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| Titel |
The magnitudes and timescales of global mean surface temperature feedbacks in climate models |
| VerfasserIn |
A. Jarvis |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
2190-4979
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| Digitales Dokument |
URL |
| Erschienen |
In: Earth System Dynamics ; 2, no. 2 ; Nr. 2, no. 2 (2011-12-15), S.213-221 |
| Datensatznummer |
250000606
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| Publikation (Nr.) |
 copernicus.org/esd-2-213-2011.pdf |
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| Zusammenfassung |
| Because of the fundamental role feedbacks play in determining the response
of surface temperature to perturbations in radiative forcing, it is
important we understand the dynamic characteristics of these feedbacks.
Rather than attribute the aggregate surface temperature feedback to
particular physical processes, this paper adopts a linear systems approach
to investigate the partitioning with respect to the timescale of the
feedbacks regulating global mean surface temperature in climate models. The
analysis reveals that there is a dominant net negative feedback realised on
an annual timescale and that this is partially attenuated by a spectrum of
positive feedbacks with characteristic timescales in the range 10 to 1000 yr. This attenuation was composed of two discrete phases which are
attributed to the equilibration of "diffusive – mixed layer" and
"circulatory – deep ocean" ocean heat uptake. The diffusive equilibration
was associated with time constants on the decadal timescale and accounted
for approximately 75 to 80 percent of the overall ocean heat feedback,
whilst the circulatory equilibration operated on a centennial timescale and
accounted for the remaining 20 to 25 percent of the response. This suggests
that the dynamics of the transient ocean heat uptake feedback first
discussed by Baker and Roe (2009) tends to be dominated by loss of diffusive
heat uptake in climate models, rather than circulatory deep ocean heat
equilibration. |
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