Dynamic Processes Governing Lower-Tropospheric HDO/H 2 O Ratios as Observed from Space and Ground

Author:

Frankenberg Christian1,Yoshimura Kei2,Warneke Thorsten3,Aben Ilse1,Butz André1,Deutscher Nicholas4,Griffith David4,Hase Frank5,Notholt Justus3,Schneider Matthias5,Schrijver Hans1,Röckmann Thomas6

Affiliation:

1. SRON-Netherlands Institute for Space Research, Sorbonnelaan 2, 3584CA Utrecht, Netherlands.

2. Scripps Institution of Oceanography, University of California, La Jolla, CA 92093, USA.

3. Institute of Environmental Physics, Otto-Hahn-Allee 1, Bremen, 28359, Germany.

4. School of Chemistry, University of Wollongong, Wollongong, Australia.

5. Institute for Meteorology and Climate Research, IMK-ASF Karlsruhe, Germany.

6. Institute for Marine and Atmospheric Research Utrecht, Princetonplein 5, Utrecht, 3584 CC, Netherlands.

Abstract

Cycling Around Water vapor is the most important greenhouse gas, and clouds are one of the most important components of climate, but the global hydrological cycle is still poorly-enough understood that the atmospheric cycling of water and cloud formation are inadequately represented in global climate models. As the transformation from liquid into vapor tends to deplete water of the isotope deuterium, Frankenburg et al. (p. 1374 ) were able to use satellite measurements of global “heavy” water abundances to provide a deeper understanding of atmospheric water dynamics.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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