what is the relationship between temperature and elevation?
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The reason why temperature decreases as elevation increases is because air pressure similarly decreases with elevation. As the air pressure decreases, the air density also decreases causing a decrease in temperature.
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In the stratosphere, temperature increases with altitude. The reason is that the direct heat source for the stratosphere is the Sun. A layer of ozone molecules absorbs solar radiation, which heats the stratosphere.
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Because warm air rises and cool air sinks, the troposphere is unstable. In the stratosphere, temperature increases with altitude. The stratosphere contains the ozone layer, which protects the planet from the Sun's harmful UV radiation.
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Pressure with Height: pressure decreases with increasing altitude. The pressure at any level in the atmosphere may be interpreted as the total weight of the air above a unit area at any elevation. At higher elevations, there are fewer air molecules above a given surface than a similar surface at lower levels.
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Normally, air temperature decreases with an increase in altitude. During an inversion, warmer air is held above cooler air; the normal temperature profile with altitude is inverted. An inversion traps air pollution, such as smog, close to the ground. An inversion can also suppress convection by acting as a "cap".
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The two have an inverse relationship, that is, when elevation increases, atmospheric pressure decreases. This is due to the amount of air on top of you at your current elevation. At lower elevations, you have more air above you, and thus more pressure.
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An inversion exists when temperature increases with altitude. The figure below shows the four layers: the Troposphere, the Stratosphere, the Mesosphere, and the Thermosphere. Between each layer exists a "pause" in which the temperature remains constant with height.
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As you increase altitude, the air gets increasingly rarer, which leads to a loss of pressure. Temperature is directly proportional to pressure, so the lower the pressure, the lower the temperature. In short, the higher the altitude, the lower the temperature.
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Temperature is inversely related to latitude. As latitude increases, the temperature falls, and vice versa. Generally, around the world, it gets warmer towards the equator and cooler towards the poles.
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The physical rationale behind the relationship between rainfall and temperature is that rainfall may affect soil moisture which may in turn affect surface temperature by controlling the partitioning between the sensible and latent heat fluxes [41].
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What is the relationship between the speed of plates and height of mountain ranges? The faster the plates are moving, the higher the mountain ranges.
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Altitude is height above sea level. The density of air decreases with height. There are two reasons: at higher altitudes, there is less air pushing down from above, and gravity is weaker farther from Earth's center. So at higher altitudes, air molecules can spread out more, and air density decreases (Figure below).
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In contrast to surface temperature is air temperature, which is measured at a standard height of 1.2 m (4.0 ft) above the ground surface. In general, air temperatures above a surface reflect the same trends as ground surface temperatures, but ground temperatures are likely to be more extreme. ...
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The distance above sea level. How does latitude and altitude affect climate? The altitude affects the climate because the higher the altitude, the cooler and harsher the climate. Also, if the latitude is to 0 degrees, the hotter the temperature and the more humidity in the atmosphere.
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Temperature is directly proportional to the depth inside Earth. In simple terms, it means the temperature increases as the depth increases inside..
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As atmospheric pressure decreases, water boils at lower temperatures. At sea level, water boils at 212 °F. With each 500-feet increase in elevation, the boiling point of water is lowered by just under 1 °F.
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Simple summary, in the lowest atmosphere, the troposphere, the temperature declines as altitude rises, as rising pockets of air lose thermal energy to gain potential energy. In the stratosphere it increases with altitude, due to UV absorption. In the mesosphere it declines again.