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How the atmosphere heated?

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Anonymous

8y ago
Updated: 11/20/2021

A small part of the heating of the atmosphere is directly from the sun. A lot of heating near the surface is done through conduction from land or water that has been warmed by the sun.

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Related Questions

Is the earth heated by the sun?

it is heated by conduction by the earths atmosphere


How air get heated in atmosphere?

air gets heated with carben dioxid and the rays of the sun


Is the earth's atmosphere heated directly by a planet or a star?

Earth is heated by the sun, which is a star.


Is the earths atmosphere heated by solar energy?

Yes, the Earth's atmosphere is heated by solar energy. Sunlight penetrates the atmosphere and warms the surface of the Earth. This heat is then radiated back into the atmosphere, contributing to its overall temperature.


What layer of the atmosphere is heated by the ozonosphere?

conduction


Which layer of the atmosphere is heated by the earth?

Stratosphere


What heats the lower atmosphere?

The lower atmosphere is primarily heated by the sun's radiation. As sunlight enters the atmosphere, it warms the Earth's surface, which then emits heat energy back into the atmosphere. This process creates a temperature gradient, with warmer air near the surface and cooler air at higher altitudes.


Why is the atmosphere heated more from below?

The atmosphere is more heated from below because the air is thicker the farther down you go, and so it traps the heat in the air.


What layer of the atmosphere is heated by the earths surface?

trophosphere


What layer of the atmosphere is heated by earth's surface?

trophosphere


Which term best describes how the earth's atmosphere is heated?

m


Is it a condition in which the upper regions of the atmosphere are warmer than the lower regions?

No, typically the upper atmosphere is colder than the lower atmosphere. This is because the lower regions of the atmosphere are heated by the Earth's surface, while the upper atmosphere is heated by solar radiation. This temperature difference contributes to the formation of weather patterns and circulation in the atmosphere.