Air-sea interaction throughout the troposphere over a very high sea surface temperature phenomenon
A large region of very high sea surface temperature (SST, >30°C) was maintained for more than 10 days in the tropical western Pacific. This study examined how this “hot event” (HE), observed in November 2006 (HE0611), was generated by air‐sea interaction throughout the whole troposphere. Cloud mo...
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| Veröffentlicht in: | Geophysical research letters 2010-01, Vol.37 (1), p.n/a |
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| creator | Qin, Huiling Kawamura, Hiroshi |
| description | A large region of very high sea surface temperature (SST, >30°C) was maintained for more than 10 days in the tropical western Pacific. This study examined how this “hot event” (HE), observed in November 2006 (HE0611), was generated by air‐sea interaction throughout the whole troposphere. Cloud motion wind and cloud cover data obtained from geostationary satellite measurements showed deep convective systems with divergent air flows in the eastern part of HE0611 (‐East). High‐level convergence was derived from cloud motion winds over the western part of HE0611 (‐West), where the SST rapidly increased up to 30°C. Cloud‐free conditions with convergent flow were considered to be related to the deep convection over HE0611‐East. These interactions through the whole troposphere over HE0611 may have been a true appearance of “remote convection,” which has been suggested as a mechanism of very high SST generation in tropical oceans. |
| doi_str_mv | 10.1029/2009GL041685 |
| format | Article |
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This study examined how this “hot event” (HE), observed in November 2006 (HE0611), was generated by air‐sea interaction throughout the whole troposphere. Cloud motion wind and cloud cover data obtained from geostationary satellite measurements showed deep convective systems with divergent air flows in the eastern part of HE0611 (‐East). High‐level convergence was derived from cloud motion winds over the western part of HE0611 (‐West), where the SST rapidly increased up to 30°C. Cloud‐free conditions with convergent flow were considered to be related to the deep convection over HE0611‐East. 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Res. Lett</addtitle><description>A large region of very high sea surface temperature (SST, >30°C) was maintained for more than 10 days in the tropical western Pacific. This study examined how this “hot event” (HE), observed in November 2006 (HE0611), was generated by air‐sea interaction throughout the whole troposphere. Cloud motion wind and cloud cover data obtained from geostationary satellite measurements showed deep convective systems with divergent air flows in the eastern part of HE0611 (‐East). High‐level convergence was derived from cloud motion winds over the western part of HE0611 (‐West), where the SST rapidly increased up to 30°C. Cloud‐free conditions with convergent flow were considered to be related to the deep convection over HE0611‐East. These interactions through the whole troposphere over HE0611 may have been a true appearance of “remote convection,” which has been suggested as a mechanism of very high SST generation in tropical oceans.</description><subject>Air flow</subject><subject>air-sea interaction</subject><subject>Atmospheric boundary layer</subject><subject>Atmospheric sciences</subject><subject>Cloud cover</subject><subject>Clouds</subject><subject>Convection</subject><subject>Convergence</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Geophysics</subject><subject>Geostationary satellites</subject><subject>Marine</subject><subject>Ocean-atmosphere interaction</subject><subject>Oceans</subject><subject>remote convection</subject><subject>Remote sensing</subject><subject>Sea surface temperature</subject><subject>Troposphere</subject><subject>very high SST</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNqFkU1rFTEUhoMoeK3u_AGDoLhw9OR7sqzFXoWhQlW6DJmY6aTOnYzJjPb-e0-5pYiLukhyIM_zkpNDyHMKbykw844BmG0LgqpGPiAbaoSoGwD9kGzwBmum1WPypJQrAODA6YZ0xzHXJbgqTkvIzi8xTdUy5LReDmldsAzVktOcyjyEHKr0K-TKVbjvqyFeDtWNW9bcO49g2M0YsqwIIj6lHa7pKXnUu7GEZ7fnEfl2-uHryce6_bz9dHLc1l5qxuqul70G4ZynQXvecMeh0Y30KoTvjTKsk41RSoB0ClxHwXCBCveK8c50hh-RV4fcOaefayiL3cXiwzi6KaS1WK4EFUyq_4KMcmq40gi-vhekSjCEOWWIvvgHvUprnrBfqxUVmuFzEXpzgHxOpeTQ2znHnct7S8HeTND-PUHEX95muuLd2Gc3-VjuHMaEUJJS5NiB-x3HsL83027PW6bwu1GqD1IsS7i-k1z-YbFzLe3F2da-P-PnX9hFY1v-B-oDt6E</recordid><startdate>201001</startdate><enddate>201001</enddate><creator>Qin, Huiling</creator><creator>Kawamura, Hiroshi</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><general>John Wiley & Sons, Inc</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>L7M</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>7SM</scope></search><sort><creationdate>201001</creationdate><title>Air-sea interaction throughout the troposphere over a very high sea surface temperature phenomenon</title><author>Qin, Huiling ; 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Res. Lett</addtitle><date>2010-01</date><risdate>2010</risdate><volume>37</volume><issue>1</issue><epage>n/a</epage><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>A large region of very high sea surface temperature (SST, >30°C) was maintained for more than 10 days in the tropical western Pacific. This study examined how this “hot event” (HE), observed in November 2006 (HE0611), was generated by air‐sea interaction throughout the whole troposphere. Cloud motion wind and cloud cover data obtained from geostationary satellite measurements showed deep convective systems with divergent air flows in the eastern part of HE0611 (‐East). High‐level convergence was derived from cloud motion winds over the western part of HE0611 (‐West), where the SST rapidly increased up to 30°C. Cloud‐free conditions with convergent flow were considered to be related to the deep convection over HE0611‐East. These interactions through the whole troposphere over HE0611 may have been a true appearance of “remote convection,” which has been suggested as a mechanism of very high SST generation in tropical oceans.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2009GL041685</doi><tpages>4</tpages><oa>free_for_read</oa></addata></record> |
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| source | Wiley-Blackwell AGU Digital Library; Wiley Online Library Journals Frontfile Complete; Wiley Online Library Free Content; EZB-FREE-00999 freely available EZB journals |
| subjects | Air flow air-sea interaction Atmospheric boundary layer Atmospheric sciences Cloud cover Clouds Convection Convergence Earth sciences Earth, ocean, space Exact sciences and technology Geophysics Geostationary satellites Marine Ocean-atmosphere interaction Oceans remote convection Remote sensing Sea surface temperature Troposphere very high SST |
| title | Air-sea interaction throughout the troposphere over a very high sea surface temperature phenomenon |
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