Презентация Thermal regime of the atmosphere онлайн

Содержание слайда: Thermal regime of the atmosphere Zonal temperature field (ZTF) Averaging air temperature along every latitude, we obtain ZTF. The main feature of this field is the constancy of the temperature at every point of a latitude. Although in reality it is not the case, but for better understanding of the temperature regime, presentation temperature field in this manner is very convenient.

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Содержание слайда: Vertical temperature distribution (lapse rate)

Содержание слайда: Tropopause height and air temperatures near the tropopause.

Содержание слайда: Real temperature distribution

Содержание слайда: Periodic and irregular temperature variations

Содержание слайда: Monsoons The word “monsoon” means season. However, meteorologists understand it as seasonal change of the winds and associated weather conditions. In summer permanent winds blow from sea or ocean to a continents, in winter the situation is reversed. Very often summer monsoon is accompanied by heavy rains, while the winter monsoon is known to bring fair weather.

Содержание слайда: Green house effect

Содержание слайда: General conclusion My dear fiends, We have broken the back of our course having accomplished its part dealing with energy income, energy transformation in the atmosphere determining the temperature regime. Information you have got will be needed and useful for study and understanding the further chapters of the course and some other courses of your program. You didn’t bay the Moon, did you? You were rather successful. Now, we’ll take some other topics, which will lead us to the understanding of what we call WEATHER and the processes of its formation. The first step on this way is the WATER IN THE ATMOSPHERE. by G. G. Tarakanov