UnivTrevesV1, PascalFrancis, Curation, bibRecord, 000890

Changes in distribution of brine waters on the Laptev Sea shelf in 2007

Identifieur interne : 000890 ( PascalFrancis/Curation ); précédent : 000889; suivant : 000891

Changes in distribution of brine waters on the Laptev Sea shelf in 2007

Auteurs : D. Bauch [Allemagne] ; J. Hölemann [Allemagne] ; S. Willmes [Allemagne] ; M. Gröger [Allemagne] ; A. Novikhin [Russie] ; A. Nikulina [Allemagne] ; H. Kassens [Allemagne] ; L. Timokhov [Russie]

Source :

Journal of geophysical research [ 0148-0227 ] ; 2010.

RBID : Pascal:11-0056197

Descripteurs français

Pascal (Inist)
- Eau saumâtre, Salinité, Eté, Saumure, Eau rivière, Bilan masse, Eau fond, Couche superficielle, Masse eau, Mixage, Mélangeage, Plateforme continentale interne, Plateforme continentale externe, Hiver, Glace marine, Advection, Valeur extrême, Exportation, Océan Arctique, Halocline, Zone polaire, Mer de Laptev.
Wicri :
- topic : Exportation, Océan Arctique.

English descriptors

KwdEn :
- Arctic Ocean, Halocline, Laptev Sea, Mixing, Polar region, River water, Summer, Surface layer, Water mass, Winter, advection, bottom water, brackish water, brines, export, extreme value, inner shelf, mass balance, mixing, outer shelf, salinity, sea ice.

Abstract

[1] Combined salinity and δ¹⁸O data from summer 2007 reveal a significant change in brine production in the Laptev Sea relative to summer 1994. The distribution of river water and brine-enriched waters on the Laptev Sea shelf is derived based on mass balance calculations using salinity and δ¹⁸O data. While in 1994 maximal influence of brines is seen within bottom waters, in 2007 the influence of brines is highest within the surface layer and only a moderate influence of brines is observed in the bottom layer. In contrast to 2007, salinity and δ¹⁸O data from summer 1994 clearly identify a locally formed brine-enriched bottom water mass as mixing end-member between surface layer and inner shelf waters on one side and with higher salinity water from the outer Laptev Sea on the other side. In 2007, the brine-enriched waters are predominantly part of the surface regime, and the mixing end-member between surface layer and outer shelf waters is replaced by a relatively salty bottom water mass. This relatively salty bottom water probably originates from the western Laptev Sea. The inverted distribution of brines in the water column in 2007 relative to 1994 suggests a less effective winter sea ice formation in winter 2006-2007 combined with advection of more saline waters from the western Laptev Sea or the outer shelf precedent to the climatically extreme summer 2007. The observed changes result in an altered export of waters from the Laptev Sea to the Arctic Ocean halocline.

