Upward momentum transfer in the marine boundary layer
This paper focuses on the study of momentum flux between ocean and atmosphere in light winds and is based on the data collected during several field campaigns, the Atlantic Stratocumulus Transition Experiment, the Tropical Ocean Global Atmosphere Coupled Ocean--Atmosphere Response Experiment, and th...
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Veröffentlicht in: | Journal of physical oceanography 2001-07, Vol.31 (7), p.1698-1711 |
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container_title | Journal of physical oceanography |
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creator | GRACHEV, A. A FAIRALL, C. W |
description | This paper focuses on the study of momentum flux between ocean and atmosphere in light winds and is based on the data collected during several field campaigns, the Atlantic Stratocumulus Transition Experiment, the Tropical Ocean Global Atmosphere Coupled Ocean--Atmosphere Response Experiment, and the San Clemente Ocean Probing Experiment. Weak wind at sea is frequently accompanied by the presence of fast-traveling ocean swell, which dramatically affects momentum transfer. |
doi_str_mv | 10.1175/1520-0485(2001)031<1698:umtitm>2.0.co;2 |
format | Article |
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Weak wind at sea is frequently accompanied by the presence of fast-traveling ocean swell, which dramatically affects momentum transfer.</description><subject>Atmosphere</subject><subject>Boundary layers</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Marine</subject><subject>Momentum transfer</subject><subject>Oceanography</subject><subject>Oceans</subject><subject>Physics of the oceans</subject><subject>Sea-air exchange processes</subject><subject>Wind</subject><issn>0022-3670</issn><issn>1520-0485</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2001</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>BEC</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNpdkF1LwzAUQIMoOKf_oYiIPnS7N2nSVEWQoXOwsZftOaRpih39mEmL7N_bMhHx6b4czr33EDJFmCDGfIqcQgiR5HcUAO-B4ROKRD50VVu01TOdwMQ0j_SEjH7JUzICoDRkIoZzcuH9DgAE0mRE-Hb_pV0WVE1l67argtbp2ufWBUUdtB82qLQrahukTVdn2h2CUh-suyRnuS69vfqZY7J9e93M3sPler6YvSxDEzHehlwLzjWTsciYESyiAlkUU2YkphaN5qnUGU-o0ImMMsvRYJwkOsoMEyY1GRuT26N375rPzvpWVYU3tix1bZvOK5QoIe6tY3L9D9w1nav72xSlLImklKyH5kfIuMZ7Z3O1d0X_30EhqKGtGoqpoZga2qq-rRraqu1qs9isFFWgZmtFe9PNzzrtjS7zvpkp_B9dwoZfvwFbI3xc</recordid><startdate>20010701</startdate><enddate>20010701</enddate><creator>GRACHEV, A. 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A</au><au>FAIRALL, C. W</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Upward momentum transfer in the marine boundary layer</atitle><jtitle>Journal of physical oceanography</jtitle><date>2001-07-01</date><risdate>2001</risdate><volume>31</volume><issue>7</issue><spage>1698</spage><epage>1711</epage><pages>1698-1711</pages><issn>0022-3670</issn><eissn>1520-0485</eissn><coden>JPYOBT</coden><abstract>This paper focuses on the study of momentum flux between ocean and atmosphere in light winds and is based on the data collected during several field campaigns, the Atlantic Stratocumulus Transition Experiment, the Tropical Ocean Global Atmosphere Coupled Ocean--Atmosphere Response Experiment, and the San Clemente Ocean Probing Experiment. Weak wind at sea is frequently accompanied by the presence of fast-traveling ocean swell, which dramatically affects momentum transfer.</abstract><cop>Boston, MA</cop><pub>American Meteorological Society</pub><doi>10.1175/1520-0485(2001)031<1698:umtitm>2.0.co;2</doi><tpages>14</tpages><oa>free_for_read</oa></addata></record> |
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source | American Meteorological Society; EZB Electronic Journals Library |
subjects | Atmosphere Boundary layers Earth, ocean, space Exact sciences and technology External geophysics Marine Momentum transfer Oceanography Oceans Physics of the oceans Sea-air exchange processes Wind |
title | Upward momentum transfer in the marine boundary layer |
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