S 290 unit 7 quiz answers 2025

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This is a katabatic wind (sometimes also called a mountain breeze). If the slopes are covered with ice and snow, the katabatic wind will , not only at night, but also during the day, carrying the cold dense air into the warmer valleys.
Although the density of the atmosphere decreases without limit with increasing height, for most practical purposes one can roughly place its upper boundary at about 500 km. However, half the mass of the atmosphere lies within 5 km, and 99.99% within 80 km of the surface.
Monsoons are winds which seasonally change their direction and characteristics, blowing from the sea in the summer and from the continent in the winter. The phenomenon of seasonal reversing winds, yet stabile in their directions is linked with insulation of Earth and heating/cooling process in these latitudes.