A01	`01`	`1`		`@0 0148-0227`
A03		`1`		`@0 J. geophys. res.`
A05				`@2 115`
A06				`@2 C11`
A08	`01`	`1`	`ENG`	`@1 Changes in distribution of brine waters on the Laptev Sea shelf in 2007`
A11	`01`	`1`		`@1 BAUCH (D.)`
A11	`02`	`1`		`@1 HÖLEMANN (J.)`
A11	`03`	`1`		`@1 WILLMES (S.)`
A11	`04`	`1`		`@1 GRÖGER (M.)`
A11	`05`	`1`		`@1 NOVIKHIN (A.)`
A11	`06`	`1`		`@1 NIKULINA (A.)`
A11	`07`	`1`		`@1 KASSENS (H.)`
A11	`08`	`1`		`@1 TIMOKHOV (L.)`
A14	`01`			`@1 Leibniz Institute of Marine Sciences (IFM-GEOMAR) @2 Kiel @3 DEU @Z 1 aut. @Z 6 aut. @Z 7 aut.`
A14	`02`			`@1 Alfred Wegener Institute for Polar and Marine Research (AWI) @2 Bremerhaven @3 DEU @Z 2 aut.`
A14	`03`			`@1 University of Trier @2 Trier @3 DEU @Z 3 aut.`
A14	`04`			`@1 MPI for Meteorology @2 Hamburg @3 DEU @Z 4 aut.`
A14	`05`			`@1 Arctic and Antarctic Research Institute (AARI) @2 Saint Petersburg @3 RUS @Z 5 aut. @Z 8 aut.`
A20				`@2 C11008.1-C11008.11`
A21				`@1 2010`
A23	`01`			`@0 ENG`
A43	`01`			`@1 INIST @2 3144 @5 354000191841680080`
A44				`@0 0000 @1 © 2011 INIST-CNRS. All rights reserved.`
A45				`@0 3/4 p.`
A47	`01`	`1`		`@0 11-0056197`
A60				`@1 P`
A61				`@0 A`
A64	`01`	`1`		`@0 Journal of geophysical research`
A66	`01`			`@0 USA`
C01	`01`		`ENG`	@0 [1] Combined salinity and δ¹⁸O data from summer 2007 reveal a significant change in brine production in the Laptev Sea relative to summer 1994. The distribution of river water and brine-enriched waters on the Laptev Sea shelf is derived based on mass balance calculations using salinity and δ¹⁸O data. While in 1994 maximal influence of brines is seen within bottom waters, in 2007 the influence of brines is highest within the surface layer and only a moderate influence of brines is observed in the bottom layer. In contrast to 2007, salinity and δ¹⁸O data from summer 1994 clearly identify a locally formed brine-enriched bottom water mass as mixing end-member between surface layer and inner shelf waters on one side and with higher salinity water from the outer Laptev Sea on the other side. In 2007, the brine-enriched waters are predominantly part of the surface regime, and the mixing end-member between surface layer and outer shelf waters is replaced by a relatively salty bottom water mass. This relatively salty bottom water probably originates from the western Laptev Sea. The inverted distribution of brines in the water column in 2007 relative to 1994 suggests a less effective winter sea ice formation in winter 2006-2007 combined with advection of more saline waters from the western Laptev Sea or the outer shelf precedent to the climatically extreme summer 2007. The observed changes result in an altered export of waters from the Laptev Sea to the Arctic Ocean halocline.
C02	`01`	`3`		`@0 001E`
C02	`02`	`2`		`@0 001E01`
C02	`03`	`2`		`@0 220`
