page_title: Air-mass thunderstorm
hierarchical_section_title: Air-mass thunderstorm
caption_attribution_description: A thunderstorm over en:Wagga Wagga, New South Wales, en:Australia Photo taken by en:User:Bidgee Because this photograph concerns privacy since this was taken on a private property, only an approximate location is provided: Wagga Wagga, New South Wales, Australia
context_page_description: An air-mass thunderstorm, also called an "ordinary", "single cell", or "garden variety" thunderstorm, is a thunderstorm that is generally weak and usually not severe. These storms form in environments where at least some amount of Convective Available Potential Energy is present, but very low levels of wind shear and helicity. The lifting source, which is a crucial factor in thunderstorm development, is usually the result of uneven heating of the surface, though they can be induced by weather fronts and other low-level boundaries associated with wind convergence. The energy needed for these storms to form comes in the form of insolation, or solar radiation. Air-mass thunderstorms do not move quickly, last no longer than an hour, and have the threats of lightning, as well as showery light, moderate, or heavy rainfall. Heavy rainfall can interfere with microwave transmissions within the atmosphere.
  Lightning characteristics are related to characteristics of the parent thunderstorm, and could induce wildfires near thunderstorms with minimal rainfall. On unusual occasions there could be a weak downburst and small hail. They are common in temperate zones during a summer afternoon.
context_section_description: An air-mass thunderstorm, also called an "ordinary", "single cell", or "garden variety" thunderstorm, is a thunderstorm that is generally weak and usually not severe.  These storms form in environments where at least some amount of Convective Available Potential Energy (CAPE) is present, but very low levels of wind shear and helicity.  The lifting source, which is a crucial factor in thunderstorm development, is usually the result of uneven heating of the surface, though they can be induced by weather fronts and other low-level boundaries associated with wind convergence.  The energy needed for these storms to form comes in the form of insolation, or solar radiation.  Air-mass thunderstorms do not move quickly, last no longer than an hour, and have the threats of lightning, as well as showery light, moderate, or heavy rainfall.  Heavy rainfall can interfere with microwave transmissions within the atmosphere.
  Lightning characteristics are related to characteristics of the parent thunderstorm, and could induce wildfires near thunderstorms with minimal rainfall.  On unusual occasions there could be a weak downburst and small hail.  They are common in temperate zones during a summer afternoon.  Like all thunderstorms, the mean-layered wind field the storms form within determine motion.  When the deep-layered wind flow is light, outflow boundary progression will determine storm movement.  Since thunderstorms can be a hazard to aviation, pilots are advised to fly above any haze layers within regions of better visibility and to avoid flying under the anvil of these thunderstorms, which can be regions where hail falls from the parent thunderstorm.  Vertical wind shear is also a hazard near the base of thunderstorms which have generated outflow boundaries.
caption: An air-mass thunderstorm over Wagga Wagga.
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