Fine resolution 3D temperature fields off Kerguelen from instrumented penguins
The use of diving animals as autonomous vectors of oceanographic instruments is rapidly increasing, because this approach yields cost-efficient new information and can be used in previously poorly sampled areas. However, methods for analyzing the collected data are still under development. In partic...
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description | The use of diving animals as autonomous vectors of oceanographic instruments is rapidly increasing, because this approach yields cost-efficient new information and can be used in previously poorly sampled areas. However, methods for analyzing the collected data are still under development. In particular, difficulties may arise from the heterogeneous data distribution linked to animals’ behavior. Here we show how raw temperature data collected by penguin-borne loggers were transformed to a regular gridded dataset that provided new information on the local circulation off Kerguelen. A total of 16 king penguins (
Aptenodytes patagonicus) were equipped with satellite-positioning transmitters and with temperature–time–depth recorders (TTDRs) to record dive depth and sea temperature. The penguins’ foraging trips recorded during five summers ranged from 140 to 600
km from the colony and 11,000 dives >100
m were recorded. Temperature measurements recorded during diving were used to produce detailed 3D temperature fields of the area (0–200
m). The data treatment included dive location, determination of the vertical profile for each dive, averaging and gridding of those profiles onto 0.1°×0.1°
cells, and optimal interpolation in both the horizontal and vertical using an objective analysis. Horizontal fields of temperature at the surface and 100
m are presented, as well as a vertical section along the main foraging direction of the penguins. Compared to conventional temperature databases (Levitus World Ocean Atlas and historical stations available in the area), the 3D temperature fields collected from penguins are extremely finely resolved, by one order finer. Although TTDRs were less accurate than conventional instruments, such a high spatial resolution of penguin-derived data provided unprecedented detailed information on the upper level circulation pattern east of Kerguelen, as well as the iron-enrichment mechanism leading to a high primary production over the Kerguelen Plateau. |
doi_str_mv | 10.1016/j.dsr.2004.07.019 |
format | Article |
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Aptenodytes patagonicus) were equipped with satellite-positioning transmitters and with temperature–time–depth recorders (TTDRs) to record dive depth and sea temperature. The penguins’ foraging trips recorded during five summers ranged from 140 to 600
km from the colony and 11,000 dives >100
m were recorded. Temperature measurements recorded during diving were used to produce detailed 3D temperature fields of the area (0–200
m). The data treatment included dive location, determination of the vertical profile for each dive, averaging and gridding of those profiles onto 0.1°×0.1°
cells, and optimal interpolation in both the horizontal and vertical using an objective analysis. Horizontal fields of temperature at the surface and 100
m are presented, as well as a vertical section along the main foraging direction of the penguins. Compared to conventional temperature databases (Levitus World Ocean Atlas and historical stations available in the area), the 3D temperature fields collected from penguins are extremely finely resolved, by one order finer. Although TTDRs were less accurate than conventional instruments, such a high spatial resolution of penguin-derived data provided unprecedented detailed information on the upper level circulation pattern east of Kerguelen, as well as the iron-enrichment mechanism leading to a high primary production over the Kerguelen Plateau.</description><identifier>ISSN: 0967-0637</identifier><identifier>ISSN: 0146-6291</identifier><identifier>EISSN: 1879-0119</identifier><identifier>DOI: 10.1016/j.dsr.2004.07.019</identifier><language>eng</language><publisher>Oxford: Elsevier Ltd</publisher><subject>Aptenodytes patagonicus ; Bio-logging ; Biodiversity and Ecology ; Biotelemetry ; Coastal oceanography, estuaries. Regional oceanography ; Data collection ; Earth, ocean, space ; Environment and Society ; Environmental Sciences ; Exact sciences and technology ; External geophysics ; Geophysics. Techniques, methods, instrumentation and models ; Global Changes ; Kerguelen ; Marine ; Marine mammals ; Oceanography ; Penguins ; Physics of the oceans ; Regional circulation ; Sea temperature ; Temperature</subject><ispartof>Deep-sea research (1977), 2004-12, Vol.51 (12), p.2091-2103</ispartof><rights>2004 Elsevier Ltd</rights><rights>2005 INIST-CNRS</rights><rights>Copyright Pergamon Press Inc. Dec 