| contributor author | Flament, P. | |
| contributor author | Firing, J. | |
| contributor author | Sawyer, M. | |
| contributor author | Trefois, C. | |
| date accessioned | 2017-06-09T14:51:00Z | |
| date available | 2017-06-09T14:51:00Z | |
| date copyright | 1994/01/01 | |
| date issued | 1994 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-28149.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4165233 | |
| description abstract | Intense diurnal warming of the ocean surface was observed in April 1982 off California, using a combination of mooring, hydrographic, and satellite infrared and satellite pigment measurements. The event corresponded to a spatial and temooral minimum of the wind stress. The diurnal surface temperature amplitude exceeded 6.6°C locally despite a 490-nm optical depth of 20 m, suggesting that phytoplankton was not responsible for the shallow heat trapping. Coherent horizontal temperature streaks at least 50 km long and 4-8 km wide formedduring the subsequent erosion of the shallow warm layers. It is hypothesized that thcfr scale was set by planetary boundary-layer circulations. | |
| publisher | American Meteorological Society | |
| title | Amplitude and Horizontal Structure of a Large Diurnal Sea Surface Warming Event during the Coastal Ocean Dynamics Experiment | |
| type | Journal Paper | |
| journal volume | 24 | |
| journal issue | 1 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1994)024<0124:AAHSOA>2.0.CO;2 | |
| journal fristpage | 124 | |
| journal lastpage | 139 | |
| tree | Journal of Physical Oceanography:;1994:;Volume( 024 ):;issue: 001 | |
| contenttype | Fulltext | |