No, the temperature in the troposphere decreases as the altitude increases.
The temperature decreases with altitude.
The upper layers of the atmosphere are heated from above, while the lower layers are heated from below, because infrared radiation is given off by the Earth's surface in response to solar heating. The lower troposphere (with its denser molecules and water vapor) receives heat from both re-radiation and convection. The result is that while the atmosphere always gets thinner with altitude, the temperature decreases with altitude in the troposphere, then increases with altitude in the stratosphere. The very high temperatures in the thermosphere are moot because of the low specific heat (energy capacity) of the tenuous gases there.
It increases.
The absolute magnitude of a start will increase both:* If its surface temperature increases, and * If its diameter increases.
There is no distance from the earth to space. The atmosphere gradually gets thinner as altitude increases. The furthest noticeable part of the atmosphere is "said" to be approx. 600mile from sea level. You will be close to the thinnest part of the atmosphere when you realize that you can't increase altitude anymore.
Temperature decreases as altitude increases in the troposphere
No, the temperature does not increase in fact it decreases as the altitude increases yes it does.
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.
The temperature of the Troposphere generally decreases as altitude increases.
The temperature in the troposphere and the mesosphere decrease with altitude.
The temperature decreases with altitude.
The temp rises
as altitude increases in the troposphere the temp. decreases. on average for every 1 kilometer increase in altitude the air gets about 6.5 Celsius degrees cool.
The temperature increases like the stratosphere
It keeps getting colder. (to about -70 degrees F).
In the troposphere, temperatures decrease with altitude (air pressure), in the effect known as the adiabatic lapse rate (9.8 °C per thousand feet).
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.