From Simple English Wikipedia, the free encyclopedia

The stratopause is the part of the atmosphere between the stratosphere and mesosphere. In the stratosphere the temperature gets higher the higher up you go. The stratopause is where it is warmest. On Earth, the stratopause is about 50 kilometres (31 mi) high. The temperature is about −15 °C (5 °F).[1][2][3]

References[change | change source]

  1. "What is the Stratopause". Retrieved 2017-05-22.
  2. "stratopause | meteorology". Encyclopedia Britannica. Retrieved 2017-05-22.
  3. Philander, S. George (2012-06-13). Encyclopedia of Global Warming and Climate Change, Second Edition. SAGE Publications. ISBN 978-1-4129-9262-6.