Why Is North Tropical Atlantic SST Variability Stronger in Boreal Spring?Source: Journal of Climate:;2004:;volume( 017 ):;issue: 015::page 3017Author:Czaja, Arnaud
DOI: 10.1175/1520-0442(2004)017<3017:WINTAS>2.0.CO;2Publisher: American Meteorological Society
Abstract: It is suggested that the seasonal dependence of interannual variability displayed by observed sea surface temperature (SST) over the north tropical Atlantic primarily reflects the seasonality of the remote forcing associated with the North Atlantic and Southern Oscillations and is controlled by the mean damping time scale of SST anomaly. A stochastic model including a seasonally dependent forcing is used to test this hypothesis against observations.
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| contributor author | Czaja, Arnaud | |
| date accessioned | 2017-06-09T16:22:42Z | |
| date available | 2017-06-09T16:22:42Z | |
| date copyright | 2004/08/01 | |
| date issued | 2004 | |
| identifier issn | 0894-8755 | |
| identifier other | ams-6676.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4208133 | |
| description abstract | It is suggested that the seasonal dependence of interannual variability displayed by observed sea surface temperature (SST) over the north tropical Atlantic primarily reflects the seasonality of the remote forcing associated with the North Atlantic and Southern Oscillations and is controlled by the mean damping time scale of SST anomaly. A stochastic model including a seasonally dependent forcing is used to test this hypothesis against observations. | |
| publisher | American Meteorological Society | |
| title | Why Is North Tropical Atlantic SST Variability Stronger in Boreal Spring? | |
| type | Journal Paper | |
| journal volume | 17 | |
| journal issue | 15 | |
| journal title | Journal of Climate | |
| identifier doi | 10.1175/1520-0442(2004)017<3017:WINTAS>2.0.CO;2 | |
| journal fristpage | 3017 | |
| journal lastpage | 3025 | |
| tree | Journal of Climate:;2004:;volume( 017 ):;issue: 015 | |
| contenttype | Fulltext |