Journal
GEOPHYSICAL RESEARCH LETTERS
Volume 35, Issue 12, Pages -Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/2008GL033573
Keywords
-
Categories
Ask authors/readers for more resources
The atmospheric circulation response to CO2 doubling in various versions of an atmospheric general circulation model (AGCM) without a well-resolved stratosphere (lowtop'' model), is compared to the response in a version of the same AGCM with a well-resolved stratosphere (high-top'' model). The doubled CO2 response of the best-tuned'' (i.e. operational) low-top model version is significantly different from that in the best-tuned high-top model version. Additional experiments show that this difference is not caused by the model lid height, but instead can be mainly attributed to differences in the settings of parameterized orographic gravity-wave drag which control the strength of the zonal wind in the mid-to high-latitude lower stratosphere and the mean sea-level pressure distribution. These findings suggest a link between the strength of the winds in the mid- to high-latitude lower stratosphere and tropospheric annular mode responses, and have implications for how to proceed with high-top low-top model intercomparisons.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available