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017 _ _ |a The definitive version is available at http://dx.doi.org/10.1016/j.jastp.2006.05.021 .
024 7 _ |a 10.1016/j.jastp.2006.05.021
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041 _ _ |a eng
082 _ _ |a 530
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|a Geochemistry & Geophysics
084 _ _ |2 WoS
|a Meteorology & Atmospheric Sciences
100 1 _ |a Riese, M.
|b 0
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245 _ _ |a Long-term changes of hydrogen-containing species in the stratosphere
260 _ _ |a Amsterdam [u.a.]
|b Elsevier Science
|c 2006
300 _ _ |a 1973 - 1979
336 7 _ |a Journal Article
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440 _ 0 |a Journal of Atmospheric and Solar-Terrestrial Physics
|x 1364-6826
|0 14744
|y 17
|v 68
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a Understanding the 1% per year increase of stratospheric water vapour from 1954 to 2000 is a great challenge in atmospheric science. The increase is predominantly caused by long-term changes in transport of water vapour into the stratosphere and systematic increases of tropospheric methane levels. This paper gives a review on stratospheric water vapour changes for the 1980 and 2000 time period with emphasis on the contribution of methane oxidation. Predictions for 2050 indicate that likely increases of tropospheric methane levels will lead to an increase of upper stratospheric water vapour values of about 0.4 ppmv. A similar value is predicted as an upper limit of effects of a future hydrogen economy. (c) 2006 Elsevier Ltd. All rights reserved.
536 _ _ |a Atmosphäre und Klima
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653 2 0 |2 Author
|a stratospheric water vapour
653 2 0 |2 Author
|a methane trend
653 2 0 |2 Author
|a hydrogen economy
700 1 _ |a Grooß, J.-U.
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700 1 _ |a Feck, T.
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700 1 _ |a Rohs, S.
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773 _ _ |a 10.1016/j.jastp.2006.05.021
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|x 1364-6826
856 7 _ |u http://dx.doi.org/10.1016/j.jastp.2006.05.021
|u http://hdl.handle.net/2128/651
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