2004</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c417t-751a2ff0727b8bada34ea1c3a2d38da253fb394b00e0d1ab2279206781642a523</citedby><cites>FETCH-LOGICAL-c417t-751a2ff0727b8bada34ea1c3a2d38da253fb394b00e0d1ab2279206781642a523</cites><orcidid>0000-0002-7547-5540 ; 0000-0002-5259-9073 ; 0000-0003-1679-6974</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0967063704001578$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,881,3536,27903,27904,65309</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=16327433$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://hal.science/hal-00186827$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Charrassin, Jean-Benoît</creatorcontrib><creatorcontrib>Park, Young-Hyang</creatorcontrib><creatorcontrib>Le Maho, Yvon</creatorcontrib><creatorcontrib>Bost, Charles-André</creatorcontrib><title>Fine resolution 3D temperature fields off Kerguelen from instrumented penguins</title><title>Deep-sea research (1977)</title><description>The use of diving animals as autonomous vectors of oceanographic instruments is rapidly increasing, because this approach yields cost-efficient new information and can be used in previously poorly sampled areas. However, methods for analyzing the collected data are still under development. In particular, difficulties may arise from the heterogeneous data distribution linked to animals’ behavior. Here we show how raw temperature data collected by penguin-borne loggers were transformed to a regular gridded dataset that provided new information on the local circulation off Kerguelen. A total of 16 king penguins (
Aptenodytes patagonicus) were equipped with satellite-positioning transmitters and with temperature–time–depth recorders (TTDRs) to record dive depth and sea temperature. The penguins’ foraging trips recorded during five summers ranged from 140 to 600
km from the colony and 11,000 dives >100
m were recorded. Temperature measurements recorded during diving were used to produce detailed 3D temperature fields of the area (0–200
m). The data treatment included dive location, determination of the vertical profile for each dive, averaging and gridding of those profiles onto 0.1°×0.1°
cells, and optimal interpolation in both the horizontal and vertical using an objective analysis. Horizontal fields of temperature at the surface and 100
m are presented, as well as a vertical section along the main foraging direction of the penguins. Compared to conventional temperature databases (Levitus World Ocean Atlas and historical stations available in the area), the 3D temperature fields collected from penguins are extremely finely resolved, by one order finer. Although TTDRs were less accurate than conventional instruments, such a high spatial resolution of penguin-derived data provided unprecedented detailed information on the upper level circulation pattern east of Kerguelen, as well as the iron-enrichment mechanism leading to a high primary production over the Kerguelen Plateau.</description><subject>Aptenodytes patagonicus</subject><subject>Bio-logging</subject><subject>Biodiversity and Ecology</subject><subject>Biotelemetry</subject><subject>Coastal oceanography, estuaries. Regional oceanography</subject><subject>Data collection</subject><subject>Earth, ocean, space</subject><subject>Environment and Society</subject><subject>Environmental Sciences</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Geophysics. Techniques, methods, instrumentation and models</subject><subject>Global Changes</subject><subject>Kerguelen</subject><subject>Marine</subject><subject>Marine mammals</subject><subject>Oceanography</subject><subject>Penguins</subject><subject>Physics of the oceans</subject><subject>Regional circulation</subject><subject>Sea temperature</subject><subject>Temperature</subject><issn>0967-0637</issn><issn>0146-6291</issn><issn>1879-0119</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2004</creationdate><recordtype>article</recordtype><recordid>eNp9kUGLFDEQhYMoOK7-AG9BUPDQbSXpSbrxtKy7rjjsXvQc0kllzdCdjEn3gv9-M86i4MFTweN7r6h6hLxm0DJg8sO-dSW3HKBrQbXAhidkw3o1NMDY8JRsYJCqASnUc_KilD1ANfWwITdXISLNWNK0LiFFKj7RBecDZrOsGakPOLlCk_f0K-a7FSeM1Oc00xDLktcZ44KOHjDerVV5SZ55MxV89TjPyPery28X183u9vOXi_NdYzumlkZtmeHeg-Jq7EfjjOjQMCsMd6J3hm-FH8XQjQAIjpmRczVwkKpnsuNmy8UZeX_K_WEmfchhNvmXTibo6_OdPmr1vl72XN2zyr47sYecfq5YFj2HYnGaTMS0Fs1UvxXqd-ibf8B9WnOsd2g2SKmkgqFC7ATZnErJ6P-sZ6CPVei9rlXoYxUalK5VVM_bx2BTrJl8NtGG8tcoBVedEJX7eOKwvu4-YNbFBowWXchoF-1S-M-WBxUpnN0</recordid><startdate>20041201</startdate><enddate>20041201</enddate><creator>Charrassin, Jean-Benoît</creator><creator>Park, Young-Hyang</creator><creator>Le Maho, Yvon</creator><creator>Bost, Charles-André</creator><general>Elsevier Ltd</general><general>Elsevier</general><general>Pergamon Press Inc</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H95</scope><scope>H96</scope><scope>L.G</scope><scope>1XC</scope><orcidid>https://orcid.org/0000-0002-7547-5540</orcidid><orcidid>https://orcid.org/0000-0002-5259-9073</orcidid><orcidid>https://orcid.org/0000-0003-1679-6974</orcidid></search><sort><creationdate>20041201</creationdate><title>Fine