C03	`01`	`2`	`FRE`	`@0 Eau saumâtre @5 01`
C03	`01`	`2`	`ENG`	`@0 brackish water @5 01`
C03	`01`	`2`	`SPA`	`@0 Agua salobre @5 01`
C03	`02`	`2`	`FRE`	`@0 Salinité @5 02`
C03	`02`	`2`	`ENG`	`@0 salinity @5 02`
C03	`02`	`2`	`SPA`	`@0 Salinidad @5 02`
C03	`03`	`X`	`FRE`	`@0 Eté @5 03`
C03	`03`	`X`	`ENG`	`@0 Summer @5 03`
C03	`03`	`X`	`SPA`	`@0 Verano @5 03`
C03	`04`	`2`	`FRE`	`@0 Saumure @5 04`
C03	`04`	`2`	`ENG`	`@0 brines @5 04`
C03	`04`	`2`	`SPA`	`@0 Salmuera @5 04`
C03	`05`	`X`	`FRE`	`@0 Eau rivière @5 05`
C03	`05`	`X`	`ENG`	`@0 River water @5 05`
C03	`05`	`X`	`SPA`	`@0 Agua río @5 05`
C03	`06`	`2`	`FRE`	`@0 Bilan masse @5 06`
C03	`06`	`2`	`ENG`	`@0 mass balance @5 06`
C03	`06`	`2`	`SPA`	`@0 Balance masa @5 06`
C03	`07`	`2`	`FRE`	`@0 Eau fond @5 07`
C03	`07`	`2`	`ENG`	`@0 bottom water @5 07`
C03	`07`	`2`	`SPA`	`@0 Agua fondo @5 07`
C03	`08`	`X`	`FRE`	`@0 Couche superficielle @5 08`
C03	`08`	`X`	`ENG`	`@0 Surface layer @5 08`
C03	`08`	`X`	`SPA`	`@0 Capa superficial @5 08`
C03	`09`	`X`	`FRE`	`@0 Masse eau @5 09`
C03	`09`	`X`	`ENG`	`@0 Water mass @5 09`
C03	`09`	`X`	`SPA`	`@0 Masa agua @5 09`
C03	`10`	`2`	`FRE`	`@0 Mixage @5 10`
C03	`10`	`2`	`ENG`	`@0 mixing @5 10`
C03	`10`	`2`	`SPA`	`@0 Mezcla @5 10`
C03	`11`	`X`	`FRE`	`@0 Mélangeage @5 11`
C03	`11`	`X`	`ENG`	`@0 Mixing @5 11`
C03	`11`	`X`	`SPA`	`@0 Mezclado @5 11`
C03	`12`	`2`	`FRE`	`@0 Plateforme continentale interne @5 12`
C03	`12`	`2`	`ENG`	`@0 inner shelf @5 12`
C03	`12`	`2`	`SPA`	`@0 Plataforma continental interna @5 12`
C03	`13`	`2`	`FRE`	`@0 Plateforme continentale externe @5 13`
C03	`13`	`2`	`ENG`	`@0 outer shelf @5 13`
C03	`13`	`2`	`SPA`	`@0 Plataforma continental externa @5 13`
C03	`14`	`X`	`FRE`	`@0 Hiver @5 14`
C03	`14`	`X`	`ENG`	`@0 Winter @5 14`
C03	`14`	`X`	`SPA`	`@0 Invierno @5 14`
C03	`15`	`2`	`FRE`	`@0 Glace marine @5 15`
C03	`15`	`2`	`ENG`	`@0 sea ice @5 15`
C03	`15`	`2`	`SPA`	`@0 Hielo marino @5 15`
C03	`16`	`2`	`FRE`	`@0 Advection @5 16`
C03	`16`	`2`	`ENG`	`@0 advection @5 16`
C03	`17`	`2`	`FRE`	`@0 Valeur extrême @5 17`
C03	`17`	`2`	`ENG`	`@0 extreme value @5 17`
C03	`18`	`2`	`FRE`	`@0 Exportation @5 18`
C03	`18`	`2`	`ENG`	`@0 export @5 18`
C03	`18`	`2`	`SPA`	`@0 Exportación @5 18`
C03	`19`	`2`	`FRE`	`@0 Océan Arctique @2 564 @5 19`
C03	`19`	`2`	`ENG`	`@0 Arctic Ocean @2 564 @5 19`
C03	`19`	`2`	`SPA`	`@0 Océano Ártico @2 564 @5 19`
C03	`20`	`X`	`FRE`	`@0 Halocline @5 20`
C03	`20`	`X`	`ENG`	`@0 Halocline @5 20`
C03	`20`	`X`	`SPA`	`@0 Haloclina @5 20`
C03	`21`	`X`	`FRE`	`@0 Zone polaire @5 21`
C03	`21`	`X`	`ENG`	`@0 Polar region @5 21`
C03	`21`	`X`	`SPA`	`@0 Zona polar @5 21`
C03	`22`	`2`	`FRE`	`@0 Mer de Laptev @2 NG @5 61`
C03	`22`	`2`	`ENG`	`@0 Laptev Sea @2 NG @5 61`
C03	`22`	`2`	`SPA`	`@0 Mar de Laptev @2 NG @5 61`
N21				`@1 038`
N44	`01`			`@1 OTO`
N82				`@1 OTO`

