Question

Temperature range of the troposphere is ________.
(A) $ 217 - 288\;K $
(B) $ 180 - 220\;K $
(C) $ 280 - 320\;K $
(D) None of these

Answer 1

Hint: Lower atmosphere is the most reduced district of the climate which lies simply above the surface of the earth where all-natural exercises happen. At the point when daylight enters this area, $ C{O_2} $ molecules present in this locale ingest a lot of energy and get energized. This energized particle then crashes into different atoms and the abundance energy present in them is changed over into heat. This warmth causes a worldwide temperature alteration.

Complete Answer
As the thickness of the gases in this layer decline with tallness, the air gets slenderer. Hence, the temperature in the lower atmosphere likewise diminishes with tallness accordingly. As one trips higher, the temperature drops from a normal around $ \;288{\text{ }}K\left( {{{15}^o}C} \right) $ to $ 217{\text{ }}K{\text{ }}\left( { - {\text{ }}{{51}^o}C} \right) $ at the tropopause. There are, notwithstanding, various tropospheric species equipped for oxidizing these poisons so they become solvent. Despite the fact that these species are just present in moment sums, they comprise the turn of tropospheric science.

So, the answer is A.

Additional Information
No place around the Earth is the air entirely perfect. There are three end expulsion measures. The first is substance transformation to non-dirtying constituents, for example, $ {H_2}O $ or $ {O_2} $ . The second is dry affidavit, whereby gases are consumed by plants, water or soil. It is of restricted hugeness on the grounds that it frequently just applies to gases in the limit layer on a neighborhood scale. The third is expulsion by precipitation, and is just compelling for species that have enough dissolvability in water, which isn't the situation by and large.

Note
The tropopause is the limit district between the lower atmosphere and the stratosphere. In the lower atmosphere, temperature diminishes with height. In the stratosphere, in any case, the temperature stays consistent for some time and afterward increments with height. This coldest layer of the climate, where the pass rate changes from positive (in the lower atmosphere) to negative (in the stratosphere), is characterized as the tropopause. Subsequently, the tropopause is a reversal layer, and there is small blending between the two layers of the air.