Stratospheric H2O

Details Stratospheric H2O Stratospheric H2O

Aug 1980

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980p%26ss...28..827e&link_type=abstract

Planetary and Space Science, vol. 28, Aug. 1980, p. 827-835. Research supported by the Department of Industry of England, Manuf

Mathematics

Logic

6

Atmospheric Moisture, Stratosphere, Water Vapor, Atmospheric Circulation, Atmospheric Temperature, Long Term Effects, Mesosphere

Scientific paper

The present state of our knowledge and understanding of H2O in the stratosphere is reviewed. This reveals continuing discrepancies between observations and expectations following from the Brewer-Dobson hypothesis of stratospheric circulation. In particular, available observations indicate unexplained upward and poleward directed H2O gradients immediately downstream from the tropical tropopause and variable vertical gradients above 20 km which generally disagree with those expected from oxidation of CH4.

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