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Le document en format XML

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<author><name sortKey="Holemann, J" sort="Holemann, J" uniqKey="Holemann J" first="J." last="Hölemann">J. Hölemann</name>
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<author><name sortKey="Willmes, S" sort="Willmes, S" uniqKey="Willmes S" first="S." last="Willmes">S. Willmes</name>
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<author><name sortKey="Groger, M" sort="Groger, M" uniqKey="Groger M" first="M." last="Gröger">M. Gröger</name>
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<author><name sortKey="Nikulina, A" sort="Nikulina, A" uniqKey="Nikulina A" first="A." last="Nikulina">A. Nikulina</name>
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<author><name sortKey="Kassens, H" sort="Kassens, H" uniqKey="Kassens H" first="H." last="Kassens">H. Kassens</name>
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<author><name sortKey="Timokhov, L" sort="Timokhov, L" uniqKey="Timokhov L" first="L." last="Timokhov">L. Timokhov</name>
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<sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Changes in distribution of brine waters on the Laptev Sea shelf in 2007</title>
<author><name sortKey="Bauch, D" sort="Bauch, D" uniqKey="Bauch D" first="D." last="Bauch">D. Bauch</name>
<affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Leibniz Institute of Marine Sciences (IFM-GEOMAR)</s1>
<s2>Kiel</s2>
<s3>DEU</s3>
<sZ>1 aut.</sZ>
<sZ>6 aut.</sZ>
<sZ>7 aut.</sZ>
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<country>Allemagne</country>
</affiliation>
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<author><name sortKey="Holemann, J" sort="Holemann, J" uniqKey="Holemann J" first="J." last="Hölemann">J. Hölemann</name>
<affiliation wicri:level="1"><inist:fA14 i1="02"><s1>Alfred Wegener Institute for Polar and Marine Research (AWI)</s1>
<s2>Bremerhaven</s2>
<s3>DEU</s3>
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</inist:fA14>
<country>Allemagne</country>
</affiliation>
</author>
<author><name sortKey="Willmes, S" sort="Willmes, S" uniqKey="Willmes S" first="S." last="Willmes">S. Willmes</name>
<affiliation wicri:level="1"><inist:fA14 i1="03"><s1>University of Trier</s1>
<s2>Trier</s2>
<s3>DEU</s3>
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</inist:fA14>
<country>Allemagne</country>
</affiliation>
</author>
<author><name sortKey="Groger, M" sort="Groger, M" uniqKey="Groger M" first="M." last="Gröger">M. Gröger</name>
<affiliation wicri:level="1"><inist:fA14 i1="04"><s1>MPI for Meteorology</s1>
<s2>Hamburg</s2>
<s3>DEU</s3>
<sZ>4 aut.</sZ>
</inist:fA14>
<country>Allemagne</country>
</affiliation>
</author>
<author><name sortKey="Novikhin, A" sort="Novikhin, A" uniqKey="Novikhin A" first="A." last="Novikhin">A. Novikhin</name>
<affiliation wicri:level="1"><inist:fA14 i1="05"><s1>Arctic and Antarctic Research Institute (AARI)</s1>
<s2>Saint Petersburg</s2>
<s3>RUS</s3>
<sZ>5 aut.</sZ>
<sZ>8 aut.</sZ>
</inist:fA14>
<country>Russie</country>
</affiliation>
</author>
<author><name sortKey="Nikulina, A" sort="Nikulina, A" uniqKey="Nikulina A" first="A." last="Nikulina">A. Nikulina</name>
<affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Leibniz Institute of Marine Sciences (IFM-GEOMAR)</s1>
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</affiliation>
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<author><name sortKey="Kassens, H" sort="Kassens, H" uniqKey="Kassens H" first="H." last="Kassens">H. Kassens</name>
<affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Leibniz Institute of Marine Sciences (IFM-GEOMAR)</s1>
<s2>Kiel</s2>
<s3>DEU</s3>
<sZ>1 aut.</sZ>
<sZ>6 aut.</sZ>
<sZ>7 aut.</sZ>
</inist:fA14>
<country>Allemagne</country>
</affiliation>
</author>
<author><name sortKey="Timokhov, L" sort="Timokhov, L" uniqKey="Timokhov L" first="L." last="Timokhov">L. Timokhov</name>
<affiliation wicri:level="1"><inist:fA14 i1="05"><s1>Arctic and Antarctic Research Institute (AARI)</s1>
