Ch 7 Flashcards
Winds
generated by pressure differences that arise because of unequal heating of Earths surface
Macroscale
planetary, weeks or longer, 1000-40000 km ex trade winds
synoptic/weather-map scale, days to week, 100-5000 km ex mid latitude cyclone, anticyclones, and hurricanes
Mesoscale
minutes to hours, 1-100 km ex thunderstorms, tornadoes, and land-sea breeze
Microscale
seconds to minutes; <1 km ex. turbulence, dust devils, and gusts
Global winds
composite of all scales of motions
Typhoon Vongfong
appears as a large whirling cloud; can easily see its counterclockwise rotation; moving north; made of many individual cumulonimbus clouds (thunderstorms) each of these clouds are made up of even smaller-scale turbulences
Local Winds
mesoscale winds produced by a locally generated pressure gradient; many mesoscale circulations are the result of differential heating; if the heating/cooling is not uniform in the horizontal, the change in the thickness can result in horizontal pressure gradient which will drive the circulation
Sea Breeze
during the daylight hours the air above the land heats and expands, creating an area of lower pressure, cooler and denser air over the water moves onto the land
Land Breeze
at night the land cools more rapidly than the sea, generating offshore flow
Mountain Breeze
at night, the mountain slopes cool the surrounding air more quickly than the air found lower in the atmosphere. This creates a high pressure as air becomes more densely packed. The resulting high pressure causes winds to blow down the mountain towards the valley floor.
Valley Breeze
During the day, the surface of the mountain heats the air high up in the atmosphere, quicker than the valley floor cal. As the warmer air expands a low pressure is created near the top of the mountain. this attracts the air from the valley, creating a breeze that blows from the valley floor up towards the top of the mountain
Chinook winds
Warm, dry winds sometimes move down the east slopes of the Rockies (snow eaters), and the alps (Foehn), such winds are often created when a strong pressure gradient develops in a mountainous region. Water is extracted from the air in the form of precipitation on the windward side. The air on the leeward side is warmer than the air on the windward side
Santa Ana winds
noted for high speed, high temperature, and extreme dryness. These hot desiccating winds greatly increase the threat of fire in this already dry area
Katabatic (fall) winds
in the winter, some adjacent to highlands may experience a local wind; these winds originate when cold air, situated over a highland area such as the ice sheet of Greenland or Antarctica, is set in motion; the initial temperatures are so low that the wind arrives in the lowlands still colder and more dense than the air it invades
Country Breeze
circulation pattern is characterized by a light wind blowing from surrounding country side into the city; result of the urban heat island; clear calm nights; city buildings contain rock-like materials, tend to retain the heat accumulated during the day more than the less built up outlying areas