AustralieFrV1, PascalFrancis, Curation, bibRecord, 003C68

Direct evidence of the South Java Current system in Ombai Strait

Identifieur interne : 003C68 ( PascalFrancis/Curation ); précédent : 003C67; suivant : 003C69

Direct evidence of the South Java Current system in Ombai Strait

Auteurs : Janet Sprintall [États-Unis] ; Susan Wijffels [Australie] ; Robert Molcard [France] ; Indra Jaya [Indonésie]

Source :

Dynamics of atmospheres and oceans [ 0377-0265 ] ; 2010.

RBID : Pascal:10-0455020

Descripteurs français

Pascal (Inist)
- Détroit, Mesure vitesse, Courant superficiel, Sous courant, Modélisation, Série temporelle, Amarrage, Onde Kelvin, Onde forcée, Vent local, Action vent, Mousson, Couche superficielle, Température superficielle, Cartographie, Topographie, Vent Ouest, Rafale, Variation interannuelle, Variabilité climatique, Java, Mer de Savu, Océan Indien, Mers d'Indonésie, Courant marin, Climatologie dynamique, ITF.
Wicri :
- topic : Détroit, Cartographie, Océan Indien.

English descriptors

KwdEn :
- Dynamical climatology, Forced wave, Gust, Indian Ocean, Indonesian Seas, Indonesian throughflow, Interannual variation, Java, Kelvin wave, Local wind, Modeling, Mooring, Savu Sea, Speed measurement, Strait, Surface current, Surface layer, Surface temperature, Time series, Undercurrent, Westerly wind, Wind effect, cartography, climate variability, monsoons, ocean currents, topography.

Abstract

Direct velocity measurements from 2004 through 2006 confirm the eastward flowing surface South Java Current (SJC) and its deeper Undercurrent (SJUC) crosses the Savu Sea to reach Ombai Strait, a main outflow portal of the Indonesian Throughflow (ITF). The extension of the South Java Current system into Ombai Strait was hinted at by earlier measurement and modeling studies, but the 3-year velocity time series from two moorings in Ombai Strait clearly show separate distinct cores of flow in the SJC and SJUC. The deeper SJUC is driven by Kelvin waves forced by intraseasonal and semi-annual winds in the equatorial Indian Ocean and, when present, is observed across the entire strait. Eastward flow in the surface SJC is near year-round, although it appears that the mechanisms responsible for this flow differ throughout the year. Both the wind-driven Ekman flow during the northwest monsoon and the strongest semi-annual Kelvin waves that have surface signatures can result in eastward surface layer flow across the entire strait. In contrast, during the southeast monsoon the SJC has a subsurface maximum eastward flow at 50-100 m depth in the northern part of Ombai Strait, while the westward ITF is at an annual maximum at the surface in the southern part of the strait. Surface temperature maps suggest the presence of a front during the southeast monsoon that seems to trap the SJC to within ˜10-15 km of the northern boundary of Ombai Strait. The SJC and the frontal location are related to a complex interplay between local wind-driven Ekman dynamics, the strong ITF flow and topography. Significant energy is found at short intraseasonal time scales (20-60 days) in the along-strait flow that is probably related to the short duration westerly wind bursts that drive the Kelvin waves into Ombai Strait. There is a distinct lack of energy at longer intraseasonal time scales (60-90 days) that is likely attributable to interannual climate variability.

