Growth and decay of the Arabian Sea mini warm pool during May 2000: Observations and simulations
Oceanographic surveys were carried out in the southeastern Arabian Sea in two phases during 14–17 May and 23–27 May 2000 to study the evolution of the Arabian Sea mini warm pool. The hydrographic data collected during these experiments, satellite imagery of sea surface temperature for the correspond...
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| Veröffentlicht in: | Deep-sea research. Part I, Oceanographic research papers Oceanographic research papers, 2009-04, Vol.56 (4), p.528-540 |
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| container_title | Deep-sea research. Part I, Oceanographic research papers |
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| creator | Hareesh Kumar, P.V. Joshi, Madhu Sanilkumar, K.V. Rao, A.D. Anand, P. Anil Kumar, K. Prasada Rao, C.V.K. |
| description | Oceanographic surveys were carried out in the southeastern Arabian Sea in two phases during 14–17 May and 23–27 May 2000 to study the evolution of the Arabian Sea mini warm pool. The hydrographic data collected during these experiments, satellite imagery of sea surface temperature for the corresponding period and ship drift data were utilized for this purpose. Both satellite and
in situ observations indicated the presence of a mini warm pool up to 14 May and its dissipation thereafter. The Arabian Sea mini warm pool region was characterized by low-salinity Bay of Bengal water ( |
| doi_str_mv | 10.1016/j.dsr.2008.12.004 |
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in situ observations indicated the presence of a mini warm pool up to 14 May and its dissipation thereafter. The Arabian Sea mini warm pool region was characterized by low-salinity Bay of Bengal water (<22 sigma-
t). This watermass was advected into the southeastern Arabian Sea by the East India Coastal Current mainly during November–January and recirculated in this region in an anticyclonic eddy. Immediately after the dissipation of the mini warm pool, this watermass could not be traced in this region. Simulation of mini warm pool characteristics using the Princeton Ocean Model (POM) agreed well with
in situ and satellite observations. Moreover, the model showed strengthening of southerly currents in the warm pool region during its dissipation period, which caused the disappearance of the Bay of Bengal watermass. Specific experiments with the POM revealed the significance of heat flux components, low wind speed and salinity stratification in the formation and sustenance of the mini warm pool.</description><identifier>ISSN: 0967-0637</identifier><identifier>EISSN: 1879-0119</identifier><identifier>DOI: 10.1016/j.dsr.2008.12.004</identifier><language>eng</language><publisher>Kidlington: Elsevier Ltd</publisher><subject>Advection ; Arabian Sea mini warm pool ; Dynamics of the ocean (upper and deep oceans) ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Heat flux ; Hydrography ; Marine ; Numerical model ; Oceanography ; Oceans ; Physics of the oceans ; Simulation ; Studies ; Watermass ; Western disturbance</subject><ispartof>Deep-sea research. Part I, Oceanographic research papers, 2009-04, Vol.56 (4), p.528-540</ispartof><rights>2008 Elsevier Ltd</rights><rights>2009 INIST-CNRS</rights><rights>Copyright Pergamon Press Inc. Apr 2009</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c385t-1cedaa0ba97ec6faa01e77d424a024fa5dfaba55ecd408a9929693b5849b64b33</citedby><cites>FETCH-LOGICAL-c385t-1cedaa0ba97ec6faa01e77d424a024fa5dfaba55ecd408a9929693b5849b64b33</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S096706370800246X$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3537,27901,27902,65306</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=21298841$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Hareesh Kumar, P.V.</creatorcontrib><creatorcontrib>Joshi, Madhu</creatorcontrib><creatorcontrib>Sanilkumar, K.V.</creatorcontrib><creatorcontrib>Rao, A.D.</creatorcontrib><creatorcontrib>Anand, P.</creatorcontrib><creatorcontrib>Anil Kumar, K.</creatorcontrib><creatorcontrib>Prasada Rao, C.V.K.</creatorcontrib><title>Growth and decay of the Arabian Sea mini warm pool during May 2000: Observations and simulations</title><title>Deep-sea research. Part I, Oceanographic research papers</title><description>Oceanographic surveys were carried out in the southeastern Arabian Sea in two phases during 14–17 May and 23–27 May 2000 to study the evolution of the Arabian Sea mini warm pool. The hydrographic data collected during these experiments, satellite imagery of sea surface temperature for the corresponding period and ship drift data were utilized for this purpose. Both satellite and
in situ observations indicated the presence of a mini warm pool up to 14 May and its dissipation thereafter. The Arabian Sea mini warm pool region was characterized by low-salinity Bay of Bengal water (<22 sigma-
t). This watermass was advected into the southeastern Arabian Sea by the East India Coastal Current mainly during November–January and recirculated in this region in an anticyclonic eddy. Immediately after the dissipation of the mini warm pool, this watermass could not be traced in this region. Simulation of mini warm pool characteristics using the Princeton Ocean Model (POM) agreed well with