<s2>Saint Petersburg</s2>
<s3>RUS</s3>
<sZ>5 aut.</sZ>
<sZ>8 aut.</sZ>
</inist:fA14>
<country>Russie</country>
</affiliation>
</author>
</analytic>
<series><title level="j" type="main">Journal of geophysical research</title>
<title level="j" type="abbreviated">J. geophys. res.</title>
<idno type="ISSN">0148-0227</idno>
<imprint><date when="2010">2010</date>
</imprint>
</series>
</biblStruct>
</sourceDesc>
<seriesStmt><title level="j" type="main">Journal of geophysical research</title>
<title level="j" type="abbreviated">J. geophys. res.</title>
<idno type="ISSN">0148-0227</idno>
</seriesStmt>
</fileDesc>
<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Arctic Ocean</term>
<term>Halocline</term>
<term>Laptev Sea</term>
<term>Mixing</term>
<term>Polar region</term>
<term>River water</term>
<term>Summer</term>
<term>Surface layer</term>
<term>Water mass</term>
<term>Winter</term>
<term>advection</term>
<term>bottom water</term>
<term>brackish water</term>
<term>brines</term>
<term>export</term>
<term>extreme value</term>
<term>inner shelf</term>
<term>mass balance</term>
<term>mixing</term>
<term>outer shelf</term>
<term>salinity</term>
<term>sea ice</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Eau saumâtre</term>
<term>Salinité</term>
<term>Eté</term>
<term>Saumure</term>
<term>Eau rivière</term>
<term>Bilan masse</term>
<term>Eau fond</term>
<term>Couche superficielle</term>
<term>Masse eau</term>
<term>Mixage</term>
<term>Mélangeage</term>
<term>Plateforme continentale interne</term>
<term>Plateforme continentale externe</term>
<term>Hiver</term>
<term>Glace marine</term>
<term>Advection</term>
<term>Valeur extrême</term>
<term>Exportation</term>
<term>Océan Arctique</term>
<term>Halocline</term>
<term>Zone polaire</term>
<term>Mer de Laptev</term>
</keywords>
<keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Exportation</term>
<term>Océan Arctique</term>
</keywords>
</textClass>
</profileDesc>
</teiHeader>
<front><div type="abstract" xml:lang="en">[1] Combined salinity and δ<sup>18</sup>
O data from summer 2007 reveal a significant change in brine production in the Laptev Sea relative to summer 1994. The distribution of river water and brine-enriched waters on the Laptev Sea shelf is derived based on mass balance calculations using salinity and δ<sup>18</sup>
O data. While in 1994 maximal influence of brines is seen within bottom waters, in 2007 the influence of brines is highest within the surface layer and only a moderate influence of brines is observed in the bottom layer. In contrast to 2007, salinity and δ<sup>18</sup>
O data from summer 1994 clearly identify a locally formed brine-enriched bottom water mass as mixing end-member between surface layer and inner shelf waters on one side and with higher salinity water from the outer Laptev Sea on the other side. In 2007, the brine-enriched waters are predominantly part of the surface regime, and the mixing end-member between surface layer and outer shelf waters is replaced by a relatively salty bottom water mass. This relatively salty bottom water probably originates from the western Laptev Sea. The inverted distribution of brines in the water column in 2007 relative to 1994 suggests a less effective winter sea ice formation in winter 2006-2007 combined with advection of more saline waters from the western Laptev Sea or the outer shelf precedent to the climatically extreme summer 2007. The observed changes result in an altered export of waters from the Laptev Sea to the Arctic Ocean halocline.</div>
</front>
</TEI>
<inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0148-0227</s0>
</fA01>
<fA03 i2="1"><s0>J. geophys. res.</s0>
</fA03>
<fA05><s2>115</s2>
</fA05>
<fA06><s2>C11</s2>
</fA06>
<fA08 i1="01" i2="1" l="ENG"><s1>Changes in distribution of brine waters on the Laptev Sea shelf in 2007</s1>
</fA08>
<fA11 i1="01" i2="1"><s1>BAUCH (D.)</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>HÖLEMANN (J.)</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>WILLMES (S.)</s1>
</fA11>
<fA11 i1="04" i2="1"><s1>GRÖGER (M.)</s1>
</fA11>
