The opposite phase, La Niña, amplifies the jet stream, therefore arctic air intrusions become even colder and more prevalent. Winter precipitation. Winter precipitation comes in a few different forms. Snow is the main form of precipitation, but freezing rain, ice, sleet and sometimes even rain are all possible during  the winter months. Larger storm systems, often Panhandle hooks or other storms that occur with a meridional flow, can bring large amounts of snow and even blizzard conditions. Alberta clippers. Alberta clippers are fast-moving areas of low pressure that move through Minnesota during the winter months. Clippers get their name from Alberta, Canada, the province from which they begin their southward track. (Other variations of the same type of storm systems are "Saskatchewan Screamers" or "Manitoba Maulers".) Although clippers often originate over the northern Pacific Ocean, they lose most of their moisture through orographic lift when they collide with  the Canadian Rockies. Because of the limited moisture content and quick movement of the systems, clippers rarely produce more than of snow as they pass through Minnesota. The biggest effects of an Alberta Clipper are what follows them; arctic air, high wind speed, and dangerous wind chills. This often results in severe blowing and drifting snow, and sometimes even blizzard conditions. Alberta Clippers often proceed to become copious lake-effect snow producers on the southern and eastern shores of the Great Lakes. Panhandle hooks. In terms of their characteristics, Panhandle hooks are nearly the opposite of Alberta clippers. Instead of  forming in the north and dropping south, these low pressure systems form in the southwestern United States and then move northeast. They get their name from the location where they usually make their turn to the north; near the panhandles of Oklahoma and Texas. Unlike clippers, these storms usually have a great deal of moisture to work with. As the storms make their turn to the north, they pull in moist air from the nearby Gulf of Mexico and pull it northward toward Minnesota and other parts of the Midwest. As these systems move to the northeast, there will usually  be a heavy band of snow to the northwest of the low pressure center if there is enough cold air present. A wintery mix of precipitation, rain, or sometimes even thunderstorms will then often occur to the south of it. Snowfall of over a foot (30 cm) is not uncommon with a panhandle hook, and because of the high moisture content in these systems the snow is usually wet and heavy. Large panhandle hooks can become powerful enough to draw in arctic air after they pass by the state, leaving bitter cold temperatures and wind chills in their wake. Panhandle  Hooks are responsible for some of the most famous blizzards that have occurred in the Midwest, including the blizzard of November 1940 and the Great Storm of 1975. Spring. Spring is a time of major transition in Minnesota. As winter nears its end, the sun rises higher in the sky and temperatures begin to moderate. As this happens much of the Midwest starts to experience severe thunderstorms and tornadoes. Storm systems that move inland from the Pacific begin to collide with the increasingly warm and moist air from the Gulf of Mexico. In the early part of the spring, Minnesota  is usually not in a geographically favorable position to experience severe weather since the warm air needed for it has not yet pushed that far to the north. Early spring tornado outbreaks do occur occasionally in Minnesota though, as evidenced by the 1998 Comfrey – St. Peter tornado outbreak on March 29, 1998. More often, Minnesota is on the northern (cooler) side of major storm systems in the early spring, which instead results in only rain and possibly snow. Even though the winter snow pack typically starts to melt in southern Minnesota in early March, there is usually still enough cold  air present over Canada to allow for major snow storms in Minnesota until late April. Very heavy (30+ inches) monthly snowfalls can occur in March, such as in 1951 and 1965, and rarely, April, such as in April 2002 when over 20 inches of snow fell at Minneapolis, and April 2013, when heavy snow blanketed Minnesota and Duluth received a record monthly snowfall (for any month) of over 50 inches. Wind. With the exception of areas along the shores of Lake Superior, winds in Minnesota generally prevail from the north and northwest in the winter, and south and southeast  in the summer. On average, autumn and spring are the windiest times of the year in Minnesota. October is the windiest month in northwest Minnesota, while April is the windiest over the rest of the state. Winds generally average between 9 and 11 mph (14 and 18 km/h) across the state, with one major exception. The heaviest winds in the state are found on the Buffalo Ridge, or Coteau des Prairies, a flatiron-shaped area extending from Watertown, South Dakota, diagonally across southwestern Minnesota and into Iowa. Created by two lobes of a glacier parting around a pre-existing  plateau during the (Pleistocene) Ice Age, the Buffalo Ridge is ideal for wind