| 31. | The result is a wind which increases with altitude through the tropopause and upward to 100, 000 feet or above.
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| 32. | However, prior to 2000, increases in average Western Pacific SSTs had resulted in increases in tropopause cold point temperatures.
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| 33. | The tropopause is an inversion layer, where the air temperature ceases to decrease with height and remains constant through its thickness.
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| 34. | Due to the variation in starting height, the tropopause extremes are referred to as the equatorial tropopause and the polar tropopause.
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| 35. | Due to the variation in starting height, the tropopause extremes are referred to as the equatorial tropopause and the polar tropopause.
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| 36. | Due to the variation in starting height, the tropopause extremes are referred to as the equatorial tropopause and the polar tropopause.
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| 37. | Typically, radiative forcing is quantified at the tropopause in units of watts per square meter of the Earth's surface.
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| 38. | Where air density is significantly different, for instance because of temperature gradient, especially at the tropopause, CAT can occur.
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| 39. | This is why temperatures at the top of the troposphere ( known as the tropopause ) are about-50 degrees Celsius.
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| 40. | 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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