Local winds are caused by differences in air pressure due to uneven heating of land and water surfaces. During the day, sea breezes and valley breezes blow in from cooler waters or valleys to replace rising warm air above heated land or mountain surfaces. At night, land and mountains cool faster than water or valleys, so mountain breezes and katabatic winds blow down from elevated areas. Foehn and chinook winds are gusty winds caused by warm, dry air descending on the leeward side of mountains after being cooled and dried on the windward side.
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Physical Geography Lecture 08 - Precipitation, Air Masses, and Storms 110216angelaorr
The formation of precipitation. Types of precipitation. Global and U.S. precipitation. Air masses, source regions, classification. Air masses of North America. Fronts. Warm front, cold front, stationary front, occluded front. Life-cycle of a midlatitude cyclone. Weather changes with the passage of a cold front. Midlatitude anticyclones. Lightning, thunder. Tornadoes. Hurricanes. Storm surge.
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Global water budget. Hydrologic cycle. Residence time. Latent Heat Transfer diagram. Saturation. Factors affecting rate of evaporation. Vapor pressure. Relative Humidity. Dew point. The adiabatic process. DAR, LCL, latent heat of condensation, SAR. Stable vs Unstable air. Clouds. Fog. Dew.
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The wind blowing from land towards the sea is Land breeze. The wind blowing from the sea towards the land is Sea breeze. It occurs during the nights or early mornings. The wind blowing from land towards the sea is Land breeze. The wind blowing from the sea towards the land is Sea breeze. It occurs during the nights or early mornings.
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https://viralsocialtrends.com/vat-registration-outlined-in-uae/
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