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Titel |
Set-up and preliminary results of mid-Pliocene climate simulations with CAM3.1 |
VerfasserIn |
Q. Yan, Z. S. Zhang, H. J. Wang, Y. Q. Gao, W. P. Zheng |
Medientyp |
Artikel
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Sprache |
Englisch
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ISSN |
1991-959X
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Digitales Dokument |
URL |
Erschienen |
In: Geoscientific Model Development ; 5, no. 2 ; Nr. 5, no. 2 (2012-03-09), S.289-297 |
Datensatznummer |
250002442
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Publikation (Nr.) |
copernicus.org/gmd-5-289-2012.pdf |
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Zusammenfassung |
The mid-Pliocene warm period ~3.264 to 3.025 Ma) is a
potential analogue for future climate under global warming. In this study,
we use an atmospheric general circulation model (AGCM) called CAM3.1 to
simulate the mid-Pliocene climate with the PRISM3D boundary conditions. The
simulations show that the global annual mean surface air temperature (SAT)
increases by 2.0 °C in the mid-Pliocene compared with the
pre-industrial temperature. The greatest warming occurs at high latitudes of
both hemispheres, with little change in SAT at low latitudes. The
equator-to-pole SAT gradient is reduced in the mid-Pliocene simulation. The
annual mean precipitation is enhanced by 3.6% of the pre-industrial
value. However, the changes in precipitation are greater at low latitudes
than at high latitudes. |
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