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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.
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How does the temperature change with elevation in the Andes?
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.
How does elevation affect temperature high land climate zones?
Elevation significantly affects temperature in highland climate zones due to the decrease in atmospheric pressure and density at higher altitudes. As elevation increases, the air becomes thinner and less able to retain heat, leading to cooler temperatures. This phenomenon, known as the lapse rate, typically results in a temperature drop of about 6.5 degrees Celsius for every 1,000 meters ascended. Consequently, regions at higher elevations tend to have distinct climate characteristics, including cooler temperatures and increased precipitation patterns compared to lower areas.
How does elevation effect climate?
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.
What is the effect of elevation on temperature and precipitation?
Elevation significantly influences temperature and precipitation patterns. Generally, as elevation increases, temperature decreases due to the thinning atmosphere, leading to cooler conditions at higher altitudes. Additionally, higher elevations often experience increased precipitation, particularly in mountainous regions, where moist air rises, cools, and condenses, resulting in orographic rainfall. This phenomenon contributes to diverse ecosystems and climatic variations in mountainous areas compared to surrounding lowlands.
How does elevation effect temperature?
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.
How temperature changes with increased elevation?
At higher altitude the temperature is lower.
What is the average temperature drop per 1000 feet of elevation?
The average temperature drops by about 3.5F per 1000 feet of elevation gain.
What are two ways for air to become saturated?
From increased evaporation or from a drop in the temperature.
How much does the temperature drop from every 1000 feet of elevation?
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.
How does the temperature change with elevation in the Andes?
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.
What is the relationship between elevation and temperature?
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.
Can elevation drop?
Yes.
What is relationship between temperature and elevation?
Temperature decreases as the elevation increases.
40 Describe at least two ways in which physical geography can affect weather?
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"
How does elevation affect temperature high land climate zones?
Elevation significantly affects temperature in highland climate zones due to the decrease in atmospheric pressure and density at higher altitudes. As elevation increases, the air becomes thinner and less able to retain heat, leading to cooler temperatures. This phenomenon, known as the lapse rate, typically results in a temperature drop of about 6.5 degrees Celsius for every 1,000 meters ascended. Consequently, regions at higher elevations tend to have distinct climate characteristics, including cooler temperatures and increased precipitation patterns compared to lower areas.
Temperature vs elevation?
As the altitude or elevation increases the temperature decreases. The temperature drops about 6.5 degree Celsius for every I km increase.
How does elevation effect climate?
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.
