On average, temperature decreases with height in the troposphere. The troposphere is bounded by the earth's surface and the tropopause (located at about 150 millibars in the tropics and 300 mb at high latitudes). In the troposphere on any given day, there are various layers between the surface and the tropopause where the lapse rates are far from average (the average environmental lapse rate is near 6.5 degrees C/km). Rawinsonde weather balloons measure temperature as they rise (this is the plot of the environmental lapse rate). Under certain conditions, the lapse rate in the atmosphere (defined as the change in temperature with height) is much above or much below normal.
Humans think of themselves as living on the surface of the earth, which, of course, is true. However, what is less obvious and more difficult for people to visualize is that life exists at the bottom of an ocean of air (the atmosphere).
The atmosphere is held tightly against the planet by the pull of gravity from within the planet. Investigations have revealed, however, that the atmosphere is not a homogeneous and unchanging mixture of gases from the surface of the planet on out into space. Rather, the atmosphere exists in layers and the conditions of temperature and pressure within each layer are different from the layers below it or above it.
The thermosphere has the greatest range of temperature, with temperatures increasing with altitude reaching up to thousands of degrees Fahrenheit due to absorption of solar radiation.
In the troposphere, temperature generally decreases as altitude increases. This is due to the decreasing air pressure and the fact that the upper regions of the troposphere are cooler due to their distance from the Earth's surface.
In the troposphere, temperature generally decreases with increasing altitude. This is because the troposphere is heated from the ground up by solar radiation, causing the lower layers to be warmer than the higher layers. This temperature decrease is known as the lapse rate.
In the troposphere, temperature generally decreases with increasing altitude at a rate of around 6.5°C per kilometer due to the adiabatic cooling effect as air pressure decreases with height. This relationship is known as the environmental lapse rate and defines the temperature profile of the troposphere.
The Earth's atmosphere is divided into five primary layers: the troposphere, stratosphere, mesosphere, thermosphere, and exosphere. Each layer has distinct characteristics, such as temperature changes, composition, and altitude range.
The thermosphere has the greatest range of temperature, with temperatures increasing with altitude reaching up to thousands of degrees Fahrenheit due to absorption of solar radiation.
the temperature of the troposhere is always cold and goes up and down but at the beginning of the troposphere it is about 15 degree's C.
Air temperature can be measured beyond the troposphere.
Air temperature can be measured beyond the troposphere.
The temperature of troposphere is not constant. It varies from -51C to 17 Celcius.
In the troposphere, temperature generally decreases as altitude increases. This is due to the decreasing air pressure and the fact that the upper regions of the troposphere are cooler due to their distance from the Earth's surface.
The temperature increases with altitude in the troposphere because of the absorption of solar radiation by the Earth's surface, which heats up the air closer to the surface. As you move higher in the troposphere, the air becomes thinner and less able to retain this heat, causing a decrease in temperature.
50 degrees
the troposphere is the closest layer to earth, so it would be the coldest right? no. the troposphere uses greenhouse gasses to trap in the heat I'm not sure what the exact temperature is but....there you go!! :)
the troposphere is the closest layer to earth, so it would be the coldest right? no. the troposphere uses greenhouse gasses to trap in the heat I'm not sure what the exact temperature is but....there you go!! :)
the temperature of the troposphere starts from 15 degrees - -6.5 degrees (believe it or not).......
In general, the temperature in the stratosphere is warmer than in the troposphere because the stratosphere absorbs ultraviolet radiation from the sun. The temperature inversion in the stratosphere creates a stabilizing effect on the atmosphere.