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Mezopauza

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Mezopauza to cienka izotermiczna warstwa atmosfery ziemskiej, znajdująca się na wysokości 80–90 km i oddzielająca mezosferę od leżącej wyżej termosfery[1]. W mezopauzie temperatura powietrza wynosi około −100 °C, a ciśnienie około 0,1 hPa. Mezopauza jest związana z występowaniem zórz polarnych w wyższych szerokościach geograficznych[2].

Przypisy

  1. Rafael Escribano Torres (ed.): Spectroscopy of the Atmospheres. Editorial CSIC - CSIC Press, 2010, s. 20-21, seria: Madrid: Consejo Superior de Investigaciones Científicas. ISBN 978-84-00-09219-1. (ang.).
  2. Encyklopedia Britannica. Ziemia i Wszechświat. Poznań: Wydawnictwo KURPISZ S>A., 2006, s. 91. ISBN 978-83-60563-25-0.
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Mezopauza
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