Assimilation of N2O in the Upper Atmosphere Using a Kalman Filter: N2O Mixing Ratio

  • Released Friday, March 22, 1996
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This series of animations shows assimilation of N2O in the upper atmosphere using observations from the Cryogenic Limb Etalon Spectrometer (CLAES) on the Upper Atmosphere Research Satellite (UARS). Winds were provided by the Goddard EOS Data Assimilation System (GEOS-DAS). Flow is at the 850K isentropic level. N2O mixing ratio is expressed in parts per billion volume (ppbv).



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NASA/Goddard Space Flight Center
Scientific Visualization Studio

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This page was originally published on Friday, March 22, 1996.
This page was last updated on Wednesday, May 3, 2023 at 2:00 PM EDT.


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