First observed by World War II pilots, they develop just below the tropopause over areas of steep pressure gradient on the surface.
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In the upper troposphere the tropopause slants downward the further north in latitude and there is more high potential vorticity stratospheric air northward.
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In general, winds are strongest immediately under the tropopause ( except locally, during tornadoes, tropical cyclones or other anomalous situations ).
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Although the temperature may be at the tropopause, the top of the stratosphere is much warmer, and may be near 0 �C.
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The decreased water content is a result of a lower tropopause within the vortex, which places dry stratospheric air above moist tropospheric air.
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By dropping the extra ballast just before entering the tropopause, the crew hopes to speed up the balloon's ascent to safer altitudes.
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On Earth, the main jet streams are located near the altitude of the tropopause and are westerly winds ( flowing west to east ).
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Because the temperature in the tropopause and lower stratosphere is largely constant with increasing altitude, very little convection and its resultant turbulence occurs there.
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After reaching the tropopause, the bottom of the region of strong static stability, the cloud tends to slow its ascent and spread out.
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The Great Dark Spot generated large white clouds at or just below the tropopause layer similar to high-altitude cirrus clouds found on Earth.