| contributor author | Hastenrath, Stefan | |
| date accessioned | 2017-06-09T14:43:19Z | |
| date available | 2017-06-09T14:43:19Z | |
| date copyright | 2002/05/01 | |
| date issued | 2002 | |
| identifier issn | 0003-0007 | |
| identifier other | ams-25208.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4161966 | |
| description abstract | The term ?dipole? implies a seesaw, inverse variations of an element at the extremities of an oscillationsystem. The Southern Oscillation and North Atlantic Oscillation are examples of such mainly standing oscillations inpressure. By contrast, for the sea surface temperature (SST) fields in the tropical Atlantic and equatorialIndian Oceans, the SST gradient was found to be closely associated with climatic anomalies, but there is no seesaw. Use the term dipole is misleading. | |
| publisher | American Meteorological Society | |
| title | Dipoles, Temperature Gradients, and Tropical Climate Anomalies | |
| type | Journal Paper | |
| journal volume | 83 | |
| journal issue | 5 | |
| journal title | Bulletin of the American Meteorological Society | |
| identifier doi | 10.1175/1520-0477(2002)083<0735:WLACNM>2.3.CO;2 | |
| journal fristpage | 735 | |
| journal lastpage | 738 | |
| tree | Bulletin of the American Meteorological Society:;2002:;volume( 083 ):;issue: 005 | |
| contenttype | Fulltext | |
