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ATMN&OCN 100
study prep for quiz on chapters 7&8
Term | Definition |
---|---|
Large body of air that has similar horizontal temperature and moisture characteristics | air mas |
Continental tropical air mass | cT |
Continental arctic air mass | cA |
Cool, moist, unstable air mass, often originating over the North Pacific or North Atlantic | maritime polar (mP) |
Type of air mass associated with atmospheric rivers | maritime tropical (mT) |
Hemisphere where you typically find the ITCZ in July | northern hemisphere |
Vast band of deep convection that moves seasonally north and south in the tropics | ITCZ (intertropical convergence zone) |
The major climate zone where Wisconsin is found | mid-latitudes |
Climate zone between 23N and 23S | equatorial/tropics |
The major climate zone where most of the global deserts are found | subtropics |
The type of scale of motion associated with high pressure systems, low pressure systems, fronts, and hurricanes | synoptic scale |
The type of scale of motion associated with longwave ridges and troughs | global/planetary scale |
The type of scale of motion associated with land-sea breezes, mountain breezes, thunderstorms, and tornadoes | mesoscale |
The type of scale of motion associated with eddies | microscale |
The smallest atmospheric scale of motion | microscale |
Refreshing breeze from the ocean to land during a summer afternoon along the ocean shore | sea breeze |
Phenomenon associated with warmer than normal ocean temperatures in the eastern tropical Pacific Ocean | El Nino |
Rising of deeper cold ocean water to the surface | upwelling |
Warm ocean current off the east coast of the United States | Gulf stream |
The cold northerly ocean current off northern California | California Current |
Line of constant pressure | isobar |
Type of jet stream typically found around 30 degrees latitude | subtropical jet stream |
Season over South Africa in July | winter |
Distance from ridge to ridge or trough to trough | wavelength |
Third factor that leads to the global circulation patterns of wind and pressure besides Earth’s rotation and land-sea differences | solar radiation |
Transition zone between two distinct air masses with different densities | front |
Type of weather front labeled by a red line with red semicircles | warm front |
Type of weather front labeled by a blue line with blue triangles | cold front |
Fourth type of weather front, besides cold front, warm front, and occluded front | stationary front |
Type of weather front in which a faster moving cold front overtakes a warm front | occluded front |
Theory that explains the life cycle of a most extratropical cyclones | polar front theory |
Spreading out of air, commonly found in the upper troposphere above a surface cyclone | divergence |
First stage of the life cycle of a mid-latitude cyclone | stationary front |
Last stage of the life cycle of a mid-latitude cyclone | cut-off |
Life cycle stage for a mid-latitude cyclone that follows the frontal wave stage | open wave stage |
Seasonal wind reversal in India, China, Australia, and West Africa | monsoon |
The third major atmospheric cell in addition to the Hadley Cell and Ferrel Cell | Polar cell |
Large atmospheric cell between 30 and 60 degrees latitude | Ferrel Cell |
Large stable cold anticyclone over Asia in winter | Siberian high |
The type of atmospheric circulation due to heating and cooling of air in which warm, less dense air rises and cold, denser air sinks | thermal circulation |
Snowfall downwind of the Great Lakes triggered by cold air passing over relatively warm, moist lakes | lake-effect snow |
Narrow channel of high-level atmospheric moisture flowing from the tropics and subtropics to the mid-latitudes | atmospheric river |
The state that is a peninsula and frequently experiences thunderstorms due to the convergence of sea breeze fronts | Florida |
Line of intense damaging winds and thunderstorms that travels a long distance | derecho |
Wintertime cyclones forming to the east of the Canadian Rockies and moving quickly into northern United States | Alberta Clipper |
Transport of cold air by the wind from a region of lower temperatures to a region of higher temperatures | cold advection |
Type of temperature advection you would expect to see to the east of a Northern Hemisphere cyclone | warm advection |
Steady northeasterly winds across the tropics in the Northern Hemisphere | trade winds |
Direction of air flow around an anticyclone over Europe | clockwise |
Direction of air flow around a cyclone over Canada | counterclockwise |
Narrow band of swiftly-flowing, wavy upper-level westerly air current | jet stream |
General time of day when a land breeze is most active along a coastal region | night |
The vast subtropical desert over northern Africa | Saharan Desert |
Linkage between weather changes occurring in widely separated regions of the world | teleconnection |
Another name for a large, slow-moving wave in the upper-level westerlies | Rossby wave |