in situ and satellite observations. Moreover, the model showed strengthening of southerly currents in the warm pool region during its dissipation period, which caused the disappearance of the Bay of Bengal watermass. Specific experiments with the POM revealed the significance of heat flux components, low wind speed and salinity stratification in the formation and sustenance of the mini warm pool.</description><subject>Advection</subject><subject>Arabian Sea mini warm pool</subject><subject>Dynamics of the ocean (upper and deep oceans)</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Heat flux</subject><subject>Hydrography</subject><subject>Marine</subject><subject>Numerical model</subject><subject>Oceanography</subject><subject>Oceans</subject><subject>Physics of the oceans</subject><subject>Simulation</subject><subject>Studies</subject><subject>Watermass</subject><subject>Western disturbance</subject><issn>0967-0637</issn><issn>1879-0119</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</creationdate><recordtype>article</recordtype><recordid>eNp9kM1u1TAQRi1EJS4tD8DOQmp3SceOk9iwqir6IxV1AazNxHaorxL71k5a9e1xuRWLLliNRzrfN9Yh5CODmgHrTre1zanmALJmvAYQb8iGyV5VwJh6Szagur6Crunfkfc5bwFKSMKG_LpM8XG5oxgstc7gE40jXe4cPUs4eAz0u0M6--DpI6aZ7mKcqF2TD7_ptwKXg_CZ3g7ZpQdcfAz5b1P28zrt9yNyMOKU3YeXeUh-Xnz9cX5V3dxeXp-f3VSmke1SMeMsIgyoeme6sTyZ63sruEDgYsTWjjhg2zpjBUhUiqtONUMrhRo6MTTNITnZ9-5SvF9dXvTss3HThMHFNWsOgkneigJ-egVu45pC-ZtmRVLTqR4KxPaQSTHn5Ea9S37G9KQZ6GfhequLcP0sXDOui_CSOX4pxmxwGhMG4_O_IGdcSSlY4b7sOVd0PHiXdDbehSLAJ2cWbaP_z5U_kQiU8w</recordid><startdate>20090401</startdate><enddate>20090401</enddate><creator>Hareesh Kumar, P.V.</creator><creator>Joshi, Madhu</creator><creator>Sanilkumar, K.V.</creator><creator>Rao, A.D.</creator><creator>Anand, P.</creator><creator>Anil Kumar, K.</creator><creator>Prasada Rao, C.V.K.</creator><general>Elsevier Ltd</general><general>Elsevier</general><general>Pergamon Press Inc</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>20090401</creationdate><title>Growth and decay of the Arabian Sea mini warm pool during May 2000: Observations and simulations</title><author>Hareesh Kumar, P.V. ; Joshi, Madhu ; Sanilkumar, K.V. ; Rao, A.D. ; Anand, P. ; Anil Kumar, K. ; Prasada Rao, C.V.K.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c385t-1cedaa0ba97ec6faa01e77d424a024fa5dfaba55ecd408a9929693b5849b64b33</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>Advection</topic><topic>Arabian Sea mini warm pool</topic><topic>Dynamics of the ocean (upper and deep oceans)</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Heat flux</topic><topic>Hydrography</topic><topic>Marine</topic><topic>Numerical model</topic><topic>Oceanography</topic><topic>Oceans</topic><topic>Physics of the oceans</topic><topic>Simulation</topic><topic>Studies</topic><topic>Watermass</topic><topic>Western disturbance</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Hareesh Kumar, P.V.</creatorcontrib><creatorcontrib>Joshi, Madhu</creatorcontrib><creatorcontrib>Sanilkumar, K.V.</creatorcontrib><creatorcontrib>Rao, A.D.</creatorcontrib><creatorcontrib>Anand, P.</creatorcontrib><creatorcontrib>Anil Kumar, K.</creatorcontrib><creatorcontrib>Prasada Rao, C.V.K.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</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>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Deep-sea research. Part I, Oceanographic research papers</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Hareesh Kumar, P.V.</au><au>Joshi, Madhu</au><au>Sanilkumar, K.V.</au><au>Rao, A.D.</au><au>Anand, P.</au><au>Anil Kumar, K.</au><au>Prasada Rao, C.V.K.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Growth and decay of the Arabian Sea mini warm pool during May 2000: Observations and simulations</atitle><jtitle>Deep-sea research. Part I, Oceanographic research papers</jtitle><date>2009-04-01</date><risdate>2009</risdate><volume>56</volume><issue>4</issue><spage>528</spage><epage>540</epage><pages>528-540</pages><issn>0967-0637</issn><eissn>1879-0119</eissn><abstract>Oceanographic surveys were carried out in the southeastern Arabian Sea in two phases during 14–17 May and 23–27 May 2000 to study the evolution of the Arabian Sea mini warm pool. The hydrographic data collected during these experiments, satellite imagery of sea surface temperature for the corresponding period and ship drift data were utilized for this purpose. Both satellite and
in situ observations indicated the presence of a mini warm pool up to 14 May and its dissipation thereafter. The Arabian Sea mini warm pool region was characterized by low-salinity Bay of Bengal water (<22 sigma-
t). This watermass was advected into the southeastern Arabian Sea by the East India Coastal Current mainly during November–January and recirculated in this region in an anticyclonic eddy. Immediately after the dissipation of the mini warm pool, this watermass could not be traced in this region. Simulation of mini warm pool characteristics using the Princeton Ocean Model (POM) agreed well with
in situ and satellite observations. Moreover, the model showed strengthening of southerly currents in the warm pool region during its dissipation period, which caused the disappearance of the Bay of Bengal watermass. Specific experiments with the POM revealed the significance of heat flux components, low wind speed and salinity stratification in the formation and sustenance of the mini warm pool.</abstract><cop>Kidlington</cop><pub>Elsevier Ltd</pub><doi>10.1016/j.dsr.2008.12.004</doi><tpages>13</tpages></addata></record> |
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| subjects | Advection Arabian Sea mini warm pool Dynamics of the ocean (upper and deep oceans) Earth, ocean, space Exact sciences and technology External geophysics Heat flux Hydrography Marine Numerical model Oceanography Oceans Physics of the oceans Simulation Studies Watermass Western disturbance |
| title | Growth and decay of the Arabian Sea mini warm pool during May 2000: Observations and simulations |
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