A case study of the tropical Hot Event in November 2006 (HE0611) using a geostationary meteorological satellite and the TAO/TRITON mooring array
Qin et al. have found Hot Events (HE), which are short‐term (about 20 days) large‐scale (about 15,000,000 km2) regions with very high Sea Surface Temperatures (SST > 30°C). Following their definition, an HE was identified in the tropical western Pacific in November 2006, which is named HE0611. A...
Gespeichert in:
Veröffentlicht in: | Journal of Geophysical Research. C. Oceans 2008-08, Vol.113 (C8), p.n/a |
---|---|
Hauptverfasser: | , , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | n/a |
---|---|
container_issue | C8 |
container_start_page | |
container_title | Journal of Geophysical Research. C. Oceans |
container_volume | 113 |
creator | Qin, Huiling Kawamura, Hiroshi Sakaida, Futoki Ando, Kentaro |
description | Qin et al. have found Hot Events (HE), which are short‐term (about 20 days) large‐scale (about 15,000,000 km2) regions with very high Sea Surface Temperatures (SST > 30°C). Following their definition, an HE was identified in the tropical western Pacific in November 2006, which is named HE0611. A case study of HE is conducted by using the advanced satellite products and in‐situ measurements from the TAO/TRITON mooring array. Two parts (HE0611‐East and ‐West) with very high SST connected to form HE0611. SST in HE0611‐West increases quickly with large diurnal SST variations, which are caused by large solar radiation and suppressed latent heat loss. The increase of the mixed‐layer heat content is clearly accounted for the accumulated heat gain through the air‐sea interaction. The formation mechanism of HE0611‐East is completely different; its very high SST is supported by a subsurface high SST anomaly associated with the El Niño. Two phenomena similar to HE0611 were observed in November of the El Niño years of 1994 and 2002. |
doi_str_mv | 10.1029/2007JC004640 |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_19536793</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1919954473</sourcerecordid><originalsourceid>FETCH-LOGICAL-a5383-7345426c50b2cd5e34aa0335d71f31de58229469e2c218f37aa89a20529f2a233</originalsourceid><addsrcrecordid>eNqFkcFuEzEQhlcIJKLSGw_gC6hIbDse2-vdYxSFpFVJUBWgN8vd9QbD7jrYTiFv0UfGSaqKE8xlLt__zWgmy15TOKeA1QUCyKsJAC84PMtGSEWRIwI-z0ZAeZkDonyZnYbwHVJxkTA6yh7GpNbBkBC3zY64lsRvhkTvNrbWHZm7SKb3ZojEDmTh7k1_ZzxJkwpyNp9CQek7sg12WBNN1saFqKN1g_Y70ptonHedWx9EQUfTdTYaoofmMGM1Xl6sbi5XywXpnfMHh_d69yp70eoumNPHfpJ9_jBdTeb59XJ2ORlf51qwkuWSccGxqAXcYd0Iw7jWwJhoJG0ZbYwoESteVAZrpGXLpNZlpREEVi1qZOwke3v0brz7uTUhqt6GOi2pB-O2QdFKsEJWe_DsPyCtKsG53KPvj2jtXQjetGrjbZ_OoSio_ZPU309K-JtHsw7pSK3XQ23DUwZBQikQE8eO3C_bmd0_nepqdjOhkHZPqfyYsiGa308p7X-oQjIp1NfFTH0RH29x9ulWAfsD9AWrpA</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1919954473</pqid></control><display><type>article</type><title>A case study of the tropical Hot Event in November 2006 (HE0611) using a geostationary meteorological satellite and the TAO/TRITON mooring array</title><source>Wiley Journals</source><source>Wiley-Blackwell AGU Digital Library</source><source>Wiley Online Library (Open Access Collection)</source><source>Alma/SFX Local Collection</source><creator>Qin, Huiling ; Kawamura, Hiroshi ; Sakaida, Futoki ; Ando, Kentaro</creator><creatorcontrib>Qin, Huiling ; Kawamura, Hiroshi ; Sakaida, Futoki ; Ando, Kentaro</creatorcontrib><description>Qin et al. have found Hot Events (HE), which are short‐term (about 20 days) large‐scale (about 15,000,000 km2) regions with very high Sea Surface Temperatures (SST > 30°C). Following their definition, an HE was identified in the tropical western Pacific in November 2006, which is named HE0611. A case study of HE is conducted by using the advanced satellite products and in‐situ measurements from the TAO/TRITON mooring array. Two parts (HE0611‐East and ‐West) with very high SST connected to form HE0611. SST in HE0611‐West increases quickly with large diurnal SST variations, which are caused by large solar radiation and suppressed latent heat loss. The increase of the mixed‐layer heat content is clearly accounted for the accumulated heat gain through the air‐sea interaction. The formation mechanism of HE0611‐East is completely different; its very high SST is supported by a subsurface high SST anomaly associated with the El Niño. Two phenomena similar to HE0611 were observed in November of the El Niño years of 1994 and 2002.