The relationship between arctic tropopause height and surface air temperature is discussed by using the aerological sounding and surface data during 1977-1990 in Beijing area.
When you see the top of a storm cloud flattening out into the classic anvil shape, you are looking at the boundary between the troposphere and stratosphere.
Buildings, mountains, buildings on mountains… all these things obstruct and redirect the wind, creating eddies in the troposphere that shake aircraft like a Polaroid picture.
This mammoth skyscraper will extend for more than 12 miles from top to bottom, meaning its “roof” or top will be somewhere in the troposphere, far above the Earth's surface.
Scientists simulated an AACP using a numerical model and environmental conditions known to produce severe storms. Typically, storms stay in the troposphere, the lowest part of the atmosphere where we live.