tropopause's Usage Examples:

The border between the troposphere and stratosphere, the tropopause, marks where this temperature inversion begins.

Atop the troposphere is the tropopause, which is the border between the troposphere and stratosphere.

The tropopause is an inversion layer, where the.

The tropopause is the boundary in the Earth's atmosphere between the troposphere and the stratosphere.

altitudes of around 7,000–12,000 metres (23,000–39,000 ft) as it meets the tropopause.

convective layer (FCL) and reaching the equilibrium level (EL), near the tropopause.

This level is often near the tropopause and can be indicated as near where the anvil of a thunderstorm because.

On Earth, the main jet streams are located near the altitude of the tropopause and are westerly winds (flowing west to east).

Higher than the troposphere, at the tropopause, the temperature is approximately constant with altitude (up to ~20 km).

temperature is approximately constant; this layer is called the tropopause.

The troposphere and tropopause together consist of ~99% of the atmospheric CO2.

cumulonimbus cloud that is capable of precipitation but has not yet reached the tropopause, which is the height of stratospheric stability at which cumulonimbus.

in the sense that they are maintained by subsidence warming near the tropopause which balances radiational cooling.

rear component of the pressure seal in all aircraft that cruise in a tropopause zone in the earth's atmosphere.

It lies above the troposphere and is separated from it by the tropopause.

kilometers of height where the lapse rate reaches zero, known today as the tropopause.

surface of the Earth to about 11 km (7 mi) into the atmosphere where the tropopause (the boundary between the troposphere stratosphere) is located.

{\textstyle \tau _{\text{tp}}} , in the tropopause, which is determined by the temperature and pressure at the tropopause according to the saturation vapor.

There is no tropopause in the jet standard atmosphere.

In the ISA, the tropopause is the height at which the temperature stops.

attention given to all processes extending from the earth surface to the tropopause, but special emphasis continues to be devoted to the physics of clouds.

6 mi) per month until they are dissipated at the tropical tropopause.

This point of equilibrium is often marked by the tropopause.

Synonyms:

troposphere; layer;

Antonyms:

natural object;