</description><identifier>ISSN: 0148-0227</identifier><identifier>ISSN: 2169-9275</identifier><identifier>EISSN: 2156-2202</identifier><identifier>EISSN: 2169-9291</identifier><identifier>DOI: 10.1029/2007JC004640</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>diurnal SST variation ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Hot event ; Marine</subject><ispartof>Journal of Geophysical Research. C. Oceans, 2008-08, Vol.113 (C8), p.n/a</ispartof><rights>Copyright 2008 by the American Geophysical Union.</rights><rights>2008 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a5383-7345426c50b2cd5e34aa0335d71f31de58229469e2c218f37aa89a20529f2a233</citedby><cites>FETCH-LOGICAL-a5383-7345426c50b2cd5e34aa0335d71f31de58229469e2c218f37aa89a20529f2a233</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2007JC004640$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2007JC004640$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,1433,11514,27924,27925,45574,45575,46409,46468,46833,46892</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=20708522$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Qin, Huiling</creatorcontrib><creatorcontrib>Kawamura, Hiroshi</creatorcontrib><creatorcontrib>Sakaida, Futoki</creatorcontrib><creatorcontrib>Ando, Kentaro</creatorcontrib><title>A case study of the tropical Hot Event in November 2006 (HE0611) using a geostationary meteorological satellite and the TAO/TRITON mooring array</title><title>Journal of Geophysical Research. C. Oceans</title><addtitle>J. Geophys. Res</addtitle><description>Qin et al. have found Hot Events (HE), which are short‐term (about 20 days) large‐scale (about 15,000,000 km2) regions with very high Sea Surface Temperatures (SST > 30°C). Following their definition, an HE was identified in the tropical western Pacific in November 2006, which is named HE0611. A case study of HE is conducted by using the advanced satellite products and in‐situ measurements from the TAO/TRITON mooring array. Two parts (HE0611‐East and ‐West) with very high SST connected to form HE0611. SST in HE0611‐West increases quickly with large diurnal SST variations, which are caused by large solar radiation and suppressed latent heat loss. The increase of the mixed‐layer heat content is clearly accounted for the accumulated heat gain through the air‐sea interaction. The formation mechanism of HE0611‐East is completely different; its very high SST is supported by a subsurface high SST anomaly associated with the El Niño. Two phenomena similar to HE0611 were observed in November of the El Niño years of 1994 and 2002.</description><subject>diurnal SST variation</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Hot event</subject><subject>Marine</subject><issn>0148-0227</issn><issn>2169-9275</issn><issn>2156-2202</issn><issn>2169-9291</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2008</creationdate><recordtype>article</recordtype><recordid>eNqFkcFuEzEQhlcIJKLSGw_gC6hIbDse2-vdYxSFpFVJUBWgN8vd9QbD7jrYTiFv0UfGSaqKE8xlLt__zWgmy15TOKeA1QUCyKsJAC84PMtGSEWRIwI-z0ZAeZkDonyZnYbwHVJxkTA6yh7GpNbBkBC3zY64lsRvhkTvNrbWHZm7SKb3ZojEDmTh7k1_ZzxJkwpyNp9CQek7sg12WBNN1saFqKN1g_Y70ptonHedWx9EQUfTdTYaoofmMGM1Xl6sbi5XywXpnfMHh_d69yp70eoumNPHfpJ9_jBdTeb59XJ2ORlf51qwkuWSccGxqAXcYd0Iw7jWwJhoJG0ZbYwoESteVAZrpGXLpNZlpREEVi1qZOwke3v0brz7uTUhqt6GOi2pB-O2QdFKsEJWe_DsPyCtKsG53KPvj2jtXQjetGrjbZ_OoSio_ZPU309K-JtHsw7pSK3XQ23DUwZBQikQE8eO3C_bmd0_nepqdjOhkHZPqfyYsiGa308p7X-oQjIp1NfFTH0RH29x9ulWAfsD9AWrpA</recordid><startdate>200808</startdate><enddate>200808</enddate><creator>Qin, Huiling</creator><creator>Kawamura, Hiroshi</creator><creator>Sakaida, Futoki</creator><creator>Ando, Kentaro</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>7TG</scope><scope>KL.