The stratosphere is normally considered to extend from about 11 km to 50 km above the earth's surface (7 - 31 miles).
The stratosphere can vary in thickness depending on altitude, but on average, it can range from about 8 to 50 kilometers (5 to 31 miles) deep. The stratopause, which is the boundary between the stratosphere and the mesosphere, is typically around 50 kilometers above the Earth's surface.
In the stratosphere, the temperature increases with height. This is due to the presence of the ozone layer near the top of the stratosphere. The ozone layer absorbs incoming UV radiation, and thus the temperatures are warmer at the top of the stratosphere than at the bottom.
As you move from the troposphere (closest to the surface) to the stratosphere, temperature generally decreases with altitude due to the decreasing density of the air. In the stratosphere, temperature starts to increase with altitude due to the absorption of solar radiation by ozone. Overall, the trend is a decrease in temperature with altitude in the troposphere and an increase in temperature with altitude in the stratosphere.
Temperature reaches its coldest at the tropopause, which is the boundary between the troposphere below and the stratosphere above. In the stratosphere, the temperature increases with height due to absorption of radiation by ozone.Temperature changes when altitude is in the stratosphere because of one things. It already rises when you climb up in the stratosphere.
the temperature already rise as you climb up in the stratosphere.
The pressure in the stratosphere ranges from about 100 to 1 millibar. This corresponds to an altitude range of approximately 10 to 50 kilometers above sea level.
The temperature in the stratosphere typically ranges from about -15°C to 0°C. However, this temperature range can vary depending on location, altitude, and other atmospheric conditions.
The stratosphere's temperature increases as altitude increases. The mesosphere's temperature decreases as it's altitude increases. This is helpful
The stratosphere can vary in thickness depending on altitude, but on average, it can range from about 8 to 50 kilometers (5 to 31 miles) deep. The stratopause, which is the boundary between the stratosphere and the mesosphere, is typically around 50 kilometers above the Earth's surface.
Ozone sets in stratosphere. The altitude of it is 28 km.
The stratosphere is the layer above the troposphere (where we live). The ozone layer is found in the lower stratosphere. The stratosphere is the lowest layer where temperature increases with increasing altitude.
In the stratosphere, the temperature increases with height. This is due to the presence of the ozone layer near the top of the stratosphere. The ozone layer absorbs incoming UV radiation, and thus the temperatures are warmer at the top of the stratosphere than at the bottom.
As you move from the troposphere (closest to the surface) to the stratosphere, temperature generally decreases with altitude due to the decreasing density of the air. In the stratosphere, temperature starts to increase with altitude due to the absorption of solar radiation by ozone. Overall, the trend is a decrease in temperature with altitude in the troposphere and an increase in temperature with altitude in the stratosphere.
the stratosphere is about 25-50 km in altitude
The altitude rises.
Temperature reaches its coldest at the tropopause, which is the boundary between the troposphere below and the stratosphere above. In the stratosphere, the temperature increases with height due to absorption of radiation by ozone.Temperature changes when altitude is in the stratosphere because of one things. It already rises when you climb up in the stratosphere.
stratosphere and thermosephere -Nikki Gallagher