NASA NTRS · 19800065049
Stratospheric H2O
Abstract
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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Ellsaesser, H. W., Harries, J. E., Kley, D., Penndorf, R.. 1980-08-01. Stratospheric H2O. https://ntrs.nasa.gov/citations/19800065049
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