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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
  • Where Is the Tropopause? - Tropopause Altitude and Other Characteristics
    The tropopause is a boundary layer in the atmosphere that separates the troposphere from the stratosphere The troposphere is the part of our atmosphere where most meteorological phenomena occur, whereas the stratosphere is a more stable and less turbulent region
  • 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
  • What is TROPO in Aviation? (Tropopause) - Aviation Terms
    Understanding the characteristics and significance of the Tropopause is fundamental for safe and efficient aviation operations The Tropopause is the atmospheric boundary where the temperature lapse rate—meaning the rate at which temperature decreases with altitude—suddenly changes
  • Tropopause - SKYbrary Aviation Safety
    The tropopause is the upper limit of the troposphere and therefore constitutes the boundary between it and the Stratosphere
  • Tropopause Essentials in Meteorology - numberanalytics. com
    The tropopause is a critical component of the Earth's atmosphere, playing a vital role in shaping our weather and climate As the boundary between the troposphere and the stratosphere, the tropopause is a complex and dynamic region that has significant implications for meteorological studies
  • Tropopause - NOAAs National Weather Service - Glossary
    Type of jet stream found near the tropopause Examples of this type of jet are the subtropical and polar fronts You can either type in the word you are looking for in the box below or browse by letter Search: Browse by letter:
  • A Modern Approach to a Stability-Based Definition of the Tropopause
    In this study we provide a review of existing tropopause definitions (and their limitations) and investigate potential improvement in the definition of the tropopause using balloon-based observations of stability and atmospheric composition
  • Tropopause - (Intro to Climate Science) - Vocab, Definition . . .
    The tropopause is the boundary layer between the troposphere and the stratosphere in the Earth's atmosphere It plays a critical role in atmospheric dynamics, acting as a cap that limits the vertical mixing of air and weather phenomena, while also marking a significant change in temperature gradient and atmospheric pressure





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