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Water‐vapor climate feedback inferred from climate fluctuations, 2003–2008

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Dessler, A. E., Zhang, Z., Yang, P.·2008·Geophysical Research Letters

Abstract

Between 2003 and 2008, the global‐average surface temperature of the Earth varied by 0.6°C. We analyze here the response of tropospheric water vapor to these variations. Height‐resolved measurements of specific humidity (q) and relative humidity (RH) are obtained from NASA's satellite‐borne Atmospheric Infrared Sounder (AIRS). Over most of the troposphere, q increased with increasing global‐average surface temperature, although some regions showed the opposite response. RH increased in some regions and decreased in others, with the global average remaining nearly constant at most altitudes. The water‐vapor feedback implied by these observations is strongly positive, with an average magnitude of λq = 2.04 W/m 2/K, similar to that simulated by climate models. The magnitude is similar to that obtained if the atmosphere maintained constant RH everywhere.

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Metadata

Authors
Dessler, A. E., Zhang, Z., & Yang, P.
Venue
Geophysical Research Letters
Published
2008-10
Volume
35
Issue
20
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W1977564923
Cited by
268
References
20
FWCI
9.40
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: Water‐vapor climate feedback inferred from climate fluctuations, 2003–2008. https://app.cochat.ai/papers/10.1029/2008gl035333
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Dessler, A. E., Zhang, Z., & Yang, P. (2008). Water‐vapor climate feedback inferred from climate fluctuations, 2003–2008. Geophysical Research Letters. https://doi.org/10.1029/2008gl035333

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