</scope></search><sort><creationdate>200808</creationdate><title>A case study of the tropical Hot Event in November 2006 (HE0611) using a geostationary meteorological satellite and the TAO/TRITON mooring array</title><author>Qin, Huiling ; Kawamura, Hiroshi ; Sakaida, Futoki ; Ando, Kentaro</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a5383-7345426c50b2cd5e34aa0335d71f31de58229469e2c218f37aa89a20529f2a233</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2008</creationdate><topic>diurnal SST variation</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Hot event</topic><topic>Marine</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Qin, Huiling</creatorcontrib><creatorcontrib>Kawamura, Hiroshi</creatorcontrib><creatorcontrib>Sakaida, Futoki</creatorcontrib><creatorcontrib>Ando, Kentaro</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><jtitle>Journal of Geophysical Research. C. Oceans</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Qin, Huiling</au><au>Kawamura, Hiroshi</au><au>Sakaida, Futoki</au><au>Ando, Kentaro</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A case study of the tropical Hot Event in November 2006 (HE0611) using a geostationary meteorological satellite and the TAO/TRITON mooring array</atitle><jtitle>Journal of Geophysical Research. C. Oceans</jtitle><addtitle>J. Geophys. Res</addtitle><date>2008-08</date><risdate>2008</risdate><volume>113</volume><issue>C8</issue><epage>n/a</epage><issn>0148-0227</issn><issn>2169-9275</issn><eissn>2156-2202</eissn><eissn>2169-9291</eissn><abstract>Qin et al. have found Hot Events (HE), which are short‐term (about 20 days) large‐scale (about 15,000,000 km2) regions with very high Sea Surface Temperatures (SST > 30°C). Following their definition, an HE was identified in the tropical western Pacific in November 2006, which is named HE0611. A case study of HE is conducted by using the advanced satellite products and in‐situ measurements from the TAO/TRITON mooring array. Two parts (HE0611‐East and ‐West) with very high SST connected to form HE0611. SST in HE0611‐West increases quickly with large diurnal SST variations, which are caused by large solar radiation and suppressed latent heat loss. The increase of the mixed‐layer heat content is clearly accounted for the accumulated heat gain through the air‐sea interaction. The formation mechanism of HE0611‐East is completely different; its very high SST is supported by a subsurface high SST anomaly associated with the El Niño. Two phenomena similar to HE0611 were observed in November of the El Niño years of 1994 and 2002.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2007JC004640</doi><tpages>11</tpages><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0148-0227 |
ispartof | Journal of Geophysical Research. C. Oceans, 2008-08, Vol.113 (C8), p.n/a |
issn | 0148-0227 2169-9275 2156-2202 2169-9291 |
language | eng |
recordid | cdi_proquest_miscellaneous_19536793 |
source | Wiley Journals; Wiley-Blackwell AGU Digital Library; Wiley Online Library (Open Access Collection); Alma/SFX Local Collection |
subjects | diurnal SST variation Earth sciences Earth, ocean, space Exact sciences and technology Hot event Marine |
title | A case study of the tropical Hot Event in November 2006 (HE0611) using a geostationary meteorological satellite and the TAO/TRITON mooring array |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-29T07%3A13%3A44IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=A%20case%20study%20of%20the%20tropical%20Hot%20Event%20in%20November%202006%20(HE0611)%20using%20a%20geostationary%20meteorological%20satellite%20and%20the%20TAO/TRITON%20mooring%20array&rft.jtitle=Journal%20of%20Geophysical%20Research.%20C.%20Oceans&rft.au=Qin,%20Huiling&rft.date=2008-08&rft.volume=113&rft.issue=C8&rft.epage=n/a&rft.issn=0148-0227&rft.eissn=2156-2202&rft_id=info:doi/10.1029/2007JC004640&rft_dat=%3Cproquest_cross%3E1919954473%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1919954473&rft_id=info:pmid/&rfr_iscdi=true |