Intrusion of warm Bering/Chukchi waters onto the shelf in the western Beaufort Sea
| Autor: | Stephen R. Okkonen, Rachel A. Potter, Robert G. Campbell, Wieslaw Maslowski, Carin J. Ashjian, Jaclyn L. Clement-Kinney |
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| Rok vydání: | 2009 |
| Předmět: |
Atmospheric Science
Soil Science Context (language use) Aquatic Science Oceanography law.invention Geochemistry and Petrology law Earth and Planetary Sciences (miscellaneous) Sea level Earth-Surface Processes Water Science and Technology Canyon geography geography.geographical_feature_category Ecology Paleontology Forestry Beaufort scale Current (stream) Sea surface temperature Geophysics Space and Planetary Science Beaufort index Upwelling Hydrography Geology |
| Zdroj: | Journal of Geophysical Research. 114 |
| ISSN: | 0148-0227 |
| DOI: | 10.1029/2008jc004870 |
| Popis: | The article of record as published may be found at https://doi.org/10.1029/2008JC004870 Wind-driven changes in the path of warm Bering/Chukchi waters carried by the Alaska Coastal Current (ACC) through Barrow Canyon during late summer are described from high-resolution hydrography, acoustic Doppler current profiler–measured currents, and satellite-measured sea surface temperature imagery acquired from mid-August to mid-September 2005–2007 near Barrow, Alaska. Numerical simulations are used to provide a multidecadal context for these observational data. Four generalized wind regimes and associated circulation states are identified. When winds are from the east or east-southeast, the ACC jet tends to be relatively strong and flows adjacent to the shelf break along the southern flank of Barrow Canyon. These easterly winds drive inner shelf currents northwestward along the Alaskan Beaufort coast where they oppose significant eastward intrusions of warm water from Barrow Canyon onto the shelf. Because these easterly winds promote sea level set down over the Beaufort shelf and upwelling along the Beaufort slope, the ACC jet necessarily becomes weaker, broader, and displaced seaward from the Beaufort shelf break upon exiting Barrow Canyon. Winds from the northeast promote separation of the ACC from the southern flank of Barrow Canyon and establish an up-canyon current along the southern flank that is fed in part by waters from the western Beaufort shelf. When winds are weak or from the southwest, warm Bering/Chukchi waters from Barrow Canyon intrude onto the western Beaufort shelf. This work was supported in 2005 and 2006 by NSF grants OPP-0436131 and OPP-0436166. In 2007, this work received support through Woods Hole Oceanographic Institution- NOAA Cooperative Institute for Climate and Ocean Research Cooperative Agreement NA17RJ1223 and University of Alaska Fairbanks-NOAA Cooperative Institute for Arctic Research Cooperative Agreement NA17RJ1224. Additional support was provided by the James M. and Ruth P. Clark Arctic Research Initiative Fund at the Woods Hole Oceanographic Institution. |
| Databáze: | OpenAIRE |
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