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From the Earth outward the layers of the atmosphere are; Troposphere, Stratosphere, Mesosphere, Thermosphere, Exosphere. These layers are divided by whether the temperature increases or deceases with an increase in altitude within the layer.
Its transfered by cunduction sun--> atmosphere
Collectively it's called the Atmosphere. There are sub-zones within the atmosphere but collectively it is referred to as the Atmosphere.
Uneven heating of the Earths atmosphere and oceans by the sun
Metamorphic rocks form when rocks change after undergoing extreme pressure or temperature increase. These temperature changes must be hot enough to reorganize matter within the rock but not hot enough to melt it.
Energy from deep within the earth
A barothermograph is an instrument used for recording both pressure and temperature within the atmosphere.
The characteristic is temperature. While pressure diminishes with increasing altitude, it is dependent on the underlying air masses. Temperature changes vary consistently within each of the major layers (troposphere, stratosphere, mesosphere, thermosphere, exosphere).
The atmosphere moderates temperature changes, keeping the surface warm at night and cool in the day. Without an atmosphere on Earth the temperature would probably go from about +100 degrees to -100 degrees every 24 hours. The atmosphere keeps it nicely within a range of ten degrees usually. Carbon dioxide allows radiant heat through to the Earth's surface but blocks heat being radiated away from the surface which is at a relatively low temperature. So it produces a 'greenhouse' effect which raises the surface temperature, but only by a little at present. On Venus, which has a 95% carbon dioxide atmosphere, the greenhouse effect has made the surface temperature 400-500 degrees C.
The atmosphere moderates temperature changes, keeping the surface warm at night and cool in the day. Without an atmosphere on Earth the temperature would probably go from about +100 degrees to -100 degrees every 24 hours. The atmosphere keeps it nicely within a range of ten degrees usually. Carbon dioxide allows radiant heat through to the Earth's surface but blocks heat being radiated away from the surface which is at a relatively low temperature. So it produces a 'greenhouse' effect which raises the surface temperature, but only by a little at present. On Venus, which has a 95% carbon dioxide atmosphere, the greenhouse effect has made the surface temperature 400-500 degrees C.
The outermost atmosphere of a star is called Stellar atmosphere. Within the Stellar atmosphere, the corona is the outermost part. The corona mostly consist of plasma which has a temperature above a million Kelvin.
Within the Solar System, that would probably be Venus, with a temperature of almost 500 °C. Mercury is quite hot, too, but it has no atmosphere to speak of.
The temperature and pressure of the atmosphere must be at that point or in an interval of values for the substance to be saturated. When mixing solutions, the temperature and pressure must be within a certain range for the substance to dissolve.
The resistance of a thermistor changes when its temperature changes due to the inherent properties of the thermistor material. In a negative temperature coefficient (NTC) thermistor, the resistance decreases as the temperature increases, whereas in a positive temperature coefficient (PTC) thermistor, the resistance increases as the temperature rises. This change in resistance is caused by the variation in the number of charge carriers (electrons or holes) and their mobility within the material as temperature changes.
From the Earth outward the layers of the atmosphere are; Troposphere, Stratosphere, Mesosphere, Thermosphere, Exosphere. These layers are divided by whether the temperature increases or deceases with an increase in altitude within the layer.
The prevailing pattern of easterly surface winds found in the tropics, within the lower portion of the Earth's atmosphere.
solar cycle is nothing but the different types of energy provided by sun to earth and the cyclic movement of this within the earth atmosphere. As there is variatiuon of temperature in temperature of various layers of atmosphere the drag force varies since it is proportional to the different of the temperature between the two given layers.