resolution 3D temperature fields off Kerguelen from instrumented penguins</title><author>Charrassin, Jean-Benoît ; Park, Young-Hyang ; Le Maho, Yvon ; Bost, Charles-André</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c417t-751a2ff0727b8bada34ea1c3a2d38da253fb394b00e0d1ab2279206781642a523</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2004</creationdate><topic>Aptenodytes patagonicus</topic><topic>Bio-logging</topic><topic>Biodiversity and Ecology</topic><topic>Biotelemetry</topic><topic>Coastal oceanography, estuaries. Regional oceanography</topic><topic>Data collection</topic><topic>Earth, ocean, space</topic><topic>Environment and Society</topic><topic>Environmental Sciences</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Geophysics. Techniques, methods, instrumentation and models</topic><topic>Global Changes</topic><topic>Kerguelen</topic><topic>Marine</topic><topic>Marine mammals</topic><topic>Oceanography</topic><topic>Penguins</topic><topic>Physics of the oceans</topic><topic>Regional circulation</topic><topic>Sea temperature</topic><topic>Temperature</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Charrassin, Jean-Benoît</creatorcontrib><creatorcontrib>Park, Young-Hyang</creatorcontrib><creatorcontrib>Le Maho, Yvon</creatorcontrib><creatorcontrib>Bost, Charles-André</creatorcontrib><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) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Deep-sea research (1977)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Charrassin, Jean-Benoît</au><au>Park, Young-Hyang</au><au>Le Maho, Yvon</au><au>Bost, Charles-André</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Fine resolution 3D temperature fields off Kerguelen from instrumented penguins</atitle><jtitle>Deep-sea research (1977)</jtitle><date>2004-12-01</date><risdate>2004</risdate><volume>51</volume><issue>12</issue><spage>2091</spage><epage>2103</epage><pages>2091-2103</pages><issn>0967-0637</issn><issn>0146-6291</issn><eissn>1879-0119</eissn><abstract>The use of diving animals as autonomous vectors of oceanographic instruments is rapidly increasing, because this approach yields cost-efficient new information and can be used in previously poorly sampled areas. However, methods for analyzing the collected data are still under development. In particular, difficulties may arise from the heterogeneous data distribution linked to animals’ behavior. Here we show how raw temperature data collected by penguin-borne loggers were transformed to a regular gridded dataset that provided new information on the local circulation off Kerguelen. A total of 16 king penguins (
Aptenodytes patagonicus) were equipped with satellite-positioning transmitters and with temperature–time–depth recorders (TTDRs) to record dive depth and sea temperature. The penguins’ foraging trips recorded during five summers ranged from 140 to 600
km from the colony and 11,000 dives >100
m were recorded. Temperature measurements recorded during diving were used to produce detailed 3D temperature fields of the area (0–200
m). The data treatment included dive location, determination of the vertical profile for each dive, averaging and gridding of those profiles onto 0.1°×0.1°
cells, and optimal interpolation in both the horizontal and vertical using an objective analysis. Horizontal fields of temperature at the surface and 100
m are presented, as well as a vertical section along the main foraging direction of the penguins. Compared to conventional temperature databases (Levitus World Ocean Atlas and historical stations available in the area), the 3D temperature fields collected from penguins are extremely finely resolved, by one order finer. Although TTDRs were less accurate than conventional instruments, such a high spatial resolution of penguin-derived data provided unprecedented detailed information on the upper level circulation pattern east of Kerguelen, as well as the iron-enrichment mechanism leading to a high primary production over the Kerguelen Plateau.</abstract><cop>Oxford</cop><pub>Elsevier Ltd</pub><doi>10.1016/j.dsr.2004.07.019</doi><tpages>13</tpages><orcidid>https://orcid.org/0000-0002-7547-5540</orcidid><orcidid>https://orcid.org/0000-0002-5259-9073</orcidid><orcidid>https://orcid.org/0000-0003-1679-6974</orcidid></addata></record> |
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subjects | Aptenodytes patagonicus Bio-logging Biodiversity and Ecology Biotelemetry Coastal oceanography, estuaries. Regional oceanography Data collection Earth, ocean, space Environment and Society Environmental Sciences Exact sciences and technology External geophysics Geophysics. Techniques, methods, instrumentation and models Global Changes Kerguelen Marine Marine mammals Oceanography Penguins Physics of the oceans Regional circulation Sea temperature Temperature |
title | Fine resolution 3D temperature fields off Kerguelen from instrumented penguins |
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