A graph that shows the general trend between differences in elevation above sea level and the average annual temperature within the troposphere would depict a decrease in temperature with increasing elevation. As you go higher in the troposphere, the temperature generally decreases due to the lapse rate, which results in cooler temperatures at higher elevations.
A graph showing a negative correlation between elevation above sea level and average annual temperature would best represent the general effect. As altitude increases, temperatures typically decrease in the troposphere due to lower air pressure and the lapse rate. This relationship is commonly observed in mountainous regions.
Temperature decreases as altitude increases in the troposphere
In the troposphere, temperature generally decreases with increasing altitude at a rate of around 6.5°C per kilometer due to the adiabatic cooling effect as air pressure decreases with height. This relationship is known as the environmental lapse rate and defines the temperature profile of the troposphere.
The troposphere is the layer of the atmosphere that extends to an average altitude of about 12 km. This is where most weather phenomena occur and where temperature generally decreases with increasing altitude.
On average, temperature decreases with height in the troposphere. The troposphere is bounded by the earth's surface and the tropopause (located at about 150 millibars in the tropics and 300 mb at high latitudes). In the troposphere on any given day, there are various layers between the surface and the tropopause where the lapse rates are far from average (the average environmental lapse rate is near 6.5 degrees C/km). Rawinsonde weather balloons measure temperature as they rise (this is the plot of the environmental lapse rate). Under certain conditions, the lapse rate in the atmosphere (defined as the change in temperature with height) is much above or much below normal.
A graph showing a negative correlation between elevation above sea level and average annual temperature would best represent the general effect. As altitude increases, temperatures typically decrease in the troposphere due to lower air pressure and the lapse rate. This relationship is commonly observed in mountainous regions.
The temperature in the troposphere can vary depending on factors such as altitude and location, but on average it decreases by about 6.5 degrees Celsius per kilometer of altitude. Near the Earth's surface, the average temperature of the troposphere is around 15 degrees Celsius.
The average temperature drops by about 3.5F per 1000 feet of elevation gain.
The troposphere is typically colder as you go higher in altitude. On average, the temperature decreases by about 6.5°C for every kilometer increase in altitude within the troposphere.
Temperature decreases as altitude increases in the troposphere
In the troposphere, temperature generally decreases with increasing altitude at a rate of around 6.5°C per kilometer due to the adiabatic cooling effect as air pressure decreases with height. This relationship is known as the environmental lapse rate and defines the temperature profile of the troposphere.
The troposphere is the layer of the atmosphere that extends to an average altitude of about 12 km. This is where most weather phenomena occur and where temperature generally decreases with increasing altitude.
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.
At 15,000 feet elevation, the air temperature can vary widely depending on multiple factors such as the time of day, season, and location. However, on average, the temperature at this elevation tends to be around 40-50 degrees Fahrenheit colder than at sea level.
On average, temperature decreases with height in the troposphere. The troposphere is bounded by the earth's surface and the tropopause (located at about 150 millibars in the tropics and 300 mb at high latitudes). In the troposphere on any given day, there are various layers between the surface and the tropopause where the lapse rates are far from average (the average environmental lapse rate is near 6.5 degrees C/km). Rawinsonde weather balloons measure temperature as they rise (this is the plot of the environmental lapse rate). Under certain conditions, the lapse rate in the atmosphere (defined as the change in temperature with height) is much above or much below normal.
The average annual temperature in Swaziland is around 68°F (20°C). It experiences mild temperatures throughout the year due to its elevation and proximity to the coast.
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.