power generation, with average wind speeds of 16.1 mph (26.8 km/h). Floods. Minnesota is prone to flooding in its major rivers by spring snowmelt runoff and ice jams. Spring flooding to some degree occurs almost annually on some Minnesota rivers, but major floods have occurred in 1965, 1969, 1997, 2001, and 2009. The flooding in 1965 was the worst flood in Minnesota history on the Mississippi River, while the flooding in 1997 was the worst in history on the Red River. The Red River flood of  1997 was aided heavily by the 11 blizzards that struck Minnesota that winter. Besides heavy winter and spring snowfall, cold winter temperatures and heavy autumn and spring rains causing sudden run-off surges are also common causes of spring river flooding in Minnesota. Minnesota is also prone to both river flooding and localized flash flooding by extended periods of heavy late-spring and summer rainfall. The Great Flood of 1993 on the Mississippi River was caused by copious amounts of rain that fell after the spring snow melt. The 2007 Midwest flooding, which affected the hilly Driftless area of southeast  Minnesota was the result of a training pattern of storms mixing warm moist air from Tropical Storm Erin with cooler Canadian air, resulting in record 24-hour rainfall totals of up to , with a similar flooding event in 2010 as a result of the remnants of tropical storm Georgette in the eastern Pacific and Hurricane Karl in the Gulf of Mexico. Summer. During a Minnesota summer, heat and humidity predominate in the south, while warm and less humid conditions are generally present in the north. A main feature of summer weather in Minnesota and the Midwestern United States as a  whole is the weakening of the jet stream, leading to slower movement of air masses, a general increase in the stability of temperatures, and less wind. The strong wind that does blow almost always comes from the south, bringing in warm temperatures and humidity. These humid conditions and a jet stream that has pushed into the northern parts of the U.S. initiate thunderstorm activity 30–40 days per year. Temperature. Daily average summer temperatures in Minnesota range from the low 70s (22 °C) in the south to the mid 60s °F (19 °C) in the north. Because summer  time air masses are not as volatile as in the winter, daily high and low temperatures rarely vary more than 15 degrees (7 °C) either side of normal. While summertime around much of the country means long stretches of hot and humid weather, Minnesota is located far enough north where periods of cooler, drier polar air frequently move in behind polar fronts dropping south from Canada. The polar air typically does not linger very long however and is quickly replaced by the warmer and more humid air from the Gulf of Mexico again. The cool, dry polar air colliding  with hot and humid summertime air keep the threat of thunderstorms and tornadoes in Minnesota through July and August. Northern Minnesota is considerably cooler and less humid than southern Minnesota during the summer months. For example, Duluth's annual average temperature and dew point are 6 degrees (3.4 °C) cooler than Minneapolis'. July is the hottest month in Minnesota statewide and is usually the month when the peak heat waves occur. In July 1936, Minnesota and the rest of the Midwest suffered through its most severe heat wave on record. Most of the state was engulfed in temperatures for  several days in a row, and Minnesota's all-time record high temperature of was equaled during this stretch. This heat wave was also responsible for the Twin Cities' all-time record high of , as well as the all-time record high of several other cities across the state. The western region of Minnesota experiences the hottest summer temperatures. Coteau des Prairies can heat cities to the north of it similar to how places in the Rocky Mountains are warmed by Chinook winds. As southwest winds blow down the slope of Coteau des Prairies, the air compresses and warms. This  heats the hot air even further and often brings locations such as Beardsley and Moorhead the hottest temperatures in the state, despite their higher latitudes. Precipitation. The summer months of June, July, August, and September account for nearly half of the annual precipitation total across the state of Minnesota. Most of this rain falls from thunderstorms, a frequent summer occurrence. Even though summer is the primary season for Minnesota to experience thunderstorms, they can occur from March to November. These storms can become severe, producing large hail, strong tornadoes, and large bow echos that result in damaging straight-line winds . Minnesota has experienced several major derecho events, most recently the Boundary Waters-Canadian Derecho which blew down millions of trees in the Boundary Waters Canoe Area Wilderness on July 4, 1999. Summertime thunderstorms are fueled by dew points that often reach beyond and sometimes even . In addition to severe conditions, thunderstorms produce heavy rain and cloud to ground lightning. Heavy rain brings flash floods to Minnesota an average of three days per year. With the exception of hail, summer