At which latitude is the heat lost by insolat | vedclass

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(C) The Earth's heat balance is maintained by the redistribution of energy from the tropics to the poles. In the tropical regions,there is a surplus o

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$40^{\circ}$ North and South

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(C) The Earth's heat balance is maintained by the redistribution of energy from the tropics to the poles. In the tropical regions,there is a surplus of heat because insolation (incoming solar radiation) exceeds terrestrial radiation (outgoing heat). Conversely,in the polar regions,there is a deficit of heat because terrestrial radiation exceeds insolation. The transition point where the incoming solar radiation and outgoing terrestrial radiation are approximately balanced occurs at approximately $40^{\circ}$ North and South latitudes. Beyond this latitude,the heat deficit increases towards the poles.

At which latitude is the heat lost by insolation approximately equal to the heat lost by terrestrial radiation?

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