Māris kļaviņŠ, azamat azizov, JĀnis zaļoksnis environment, pollution, development: the case of uzbekistan

Part of this energy is reflected by cloud cover and small particles in 
the atmo sphere. 51% of radiation from the Sun is absorbed by the 
Earth’s surface, and this energy is spent for evaporation – as infrared 
radiation from the Earth and in convection and advection processes.
The theory that the composition of the Earth’s atmo sphere can 
affect the intensity of energy received from the Sun and the Earth’s 
climate has been around for more than 100 years. Solar radiation 
warms the Earth’s surface, and then the Earth reradiates this heat 
into the atmo sphere. Since the temperature of the Earth’s surface is 
by far lower than that of the Sun’s surface, the intensity of energy 
emitted by the Earth also is much lower and the wavelength of 
this energy – much higher than that of solar radiation. The Earth’s