| contributor author | Anderson, David L. T. | |
| contributor author | McCreary, Julian P. | |
| date accessioned | 2017-06-09T14:26:00Z | |
| date available | 2017-06-09T14:26:00Z | |
| date copyright | 1985/11/01 | |
| date issued | 1985 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-19168.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4155254 | |
| description abstract | The coupled ocean-atmosphere model of Anderson and McCreary is extended to include two oceans. An advantage of the two-ocean system is that it is not necessary to specify externally convection over land. For a basin geometry that most resembles the Indian and Pacific Oceans, strong permanent convection exists in the eastern Indian Ocean, and there is an oscillation in the Pacific Ocean with a period of about five years. Associated with this oscillation is a patch of convection that develops in the central and western ocean and propagates into the eastern ocean before dissipating. | |
| publisher | American Meteorological Society | |
| title | On the Role of the Indian Ocean in a Coupled Ocean–Atmosphere Model of El Niño and the Southern Oscillation | |
| type | Journal Paper | |
| journal volume | 42 | |
| journal issue | 22 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1985)042<2439:OTROTI>2.0.CO;2 | |
| journal fristpage | 2439 | |
| journal lastpage | 2442 | |
| tree | Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 022 | |
| contenttype | Fulltext | |