u can reach the maximum height of ur body by exercising ur body with pull-ups everyday........,if u havent even taken 3 cm during 3 months u wont go longer..,u have already reached the maximum height
The temperature is relatively constant in the tropopause, remaining around -60°C to -80°C throughout its height. This stable temperature profile forms a boundary separating the troposphere below from the stratosphere above.
The standard temperature lapse rate or environmental lapse rate as it is more commonly known is basically the temperature difference between the tropopause surface divided by height. This uses the formula -dT/dz and essentially shows the temperature decreasing as the height above the tropopause increases.
The tropopause is the boundary between the troposphere (the lowest layer of Earth's atmosphere where most weather occurs) and the stratosphere (the layer above the troposphere where the ozone layer is located). This boundary is characterized by a change in temperature and is found at an average height of about 8-15 kilometers above the Earth's surface.
In the troposphere, temperature generally decreases with increasing altitude at a rate of about 6.5°C per kilometer due to the decrease in air pressure and density with height, known as the lapse rate. This trend continues until the tropopause, where the temperature stabilizes.
The tropopause is the boundary between the troposphere and the stratosphere. Its height asl varies with latitude (highest near the equator). 12-15 km approx.
what is the approximate height and temperature of the troposphere, stratosphere, mesosphere, and thermosphere?
The height of the tropopause typically ranges from 8 to 18 kilometers above the Earth's surface. The temperature at the tropopause is around -60 degrees Celsius on average, but this can vary depending on the location and season.
The temperature is relatively constant in the tropopause, remaining around -60°C to -80°C throughout its height. This stable temperature profile forms a boundary separating the troposphere below from the stratosphere above.
The approximate height of the stratopause is between 50 to 55 km. The temperature is about negative15 degrees Celsius or 5 degrees Fahrenheit.
The standard temperature lapse rate or environmental lapse rate as it is more commonly known is basically the temperature difference between the tropopause surface divided by height. This uses the formula -dT/dz and essentially shows the temperature decreasing as the height above the tropopause increases.
The height of the Tropopause depends mainly on the Latitude. At the Poles, it is about 30,000' and at the equator it is about 60,000. This number varies with a change in temperature/season. It is higher at the equator due to a naturally higher temperature at sea level, this means the parcel of air has a lower density. Because of the lower density the parcel of air will be more 'stretched out' than the air at the poles (the colder parcel of air with a higher density).
Jet streams are fast flowing, narrow air currents found at the tropopause, the transition between the troposphere (where temperature decreases with height) and the stratosphere (where temperature increases with height) and are located at 10-15 kilometers above the surface of the Earth. They form near boundaries of adjacent air masses with significant differences in temperature
The tropopause is the boundary between the troposphere (the lowest layer of Earth's atmosphere where most weather occurs) and the stratosphere (the layer above the troposphere where the ozone layer is located). This boundary is characterized by a change in temperature and is found at an average height of about 8-15 kilometers above the Earth's surface.
It really depends at what latitude the flight is operating. The lowest layer of the atmosphere, the troposphere, extends up to an altitude of about 23,000 feet (7km) at the poles, and an altitude of about 60,000 feet (17km) at the equator. Therefore, at the poles the aircraft would be flying above the troposhere, in the stratosphere. At the equator, though, the airplane would still be in the troposphere. As you go north or south from the equator, the maximum height of the troposhere (known as the tropopause) generally decreases from 17km to 7km. However, there are notable 'step' changes in the height of the tropopause, where there is a large change in temperature. This causes the high speed winds known as jetstreams, which aeroplanes use to improve journey times. At any location, the height of the tropopause (i.e. depth of the troposphere) is a function of temperature and air pressure/density. As it is warmer and pressure is lower at the equator, the tropopause is higher here than at the poles.
In the troposphere, temperature generally decreases with increasing altitude at a rate of about 6.5°C per kilometer due to the decrease in air pressure and density with height, known as the lapse rate. This trend continues until the tropopause, where the temperature stabilizes.
The tropopause is the boundary between the troposphere and the stratosphere. Its height asl varies with latitude (highest near the equator). 12-15 km approx.
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