Examples of 'tropopause' in a sentence
Meaning of "tropopause"
Tropopause is the boundary in the Earth's atmosphere between the troposphere and the stratosphere, characterized by the transition from decreasing to increasing temperatures with altitude
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- The zone of transition between the troposphere and the stratosphere (approximately 13 kilometers). The tropopause normally occurs at an altitude of between 25,000 and 45,000 feet in polar and temperate zones. It occurs at 55,000 feet in the tropics.
How to use "tropopause" in a sentence
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tropopause
The tropopause is characterized by a strong temperature inversion.
Its upper limit is called the tropopause.
The tropopause is not continuous but.
This point of equilibrium is often marked by the tropopause.
It is also possible to define the tropopause in terms of chemical composition.
Barometric readings indicate a rising tropopause.
Tropopause penetrations by cumulonimbus clouds.
At this height it is called the tropopause.
The tropopause is the boundary between the troposphere and stratosphere.
Forcing is defined as the radiative imbalance at the tropopause.
Fluctuation of the tropopause height.
This region of constant temperature is known as the tropopause.
Tropopause folding event.
There would probably not be a tropopause.
Tropopause vertical windshear.
See also
This freezing layer of dry air is called the tropopause.
It also follows that the tropopause is higher in summer than in winter.
The additional levels are in the stratosphere and at the tropopause.
The atmospheric layer between the tropopause and the stratopause.
The boundary between the two layers is called the tropopause.
This water is often above the tropopause where little water usually reaches.
This is generally in the tropopause.
The tropopause is the atmospheric boundary between the troposphere and the stratosphere.
It reaches the tropopause.
The tropopause marks the limit of the troposphere and the beginning of the stratosphere.
Standing waves normally do not extend above the tropopause at temperate latitudes.
A lower tropopause restricts the available space for free movement of air horizontally beneath it.
Warm air rises from the equator and hits the tropopause.
The mixing layerformation over the tropopause and seasonal chemical variations are shown.
Jet streams occur where there is an abrupt change in the height of the tropopause.
B The layer between the tropopause and the stratosphere.
The first surprise from the flights was the extremely low temperature of the tropopause.
Tropopause The atmospheric layer separating the troposphere and stratosphere.
The additional levels are set mainly in the boundary layer and near the tropopause.
Tropopause warming, and the humidification of the stratosphere.
The heat energy creates powerful rising air currents that swirl upwards to the tropopause.
Above the tropopause is the stratosphere, where the atmospheric churning stops.
There exist a thin buffer zone between the troposphere and next layer known as tropopause.
Nevertheless, the dynamic tropopause is useless at equatorial latitudes because the isentropes are almost vertical.
Right at the ceiling just below the Tropopause.
The altitude of the tropopause varies with latitude and season of the year . ”.
It is the most cloudy layer and reaches up to the Tropopause.
Is the tropopause higher or lower at the Equator than at the poles? 17.
We will acquire enough speed Ascend up to the Tropopause.
Tropopause = = = The tropopause is the boundary region between the troposphere and the stratosphere.
Ascend up to the Tropopause.
T1620 Tropopause chart Chart showing the distribution of tropopause heights.
Which letter marks the approximate location of the tropopause surface?
FRAME, 346 The tropopause altitude near a jet stream changes abruptly.
A jet stream is a shallow, twisting river of maximum winds, near the tropopause.
