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Atmospheric temperature - Wikipedia
Atmospheric temperature is a measure of temperature at different levels of the Earth's atmosphere. It is governed by many factors, including incoming solar radiation, humidity, and altitude. The abbreviation MAAT is often used for Mean Annual Air Temperature of a geographical location. See more
The temperature of the air near the surface of the Earth is measured at meteorological observatories and weather stations, usually using thermometers placed in a shelter such as a Stevenson screen—a … See more
The minimum temperature on calm, clear nights has been observed to occur not on the ground, but rather a few tens of centimeters above … See more
The variation in temperature that occurs from the highs of the day to the cool of nights is called diurnal temperature variation. … See more
The concept of a global temperature is commonly used in climatology, and denotes the average temperature of the Earth based on surface, near-surface or tropospheric … See more
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WEBThe atmosphere of Earth creates pressure, absorbs most meteoroids and ultraviolet solar radiation, warms the surface through heat retention (greenhouse effect), and reduces temperature extremes between day …
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WEBIn some layers, temperature increases with altitude and in others it decreases. The temperature gradient in each layer is determined by the heat source of the layer. Most of the important processes of the …
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WEB4 days ago · Earth’s atmosphere is bounded at the bottom by water and land—that is, by the surface of Earth. Heating of this surface is accomplished by three physical processes—radiation, conduction, and …
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WEBGHRC hosts a long-term record of daily and monthly average global temperatures at four levels of the atmosphere, derived from a series of Microwave Sounding Units (MSU, Advanced MSU) flown on NOAA and …
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