Upsc geography

2022-11-10 17:44:51 ■ Incoming Shortwave Solar Radiation and the Heat Budget of the earth and the Atmosphere

#Insolation

◇ The earth receives most of its energy from the sun through shortwave solar radiation. The solar energy radiated towards the earth's surface is taken as 100 per cent or 100 units.

◇ Out of the total incoming per solar radiation entering the earth's atmosphere 35 cent is sent back to space through scattering by dust particles (6%), reflection from the clouds (27%) and from the ground surface (2%), 51 per cent is received by the earth's surface (received as direct radiation), and 14 per cent is absorbed by the atmospheric gases (ozone, oxygen etc.) and water vapour in different vertical zones of the atmosphere. ओपन / कमेंट

2022-11-10 16:35:19 ओपन / कमेंट

2022-11-10 15:33:37



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2022-11-10 10:15:57 ■ FACTORS CONTROLLING, THE DISTRIBUTION OF TEMPERATURE

□ Latitudes

◇ The temperature of the atmosphere of a particular place near the ground surface depends on the amount of insolation received at that place. Since the amount of insolation received by the ground surface decreases poleward from the equator i.e. from low latitudes towards high latitudes because the sun's rays become more and more oblique (slanting) poleward and hence air temperature also decreases poleward.

◇ It may be noted that though sun's rays are almost vertical over the equator throughout the year but there is no maximum temperature on it rather maximum temperature is recorded along 20°N latitude in July because major portion of insolation is reflected by clouds and sizeable amount of heat is lost in evaporation in the low latitude zone (equatorial zone).

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2022-11-09 18:20:24 ■ FACTORS CONTROLLING, THE DISTRIBUTION OF TEMPERATURE

□ Latitudes

◇ The temperature of the atmosphere of a particular place near the ground surface depends on the amount of insolation received at that place. Since the amount of insolation received by the ground surface decreases poleward from the equator i.e. from low latitudes towards high latitudes because the sun's rays become more and more oblique (slanting) poleward and hence air temperature also decreases poleward.

◇ It may be noted that though sun's rays are almost vertical over the equator throughout the year but there is no maximum temperature on it rather maximum temperature is recorded along 20°N latitude in July because major portion of insolation is reflected by clouds and sizeable amount of heat is lost in evaporation in the low latitude zone (equatorial zone).

︎Join - @upsc_geography_notes ओपन / कमेंट

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2022-11-09 16:54:27 ■ FACTORS CONTROLLING, THE DISTRIBUTION OF TEMPERATURE

□ Latitudes

◇ The temperature of the atmosphere of a particular place near the ground surface depends on the amount of insolation received at that place. Since the amount of insolation received by the ground surface decreases poleward from the equator i.e. from low latitudes towards high latitudes because the sun's rays become more and more oblique (slanting) poleward and hence air temperature also decreases poleward.

◇ It may be noted that though sun's rays are almost vertical over the equator throughout the year but there is no maximum temperature on it rather maximum temperature is recorded along 20°N latitude in July because major portion of insolation is reflected by clouds and sizeable amount of heat is lost in evaporation in the low latitude zone (equatorial zone).

︎Join - @upsc_geography_notes ओपन / कमेंट