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Tropopause
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The '''tropopause''' is a boundary region in the
Earth's atmosphere atmosphere between the
troposphere and the
stratosphere.
The troposphere is the lowest of the Earth's atmospheric layers and is the layer in which all of what we call "
weather" occurs. It begins at ground level and ranges in height from an average of 6 km (4 miles) at the poles to 17 km (11 miles) at the equator. At the equator, the stratosphere begins at roughly 17 km (11 miles) in altitude, and it may reach as high as 50 km (31 miles) from the earth's surface. This is also the location of the
ozone layer. It is at its highest level over the
equator and the lowest over the geographical
north north pole and
south south pole poles. On account of this, the coolest layer in the atmosphere lies at about 17 km over the equator. There are two types of tropopauses, viz. equatorial tropopause, and polar tropopause.
Measuring the
adiabatic lapse rate lapse rate through the troposphere and the stratosphere identifies the location of the tropopause. In the troposphere, the lapse rate is, on average, 6.5 °C per kilometre. That is to say, for every kilometre in height, the
temperature drops by 6.5 degrees Celsius. In the stratosphere, however, the temperature increases with altitude. The region of the atmosphere where the lapse rate changes from positive (in the troposphere) to negative (in the stratosphere), ie, where the temperature no longer decreases with altitude but rather increases, is defined as the tropopause. The exact definition used by the
World Meteorological Organization is:
:the lowest level at which the lapse rate decreases to 2 °C/km or less, provided that the average lapse rate between this level and all higher levels within 2 km does not exceed 2 °C/km.
Alternatively, a dynamic definition of the tropopause is used with potential vorticity instead of vertical temperature gradient as the defining variable. There is no universally used threshold: the most common ones are: the tropopause lies at the 2 PVU or 1.5 PVU surface. PVU stands for ''
PVU potential vorticity unit''.
The tropopause is not a "hard" boundary. Vigorous
thunderstorm thunderstorms, for example, particularly those of tropical origin, will
convective overshoot overshoot into the lower stratosphere and undergo a brief (hour-order) low-frequency vertical
oscillation. Such oscillation sets up a low-frequency atmospheric
wave train capable of affecting both atmospheric and oceanic currents in the region.
{{earthsatmosphere}}
Category:Atmosphere
de:Tropopause
es:Tropopausa
fr:Tropopause
ko:대류권 계면
he:טרופופ×?וזה
ms:Tropopaus
nl:Tropopauze
pt:Tropopausa
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