<fA11 i1="05" i2="1"><s1>NOVIKHIN (A.)</s1>
</fA11>
<fA11 i1="06" i2="1"><s1>NIKULINA (A.)</s1>
</fA11>
<fA11 i1="07" i2="1"><s1>KASSENS (H.)</s1>
</fA11>
<fA11 i1="08" i2="1"><s1>TIMOKHOV (L.)</s1>
</fA11>
<fA14 i1="01"><s1>Leibniz Institute of Marine Sciences (IFM-GEOMAR)</s1>
<s2>Kiel</s2>
<s3>DEU</s3>
<sZ>1 aut.</sZ>
<sZ>6 aut.</sZ>
<sZ>7 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>Alfred Wegener Institute for Polar and Marine Research (AWI)</s1>
<s2>Bremerhaven</s2>
<s3>DEU</s3>
<sZ>2 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>University of Trier</s1>
<s2>Trier</s2>
<s3>DEU</s3>
<sZ>3 aut.</sZ>
</fA14>
<fA14 i1="04"><s1>MPI for Meteorology</s1>
<s2>Hamburg</s2>
<s3>DEU</s3>
<sZ>4 aut.</sZ>
</fA14>
<fA14 i1="05"><s1>Arctic and Antarctic Research Institute (AARI)</s1>
<s2>Saint Petersburg</s2>
<s3>RUS</s3>
<sZ>5 aut.</sZ>
<sZ>8 aut.</sZ>
</fA14>
<fA20><s2>C11008.1-C11008.11</s2>
</fA20>
<fA21><s1>2010</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
</fA23>
<fA43 i1="01"><s1>INIST</s1>
<s2>3144</s2>
<s5>354000191841680080</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 2011 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>3/4 p.</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>11-0056197</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Journal of geophysical research</s0>
</fA64>
<fA66 i1="01"><s0>USA</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>[1] Combined salinity and δ<sup>18</sup>
O data from summer 2007 reveal a significant change in brine production in the Laptev Sea relative to summer 1994. The distribution of river water and brine-enriched waters on the Laptev Sea shelf is derived based on mass balance calculations using salinity and δ<sup>18</sup>
O data. While in 1994 maximal influence of brines is seen within bottom waters, in 2007 the influence of brines is highest within the surface layer and only a moderate influence of brines is observed in the bottom layer. In contrast to 2007, salinity and δ<sup>18</sup>
O data from summer 1994 clearly identify a locally formed brine-enriched bottom water mass as mixing end-member between surface layer and inner shelf waters on one side and with higher salinity water from the outer Laptev Sea on the other side. In 2007, the brine-enriched waters are predominantly part of the surface regime, and the mixing end-member between surface layer and outer shelf waters is replaced by a relatively salty bottom water mass. This relatively salty bottom water probably originates from the western Laptev Sea. The inverted distribution of brines in the water column in 2007 relative to 1994 suggests a less effective winter sea ice formation in winter 2006-2007 combined with advection of more saline waters from the western Laptev Sea or the outer shelf precedent to the climatically extreme summer 2007. The observed changes result in an altered export of waters from the Laptev Sea to the Arctic Ocean halocline.</s0>
</fC01>
<fC02 i1="01" i2="3"><s0>001E</s0>
</fC02>
<fC02 i1="02" i2="2"><s0>001E01</s0>
</fC02>
<fC02 i1="03" i2="2"><s0>220</s0>
</fC02>
<fC03 i1="01" i2="2" l="FRE"><s0>Eau saumâtre</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="ENG"><s0>brackish water</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="SPA"><s0>Agua salobre</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="2" l="FRE"><s0>Salinité</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="ENG"><s0>salinity</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="SPA"><s0>Salinidad</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE"><s0>Eté</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="ENG"><s0>Summer</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA"><s0>Verano</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Saumure</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>brines</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="SPA"><s0>Salmuera</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE"><s0>Eau rivière</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG"><s0>River water</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA"><s0>Agua