| contributor author | Raper, Sarah C. B. | |
| contributor author | Gregory, Jonathan M. | |
| contributor author | Stouffer, Ronald J. | |
| date accessioned | 2017-06-09T16:02:24Z | |
| date available | 2017-06-09T16:02:24Z | |
| date copyright | 2002/01/01 | |
| date issued | 2002 | |
| identifier issn | 0894-8755 | |
| identifier other | ams-5946.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4200022 | |
| description abstract | The role of climate sensitivity and ocean heat uptake in determining the range of climate model response is investigated in the second phase of the Coupled Model Intercomparison Project (CMIP2) AOGCM results. The fraction of equilibrium warming that is realized at any one time is less in those models with higher climate sensitivity, leading to a reduction in the temperature response range at the time of CO2 doubling [transient climate response (TCR) range]. The range is reduced by a further 15% because of an apparent relationship between climate sensitivity and the efficiency of ocean heat uptake. Some possible physical causes for this relationship are suggested. | |
| publisher | American Meteorological Society | |
| title | The Role of Climate Sensitivity and Ocean Heat Uptake on AOGCM Transient Temperature Response | |
| type | Journal Paper | |
| journal volume | 15 | |
| journal issue | 1 | |
| journal title | Journal of Climate | |
| identifier doi | 10.1175/1520-0442(2002)015<0124:TROCSA>2.0.CO;2 | |
| journal fristpage | 124 | |
| journal lastpage | 130 | |
| tree | Journal of Climate:;2002:;volume( 015 ):;issue: 001 | |
| contenttype | Fulltext | |