precipitation in Minnesota is almost always in the form of rain. The lone exception is in far northern Minnesota, where in  mid-September, small amounts of snow become a possibility. Droughts. Droughts are an annual summer concern in Minnesota, especially for farmers. The growing season (which varies from 90 days per year in the Iron Range to 160 days in southeast Minnesota) is when Minnesota averages its highest percentage of annual precipitation, so a lack of rainfall during this time period can be devastating to crops. The last major drought in Minnesota was in 1988. During that year, the period of April to July was the second-driest in the previous century, and the period of May to August was the  hottest on record. The combination of dry skies and heat caused a severe drought which cost the state approximately 1.2 billion dollars in crop losses. Other memorable drought years were 1976 and the Dust Bowl years of the 1930s. During the dust bowl, inappropriate farming techniques enhanced by years of drought conditions led to dust storms in Southern Minnesota and the other parts of the Midwest. Drought conditions also have helped spawn forest fires. In 1894 the Great Hinckley Fire destroyed Hinckley killing an estimated 459 people, and in 1918 a forest fire killed 453 people in the vicinity of  Cloquet. More recently, in 2006, the Cavity Lake Fire burned 31,830 acres (129 km) in the Boundary Waters Canoe Area Wilderness. Tornadoes. Tornadoes are possible in Minnesota from March–November, but the peak tornado month is June, followed by July, May, and August. Tornadoes are most common in the southern half of the state, which is located on the northern edge of Tornado Alley. Just over a third of tornadoes in Minnesota strike between 4:00 pm and 6:00 pm. The state averages 27 tornadoes per year, 99% of which have ratings of F2 or weaker. On average Minnesota has an  F5 tornado once every 25 years. Some of the notable Minnesota tornadoes and outbreaks are: Autumn. Autumn weather in Minnesota is marked by the rapid decrease of severe thunderstorms, dramatic cooling, and eventually the possibility of blizzards. With summer-time heat still prevalent in the southern U.S. and colder air quickly taking hold in Canada, Minnesota can be affected by wide temperature swings in short periods of time. Because of this, the jet stream, which tends to weaken during the summer months, begins to re-strengthen. This leads to quicker changes in weather patterns and increasingly strong storm systems. As  autumn moves on, these storm systems bring with them progressively colder air, eventually changing the rain over snow, generally starting in October in the northern part of the state and November in the south. From September to December the average temperature in the state falls by approximately 43 °F (23 °C), the largest such temperature swing within any Minnesota season. Image and popular culture. Minnesota's climate has done much to shape the image of the state. Minnesota has a late but intense spring, a summer of water sports, an autumn of brilliantly colored leaves, and a long  winter with outdoor sports and activities. "Summer at the lake" is a Minnesota tradition. Water skiing was invented in Minnesota by Ralph Samuelson, and the Minneapolis Aquatennial features a milk carton boat race. Contestants build boats from milk cartons and float them on Minneapolis area lakes, with recognition based more on colorful and imaginative designs than on actual racing performance. But while Minnesota's warm summers provide its natives and tourists with a variety of outdoor activities, the state is known for its winters. The state has produced curlers, skiers, and lugers who have competed in the Winter Olympics, pioneers  who invented the snowmobile, and legions of ice fishing enthusiasts. The state is also known for enthusiastic ice hockey players, both at the amateur and professional levels. Eveleth, Minnesota, home to the United States Hockey Hall of Fame, boasts of the number of quality players and the contributions of the city (and the rest of the Mesabi Range) to the growth and development of hockey in the United States. To many outsiders, Minnesota's winters appear to be cold and inhospitable. A World War II newscaster, in describing the brutally cold conditions of the Russian front, stated that at least  Minnesotans could understand it. A New York journalist visited St. Paul and declared that the city was "another Siberia, unfit for human habitation." In response, the city decided to build a huge ice palace in 1886, similar to one that Montreal had built in 1885. They hired the architects of the Canadian ice palace to design one for St. Paul and built a palace 106 ft (32.3 m) high with ice blocks cut from a nearby lake. This began the tradition of the Saint Paul Winter Carnival, a ten-day festival which celebrates Minnesota's winter season. Minnesota's winters  are the setting of several television programs and Hollywood films, including the 1996 film "Fargo" which features the backdrop of a Minnesota winter, but like most of the characters in the movie, the climate is portrayed as bleak and inhospitable.