Science!
yes
JaMason the stud who is way kewler than JaZach and is equivilent to chuck norris, is the relationship between voltage and temperature.
They are scales for measuring temperature.
the deeper you go, generally the colder it gets
stephen gwapo kaayo
stephen gwapo kaayo
stephen gwapo kaayo
As tropospheric temperature increases, the troposphere tends to expand and its thickness grows. This is due to the fact that warmer air is less dense and occupies more space, pushing the boundaries of the troposphere higher into the atmosphere. Conversely, when tropospheric temperature decreases, the troposphere contracts and becomes thinner.
Temperature and altitude are inversely proportional in the troposphere. This means that as one increases, the other decreases. Approximately 165 meters up in the troposphere is equivalent to a 1 degree Celsius drop.
The top portion of the troposphere is known as the tropopause. It is characterized by a stable temperature gradient and acts as a boundary between the troposphere and the stratosphere above.
Yes, the temperature stops decreasing at the top of the troposphere, known as the tropopause. The tropopause marks the boundary between the troposphere and the stratosphere, and beyond this point, temperature remains relatively constant or may even increase with altitude.
Troposphere: Temperature decreases with hight Stratosphere : Temperature increases with height
The troposphere is the lowest layer of the Earth's atmosphere where weather occurs and temperature decreases with altitude. The tropopause is the boundary between the troposphere and the stratosphere, marking a stable layer where temperature stops decreasing with altitude.
The boundary between the troposphere and stratosphere is called the tropopause. It is characterized by a stable temperature inversion where the temperature stops decreasing with altitude and instead starts to increase. This boundary is located at an altitude of around 8-15 kilometers above the Earth's surface.
The thin outer layer of the troposphere that marks the boundary with the stratosphere is called the tropopause. It is characterized by a pause in the temperature change between the troposphere and the stratosphere and typically ranges in altitude from about 8 to 15 kilometers above Earth's surface.
The relationship between elevation and climate has to do with temperature. The higher up the elevation is the colder the temperature is.