Science- Unit 4

the force exerted by the weight of a column of air above a given point

An instrument used for measuring air pressure that contains an empty metal chamber that compresses or expands as pressure changes.

a high pressure system characterized by an outward, clockwise flow of air in the northern hemisphere

An instrument that measures atmospheric pressure.

the boundary between a cold and warm air mass in which the cold air replaces the warm air at the surface and the warm air is lifted.

the rotation of the earth causes the wind to bend to the right of its intended flow from high to low in the northern hemisphere (clockwise) and to the left in the southern hemisphere (counterclockwise).

a low pressure system characterized by an inward and counterclockwise flow of air in the northern hemisphere. Tornadoes, hurricanes and mid-latitude cyclones are all types of cyclones.

boundary between two different air masses

line of equal air pressure on a weather geek map

local wind that comes off the land onto the water usually during the night due to differential cooling and the formation of local high and low pressures

a large low pressure system characterized by an inward and counterclockwise flow of air and including warm and cold fronts in its middle stage ending in an occluded front- named for where air mass originates

A seasonal reversal of wind direction associated with large continents (especially Asia) caused by differential heating of land vs. water

When the warm sector between a cold and warm front is lifted above the surface as the cold front catches up to and lifts the warm front.

difference in barometric (air) pressure between two points

A local wind blowing from the ocean toward the land during the afternoon in costal areas formed due to differential heating of land vs. water and associated pressure gradient

A boundary between warm and cold air masses that are not moving into one another possibly causing clouds and rain for several days.

a front between a warm and cold air mass in which the warm air mass is replacing the cold at the surface. As warm air lifts in a gentle slope over cold air it brings a typical pattern of cirrus, cirrostratus/cirrocumulus, altostratus, stratus and finally nimbostratus drizzly rain followed by warm and clear weather. Sleet and freezing rain associated with this front in the winter.

Clear ice pellet precipitation, forms when rain falls through a thick layer of freezing air and freezes solid before hitting the ground. Associated with warm front passage in the winter

Clear, layered ice pellet precipitation that fall from cumulonimbus clouds after growing through multiple convection loops in cloud. Associated with Summer thunderstorms and cold fronts.

raindrops that fall through a cold layer and cool to below freezing but don't solidify until after they hit the ground or other cold surfaces forming a dangerous ice coating. Typically forms in the winter on a warm front.

Part of air mass classification scheme that denotes an air mass that forms over cold regions in the north. Suggests the air mass will be cold. There are both maritime and continental polar air masses.

Part of air mass classification scheme that denotes an air mass that forms over warm regions to our south. Suggests the air mass will be warm. There are both maritime and continental tropical air masses

Part of air mass classification scheme that denotes an air mass that forms over land. Suggests the air mass will be dry. There are both polar and tropical continental air masses

A bitterly cold air mass that forms over the frozen Arctic.

Part of air mass classification scheme that denotes an air mass that forms over ocean. Suggests the air mass will be humid. There are both polar and tropical maritime air masses

the movement of air from high to low pressure in an attempt to equalize air pressure

An instrument used to measure wind speed

a large-scale atmospheric convection cell in which air rises at the equator and sinks at medium latitudes, typically about 30° north or south.

The condition that exists at higher (jet stream) altitudes when the distribution of winds within a given area results in a net horizontal inflow.

The condition that exists at higher (jet stream) altitudes when the distribution of winds within a given area results in a net horizontal outflow.