tropopause वाक्य
उदाहरण वाक्य
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- Airliners typically fly at an altitude ranging from 10 km to 15 km, at the tropopause.
- They found that changes in potential vorticity at the tropopause can cause changes in the wind field.
- Measuring the temperature change with height through the troposphere and the stratosphere identifies the location of the tropopause.
- The upper circulation of strong hurricanes extends into the tropopause of the atmosphere, which at low latitudes is.
- All air entering the stratosphere must pass through the tropopause, the temperature minimum that divides the troposphere and stratosphere.
- The atmospheric region most susceptible to CAT is the high troposphere at altitudes of around as it meets the tropopause.
- Because fronts are three-dimensional phenomena, frontal shear can be observed at any altitude between surface and tropopause.
- The clouds are located in the tropopause and are arranged into bands of different latitudes, known as tropical regions.
- The tropopause lowers the further towards the pole you go in general and you have higher stratospheric potential vorticity poleward.
- Thus, the tropopause is an inversion layer, and there is little mixing between the two layers of the atmosphere.
- The result is a wind which increases with altitude through the tropopause and upward to 100, 000 feet or above.
- However, prior to 2000, increases in average Western Pacific SSTs had resulted in increases in tropopause cold point temperatures.
- The tropopause is an inversion layer, where the air temperature ceases to decrease with height and remains constant through its thickness.
- Due to the variation in starting height, the tropopause extremes are referred to as the equatorial tropopause and the polar tropopause.
- Due to the variation in starting height, the tropopause extremes are referred to as the equatorial tropopause and the polar tropopause.
- Due to the variation in starting height, the tropopause extremes are referred to as the equatorial tropopause and the polar tropopause.
- Typically, radiative forcing is quantified at the tropopause in units of watts per square meter of the Earth's surface.
- Where air density is significantly different, for instance because of temperature gradient, especially at the tropopause, CAT can occur.
- This is why temperatures at the top of the troposphere ( known as the tropopause ) are about-50 degrees Celsius.
- On comparatively rare occasions, convective lift can be powerful enough to penetrate the tropopause and push the cloud top into the stratosphere.
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