Vertical structure of stratospheric water vapour trends derived from merged satellite data

Hegglin, M. I., Plummer, D. A., Shepherd, T. G., Scinocca, J. F., Anderson, J., Froidevaux, L., Funke, B., Hurst, D., Rozanov, A., Urban, J., von Clarmann, T., Walker, K. A., Wang, H. J., Tegtmeier, Susann and Weigel, K. (2014) Vertical structure of stratospheric water vapour trends derived from merged satellite data Nature Geoscience, 7 (10). pp. 768-776. DOI 10.1038/NGEO2236.

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Abstract

Stratospheric water vapour is a powerful greenhouse gas. The longest available record from balloon observations over Boulder, Colorado, USA shows increases in stratospheric water vapour concentrations that cannot be fully explained by observed changes in the main drivers, tropical tropopause temperatures and methane. Satellite observations could help resolve the issue, but constructing a reliable long-term data record from individual short satellite records is challenging. Here we present an approach to merge satellite data sets with the help of a chemistry-climate model nudged to observed meteorology. We use the models' water vapour as a transfer function between data sets that overcomes issues arising from instrument drift and short overlap periods. In the lower stratosphere, our water vapour record extends back to 1988 and water vapour concentrations largely follow tropical tropopause temperatures. Lower and mid-stratospheric long-term trends are negative, and the trends from Boulder are shown not to be globally representative. In the upper stratosphere, our record extends back to 1986 and shows positive long-term trends. The altitudinal differences in the trends are explained by methane oxidation together with a strengthened lower-stratospheric and a weakened upper-stratospheric circulation inferred by this analysis. Our results call into question previous estimates of surface radiative forcing based on presumed global long-term increases in water vapour concentrations in the lower stratosphere.

Document Type: Article
Additional Information: WOS:000343112600024
Keywords: TROPICAL TROPOPAUSE LAYER; TEMPERATURE TRENDS; UPPER TROPOSPHERE; ERA-INTERIM; VARIABILITY; DEHYDRATION; VALIDATION; ATMOSPHERE; HYGROMETER; EXTENSION
Research affiliation: OceanRep > GEOMAR > FB1 Ocean Circulation and Climate Dynamics > FB1-ME Maritime Meteorology
OceanRep > The Future Ocean - Cluster of Excellence
Refereed: Yes
DOI etc.: 10.1038/NGEO2236
ISSN: 1752-0894
Projects: CMAM30, Future Ocean
Date Deposited: 13 Nov 2014 08:29
Last Modified: 20 Feb 2017 14:11
URI: http://eprints.uni-kiel.de/id/eprint/26022

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