BEACON eSpace at Jet Propulsion Laboratory >
JPL Technical Report Server >
JPL TRS 1992+ >
Please use this identifier to cite or link to this item:
|Title: ||ATMOS Stratospheric Deuterated Water and Implications for Troposphere-Stratosphere Transport|
|Authors: ||Moyer, E. J.|
Irion, F. W.
Yung, Y. L.
Gunson, M. R.
|Issue Date: ||1996 |
|Abstract: ||The isotopic composition of stratospheric water vapor is used as a tracer for the convective history of air injected into the stratosphere. Stratospheric profiles of HDO, H<sub>2</sub>O,CH<sub>3</sub>D, and CH<sub>4</sub> fro the ATMOS instrument, obtained over four missions from 1985-1994, are used to determine the initial deuterium-to-hydrogen ration of water vapor entering the stratosphere. We find that the initial DeltaD of stratospheric water is - 680 ± 80 (68 percent loss of deuterium), consistent with extrapolations from previous measurements at higher altitudes.|
|Appears in Collections:||JPL TRS 1992+|
Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.