río</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Bilan masse</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>mass balance</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA"><s0>Balance masa</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>Eau fond</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>bottom water</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="SPA"><s0>Agua fondo</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE"><s0>Couche superficielle</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG"><s0>Surface layer</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA"><s0>Capa superficial</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Masse eau</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG"><s0>Water mass</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Masa agua</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Mixage</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>mixing</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Mezcla</s0>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="X" l="FRE"><s0>Mélangeage</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="ENG"><s0>Mixing</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="SPA"><s0>Mezclado</s0>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Plateforme continentale interne</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>inner shelf</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Plataforma continental interna</s0>
<s5>12</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Plateforme continentale externe</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG"><s0>outer shelf</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="SPA"><s0>Plataforma continental externa</s0>
<s5>13</s5>
</fC03>
<fC03 i1="14" i2="X" l="FRE"><s0>Hiver</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="ENG"><s0>Winter</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="SPA"><s0>Invierno</s0>
<s5>14</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Glace marine</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>sea ice</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="SPA"><s0>Hielo marino</s0>
<s5>15</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Advection</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>advection</s0>
<s5>16</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Valeur extrême</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>extreme value</s0>
<s5>17</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>Exportation</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG"><s0>export</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="SPA"><s0>Exportación</s0>
<s5>18</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>Océan Arctique</s0>
<s2>564</s2>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG"><s0>Arctic Ocean</s0>
<s2>564</s2>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="2" l="SPA"><s0>Océano Ártico</s0>
<s2>564</s2>
<s5>19</s5>
</fC03>
<fC03 i1="20" i2="X" l="FRE"><s0>Halocline</s0>
<s5>20</s5>
</fC03>
<fC03 i1="20" i2="X" l="ENG"><s0>Halocline</s0>
<s5>20</s5>
</fC03>
<fC03 i1="20" i2="X" l="SPA"><s0>Haloclina</s0>
<s5>20</s5>
</fC03>
<fC03 i1="21" i2="X" l="FRE"><s0>Zone polaire</s0>
<s5>21</s5>
</fC03>
<fC03 i1="21" i2="X" l="ENG"><s0>Polar region</s0>
<s5>21</s5>
</fC03>
<fC03 i1="21" i2="X" l="SPA"><s0>Zona polar</s0>
<s5>21</s5>
</fC03>
<fC03 i1="22" i2="2" l="FRE"><s0>Mer de Laptev</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="22" i2="2" l="ENG"><s0>Laptev Sea</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="22" i2="2" l="SPA"><s0>Mar de Laptev</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fN21><s1>038</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
</inist>
</record>

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Changes in distribution of brine waters on the Laptev Sea shelf in 2007

Changes in distribution of brine waters on the Laptev Sea shelf in 2007

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