🗊 Презентация Radiation balance

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Radiation balance, слайд №1 Radiation balance, слайд №2 Radiation balance, слайд №3 Radiation balance, слайд №4 Radiation balance, слайд №5 Radiation balance, слайд №6 Radiation balance, слайд №7 Radiation balance, слайд №8 Radiation balance, слайд №9 Radiation balance, слайд №10
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Слайды и текст этой презентации

Слайд 1


Radiation balance (budget) of the Earth surface and the atmosphere Definition
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Radiation balance (budget) of the Earth surface and the atmosphere Definition

Слайд 2


Radiation balance of the Earth surface
Описание слайда:
Radiation balance of the Earth surface

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Radiation balance, слайд №3
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Слайд 4


Annual and diurnal variations of the radiation balance of the Earth surface.
Описание слайда:
Annual and diurnal variations of the radiation balance of the Earth surface.

Слайд 5


Some particularities of the radiation balance annual variation Annual variation of the radiation balance depends on latitude and type of underlying...
Описание слайда:
Some particularities of the radiation balance annual variation Annual variation of the radiation balance depends on latitude and type of underlying surface. Tropical area: radiation balance is always positive. Antarctic area: radiation balance is always negative due to large value of the surface albedo. At 60° latitude: radiation balance is positive 6 – 8 months a year. In arctic area there are some places where radiation balance (average for a year) is positive. It is valid for the places with snow and ice free surfaces for at least 2 months. The Sun shines here 24 hours at summer months. Question: Where radiation balance is larger on ocean or on land at the same altitude and weather conditions? Answer: On ocean, since water surface albedo is less than that of land

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Radiation balance depends on Sun altitude, albedo and cloudiness.
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Radiation balance depends on Sun altitude, albedo and cloudiness.

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Radiation balance of the atmosphere
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Radiation balance of the atmosphere

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Radiation balance, слайд №8
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Слайд 9


Radiation balance of the Earth as a whole planet We’ll discuss the balance of radiative energy in a vertical column including active layer of soil (...
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Radiation balance of the Earth as a whole planet We’ll discuss the balance of radiative energy in a vertical column including active layer of soil ( water) and the atmosphere.

Слайд 10


Cloudiness impact on RE value
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Cloudiness impact on RE value

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Теги Radiation balance
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