Observed Oceanic Variability at and near the Air-Sea Interface during Phase III of Project BOMEXSource: Journal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 001::page 103Author:Jacobs, Clifford A.
DOI: 10.1175/1520-0485(1978)008<0103:OOVAAN>2.0.CO;2Publisher: American Meteorological Society
Abstract: The natural variability observed at and near the air-sea interface during Period III of Project BOMEX is examined. The time and space variability in the observed oceanic parameters is large by classical oceanographic standards. Several interesting features were found in this BOMEX data set. Changes in the 10 m wind speed appear to be correlated to the movements of shallow temperature and salinity fronts. A secondary maximum in the mean diurnal sea surface temperature variation consistently appears in the early morning (local time). The diurnal heating patterns in the mixed layer imply a relationship between the vertical density gradient and the intensity of the vertical turbulent mixing. This relationship is further explored in numerical model studies in a companion paper (Jacobs, 1978).
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| contributor author | Jacobs, Clifford A. | |
| date accessioned | 2017-06-09T14:44:43Z | |
| date available | 2017-06-09T14:44:43Z | |
| date copyright | 1978/01/01 | |
| date issued | 1978 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-25784.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4162605 | |
| description abstract | The natural variability observed at and near the air-sea interface during Period III of Project BOMEX is examined. The time and space variability in the observed oceanic parameters is large by classical oceanographic standards. Several interesting features were found in this BOMEX data set. Changes in the 10 m wind speed appear to be correlated to the movements of shallow temperature and salinity fronts. A secondary maximum in the mean diurnal sea surface temperature variation consistently appears in the early morning (local time). The diurnal heating patterns in the mixed layer imply a relationship between the vertical density gradient and the intensity of the vertical turbulent mixing. This relationship is further explored in numerical model studies in a companion paper (Jacobs, 1978). | |
| publisher | American Meteorological Society | |
| title | Observed Oceanic Variability at and near the Air-Sea Interface during Phase III of Project BOMEX | |
| type | Journal Paper | |
| journal volume | 8 | |
| journal issue | 1 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1978)008<0103:OOVAAN>2.0.CO;2 | |
| journal fristpage | 103 | |
| journal lastpage | 118 | |
| tree | Journal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 001 | |
| contenttype | Fulltext |