The temperature gets colder as you go upward in the troposphere. Light from the Sun heats the ground. The warm ground gives off the heat as infrared "light". The IR energy heats the troposphere. The lowest part of the troposphere is the warmest because it is closest to the ground, where the heat is coming from.
At sea level the normal boiling temperature is 212 °F. As you go up in elevation, the boiling temperature drops.
The higher up you go in elevation the thinner the air around you becomes making it hard to breathe for many people.
it blows up and down, up and down
it's impossible to throw up while holding a tube! :P
The water becomes 100 degrees and is warm to the touch.
It gets colder by 1 degree Celsius for about every 160 meters you go up.
The relationship between elevation and climate has to do with temperature. The higher up the elevation is the colder the temperature is.
As elevation increases temperature decreases reaching the coldest altitude (around -90 degrees C). Once you ascend into the Thermosphere (56 miles high) The temperatures will be extremely high, ranging from 200 degrees C up to 500 Degrees C as you climb in elevation.
temperature and altitude
As you go up a mountain, the air pressure decreases, which can lead to lower oxygen levels. This may cause difficulties breathing and can lead to altitude sickness. The temperature also tends to drop as you ascend.
the temp goes down, the winds go up, and the pressure goes up...
It decreases because as you move up in altitude the air becomes thinner making it colder.
the line go up
As one goes up in elevation, the temperature tends to decrease due to the lapse rate, causing climatic conditions to become cooler. Also, air pressure decreases, affecting atmospheric stability and precipitation patterns. This can result in higher humidity levels, increased cloud formation, and changes in vegetation types due to the differences in temperature and precipitation.
The environmental lapse rate is used to calculate temperature changes as elevation increases. On average, the lapse rate is around 3.5°F per 1,000 feet gained in elevation. As you ascend a mountain, the temperature typically drops due to a decrease in air pressure, leading to the air expanding and cooling.
At sea level the normal boiling temperature is 212 °F. As you go up in elevation, the boiling temperature drops.
The higher up in elevation a place is, the colder it will be. As for surface currents, I have no clue.