As we rise in the troposphere, the lowest division of the atmosphere, the temperature on the average falls at about 3.5 degrees Fahrenheit. This is called the dry adiabatic lapse rate and holds until we reach the stratosphere at about 8-10 miles at which point the temperature, which has cooled to about -60 degrees Celsius starts to rise again. The drop in temperature as we move up through the troposphere is primarily caused by the decreasing weight of the air in a column above the point we are measuring. Although the actual state of the atmosphere at any moment is very complex, the simplest thermodynamic model predicts that a small volume of air will expand slightly if it rises slightly. This expansion extracts energy from the air and thus is becomes slightly cooler. The same effect, namely expansion creating cooling and compression causing warming, is used in refrigerators.
In the Andes, temperature generally decreases with increasing elevation due to the lapse rate, which causes cooler temperatures at higher altitudes. On average, for every 1,000 feet increase in elevation, the temperature can drop by around 3.5°F to 5.4°F. This temperature variation with elevation creates diverse ecosystems and climate zones in the Andes mountain range.
Elevation affects climate by influencing temperature and precipitation patterns. Generally, as elevation increases, the temperature decreases, leading to cooler conditions. Higher elevations also tend to receive more precipitation due to orographic lift, where air masses are forced to rise over mountains, leading to increased rainfall or snowfall on the windward side and drier conditions on the leeward side.
Mixing and temperature elevation
As elevation increases, the temperature typically decreases. This is because air pressure decreases with altitude, causing the air to expand and cool. The rate of temperature decrease with elevation is called the lapse rate.
The temperature after the drop was -4°F.
At higher altitude the temperature is lower.
The average temperature drops by about 3.5F per 1000 feet of elevation gain.
From increased evaporation or from a drop in the temperature.
On average, the temperature drops approximately 3.5°F for every 1,000 feet increase in elevation. This phenomenon is known as the environmental lapse rate and is a key factor in understanding how temperature changes with altitude in the atmosphere.
In the Andes, temperature generally decreases with increasing elevation due to the lapse rate, which causes cooler temperatures at higher altitudes. On average, for every 1,000 feet increase in elevation, the temperature can drop by around 3.5°F to 5.4°F. This temperature variation with elevation creates diverse ecosystems and climate zones in the Andes mountain range.
As a general rule in the atmosphere, the higher the elevation the lower the temperature. However, certain atmospheric conditions may produce an 'inversion', where temperature increases with elevation.
Yes.
Temperature decreases as the elevation increases.
Air moving from a higher elevation to a lower elevation can cause turbulence in the air stream increasing air speed at the base of an elevation drop. Air moving over water will drop in temperature causing moisture evaporation in to the atmosphere. In the winter this is sometimes called "lake effect snow"
As the altitude or elevation increases the temperature decreases. The temperature drops about 6.5 degree Celsius for every I km increase.
Elevation affects climate by influencing temperature and precipitation patterns. Generally, as elevation increases, the temperature decreases, leading to cooler conditions. Higher elevations also tend to receive more precipitation due to orographic lift, where air masses are forced to rise over mountains, leading to increased rainfall or snowfall on the windward side and drier conditions on the leeward side.
Top Elevation: 3115 Ft. Bottom Elevation: 2415 Ft.Vertical Drop: 700 Ft.