a large body of air that has similar horizontal temperature and moisture characteristics
back door cold front
a cold front moving south or southerwest along the Atlantic seaboard of the United States
a transition zone where a cold air mass advances and replaces a warm air mass
an air mass characterized by extremely low temperatures and very dry air
an air mass characterized by low temperatures and dry air
an air mass characterized by high temperatures and low humidity.
an atmospheric condition that exits when the winds cause a horizontal net inflow of air into a specified region.
the development or strengthening of middle-latitude cyclones
an atmospheric condition that exits when the winds cause a horizontal net outflow of air from a specific region.
the transition zone between two distinct air masses.
a wavelike deformation along a front in the lower levels of the atmosphere. Those that develop into storms are termed unstable waves, while those that do not are called stable waves.
a region of high wind speed that moves through the axis of a jet stream. Also called jet maximum.
localized snowstorms that form on the downwind side of a lake. Such storms are common in late fall and early winter near the Great Lakes as cold, dry air picks up moisture and warmth from the unfrozen bodies of water.
storm systems that form on the downwind (lee) side of a mountain chain. In the US lee-sode lows frequently form on the eastern side of the Rockies and Sierra Nevadas.
an air mass characterized by low temperatures and high humidity.
an air mass characterized by high temperatures and high humidity
a name given to a strong, steady wind from the northeast that is accompanied by rain and inclement weather. It often develops when a storm system moves northeastward along the coast of North America.
a complex frontal system that ideally forms when a cold front overtakes a warm front. When the air behind the front is colder than the air head of it, the front is called a cold occlusion. When the air behind the front is milder than the air ahead of it, it is called a warm occlusion.
the stage of development of a wave cyclone where a cold front and a warm front exist, but no occluded front. The center of lowest pressure in the wave is located at the junction of the two fronts.
a condition that occurs when air moves up an dover another layer of air.
polar front theory
a theory developed by a group of Scandinavian meteorologists that explains the formation, development, and overall life history of cyclonic storms that form along the polar front.
regions where air masses originate and acquire their properties of temperature and moisture.
a front hat is nearly stationary with winds blowing almost parallel and from opposite directions on each side of the front
a front that moves in such a way that warm air replaces cold air.
an extratropical cyclone that forms and moves along a front. The circulation of winds about the cyclone tends to produce a wavelike deformation on the front.