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If the temperature increases with increasing altitude in the troposphere, then a temperature inversion exists. All the weather that we are primarily interested in, occurs in the troposphere.
Troposphere
The layer of the atmosphere that contains weather is the troposphere. It is the lowest layer of the atmosphere where temperature decreases with increasing altitude and where most weather phenomena occur, including clouds, precipitation, and wind.
The troposphere, the lowest layer of Earth's atmosphere, is heated from below. The troposphere is warmest at the bottom near Earth's surface. The troposphere is coldest at its top, where it meets up with the layer above (the stratosphere) at a boundary region called the tropopause. Temperatures drop as you move upward through the troposphere.Sunlight streams down from space through the atmosphere, striking the ground or ocean beneath. The sunlight heats the surface, and that surface radiates the heat into the adjacent atmosphere. Atmospheric scientists use a concept called a "standard atmosphere" to represent an average atmosphere with variations caused by weather, latitude, season, and so forth, removed. In the standard atmosphere model, the temperature at sea level at the bottom of the troposphere is 15° C (59° F). Higher up in the troposphere, where less heat from the surface warms the air, the temperature drops. Typically, the temperature drops about 6.5° C with each increase in altitude of 1 kilometer (about 3.6° F per 1,000 feet). The rate at which the temperature changes with altitude is called the "lapse rate". In the standard atmosphere, by the time you reach the top of the troposphere the temperature has fallen to a chilly -57° C (-70° F).Of course, the atmosphere is always changing and is never "standard". Temperatures in the troposphere, both at the surface and at various altitudes, do vary based on latitude, season, time of day or night, regional weather conditions, and so on. In some circumstances, the temperature at the top of the troposphere can be as low as -80° C (-110° F). When a weather phenomenon called at "temperature inversion" occurs, temperature in some part of the troposphere gets warmer with increasing altitude, contrary to the normal situation.In the layer above the troposphere, the stratosphere, temperature rises with increasing altitude. In the stratosphere, the air is heated from above by ultraviolet "light" which is absorbed by ozone molecules in the air. The tropopause is the boundary between the troposphere (below) and the stratosphere (above). The tropopause occurs where the temperature stops dropping with increasing altitude (in the troposphere) and begins climbing with increasing altitude (the stratosphere).
The rate of change of air pressure as a function of increasing altitude decreases with increasing altitude.
If the temperature increases with increasing altitude in the troposphere, then a temperature inversion exists. All the weather that we are primarily interested in, occurs in the troposphere.
this is known as a temperature inversion
The hotter temperatures in the troposphere (layer of atmosphere closest to the earth's surface) are near the surface of the earth The colder temperatures are at the top of the troposphere.
Temperature decreases as altitude increases in the troposphere
No, the temperature in the troposphere decreases as the altitude increases.
As the altitude increases, the temperature in the troposphere will decrease. The troposphere is the lowest portion of planet's atmosphere.
in any altitude in the troposphere. :)
Temperature decreases as altitude increases.
The stratosphere is the layer above the troposphere (where we live). The ozone layer is found in the lower stratosphere. The stratosphere is the lowest layer where temperature increases with increasing altitude.
Troposphere
Troposphere
The temperature changes within the stratosphere with increasing distance from the earth. The temperature increases with altitude, reaching a maximum of about 2 degrees Celsius This is unlike the troposphere, where the temperature decreases with increasing altitude. The heating is caused by the ozone layerbecause as it absorbs solar radiation, the heat around the ozone layer charges the particles in the upper stratosphere as it releases some energy, increasing its temperature. This is also simply known as conduction. Unlike the troposphere, the stratosphere is generally stable, and the warmer air does not cool down and fall like how it does in the troposphere.