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...

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Veröffentlicht in:Journal of Geophysical Research. C. Oceans 2008-08, Vol.113 (C8), p.n/a
Hauptverfasser: Qin, Huiling, Kawamura, Hiroshi, Sakaida, Futoki, Ando, Kentaro
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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.
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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 &gt; 30°C). 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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>
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2169-9291
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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
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