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tropopause    音标拼音: [tr'ɑpəp,ɔz]


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  • Tropopause - Wikipedia
    The tropopause is the atmospheric boundary that demarcates the lowest two layers of the atmosphere of Earth – the troposphere and stratosphere – which occurs approximately 17 kilometres (11 mi) above the equatorial regions, and approximately 9 kilometres (5 6 mi) above the polar regions
  • Layers of the Atmosphere - National Oceanic and Atmospheric Administration
    The transition layer at the bottom of the stratosphere is called the tropopause Known as the lower atmosphere, almost all weather occurs in this region The troposphere begins at the Earth's surface, but the height of the troposphere varies
  • Tropopause - an overview | ScienceDirect Topics
    In the tropics, the tropopause is generally located at higher altitudes than in polar regions; the height of the tropopause depends on the season and is affected by weather conditions in the troposphere
  • Tropopause - SKYbrary Aviation Safety
    The tropopause is the upper limit of the troposphere and therefore constitutes the boundary between it and the Stratosphere
  • Tropopause | atmospheric region | Britannica
    One such layer is the tropopause, the boundary between the relatively dry stratosphere and the more meteorologically active layer below This is often the region of the jet streams
  • What Is the Tropopause and Why Is It Important?
    The tropopause is not a hard physical line, but a boundary layer where atmospheric properties shift abruptly It marks the upper limit of the troposphere, where all terrestrial weather occurs, and the beginning of the stratosphere
  • What is the Tropopause? (with pictures) - AllTheScience
    What is the Tropopause? The tropopause is a thin layer of the Earth's atmosphere that separates the lower troposphere and the higher stratosphere At the poles, it is roughly 36,000 feet (1,100 meters) above sea level, and increases to 58,000 feet (1,700m) around the equator
  • Flirting with the tropopause - Air Facts Journal
    The first pause is the tropopause, dividing the troposphere and stratosphere There, jet streams corkscrew the globe like atmospheric snakes (think meandering air currents with extraordinary velocity), and create turbulence
  • OVER AND BEYOND - Federal Aviation Administration
    A cross section of the upper troposphere and lower stratosphere showing the tropopause and associated fea tures Note the "break" between the high tropical and the lower polar tropopause





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