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A08	`01`	`1`	`ENG`	`@1 Direct evidence of the South Java Current system in Ombai Strait`
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A14	`04`			`@1 Department of Marine Sciences and Technology, Bogor Agricultural University @2 Bogor @3 IDN @Z 4 aut.`
A15	`01`			`@1 Lamont-Doherty Earth Observatory, Columbia University @3 USA @Z 1 aut.`
A15	`02`			`@1 Department of Marine Science, The University of Southern Mississippi @3 USA @Z 2 aut.`
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C01	`01`		`ENG`	@0 Direct velocity measurements from 2004 through 2006 confirm the eastward flowing surface South Java Current (SJC) and its deeper Undercurrent (SJUC) crosses the Savu Sea to reach Ombai Strait, a main outflow portal of the Indonesian Throughflow (ITF). The extension of the South Java Current system into Ombai Strait was hinted at by earlier measurement and modeling studies, but the 3-year velocity time series from two moorings in Ombai Strait clearly show separate distinct cores of flow in the SJC and SJUC. The deeper SJUC is driven by Kelvin waves forced by intraseasonal and semi-annual winds in the equatorial Indian Ocean and, when present, is observed across the entire strait. Eastward flow in the surface SJC is near year-round, although it appears that the mechanisms responsible for this flow differ throughout the year. Both the wind-driven Ekman flow during the northwest monsoon and the strongest semi-annual Kelvin waves that have surface signatures can result in eastward surface layer flow across the entire strait. In contrast, during the southeast monsoon the SJC has a subsurface maximum eastward flow at 50-100 m depth in the northern part of Ombai Strait, while the westward ITF is at an annual maximum at the surface in the southern part of the strait. Surface temperature maps suggest the presence of a front during the southeast monsoon that seems to trap the SJC to within ˜10-15 km of the northern boundary of Ombai Strait. The SJC and the frontal location are related to a complex interplay between local wind-driven Ekman dynamics, the strong ITF flow and topography. Significant energy is found at short intraseasonal time scales (20-60 days) in the along-strait flow that is probably related to the short duration westerly wind bursts that drive the Kelvin waves into Ombai Strait. There is a distinct lack of energy at longer intraseasonal time scales (60-90 days) that is likely attributable to interannual climate variability.
C02	`01`	`2`		`@0 001E02B05`
C02	`02`	`2`		`@0 001E02D10`
C03	`01`	`X`	`FRE`	`@0 Détroit @5 01`
C03	`01`	`X`	`ENG`	`@0 Strait @5 01`
C03	`01`	`X`	`SPA`	`@0 Estrecho @5 01`
C03	`02`	`X`	`FRE`	`@0 Mesure vitesse @5 02`
C03	`02`	`X`	`ENG`	`@0 Speed measurement @5 02`
C03	`02`	`X`	`SPA`	`@0 Medida velocidad @5 02`
C03	`03`	`X`	`FRE`	`@0 Courant superficiel @5 03`
C03	`03`	`X`	`ENG`	`@0 Surface current @5 03`
C03	`03`	`X`	`SPA`	`@0 Corriente superficial @5 03`
C03	`04`	`X`	`FRE`	`@0 Sous courant @5 04`
C03	`04`	`X`	`ENG`	`@0 Undercurrent @5 04`
C03	`04`	`X`	`SPA`	`@0 Hipocorriente @5 04`
C03	`05`	`X`	`FRE`	`@0 Modélisation @5 05`
C03	`05`	`X`	`ENG`	`@0 Modeling @5 05`
C03	`05`	`X`	`SPA`	`@0 Modelización @5 05`
C03	`06`	`X`	`FRE`	`@0 Série temporelle @5 06`
C03	`06`	`X`	`ENG`	`@0 Time series @5 06`
C03	`06`	`X`	`SPA`	`@0 Serie temporal @5 06`
C03	`07`	`X`	`FRE`	`@0 Amarrage @5 07`
C03	`07`	`X`	`ENG`	`@0 Mooring @5 07`
C03	`07`	`X`	`SPA`	`@0 Amarre @5 07`
C03	`08`	`X`	`FRE`	`@0 Onde Kelvin @5 08`
C03	`08`	`X`	`ENG`	`@0 Kelvin wave @5 08`
C03	`08`	`X`	`SPA`	`@0 Onda Kelvin @5 08`
C03	`09`	`X`	`FRE`	`@0 Onde forcée @5 09`
C03	`09`	`X`	`ENG`	`@0 Forced wave @5 09`
C03	`09`	`X`	`SPA`	`@0 Onda forzada @5 09`
C03	`10`	`X`	`FRE`	`@0 Vent local @5 10`
C03	`10`	`X`	`ENG`	`@0 Local wind @5 10`
C03	`10`	`X`	`SPA`	`@0 Viento local @5 10`
C03	`11`	`X`	`FRE`	`@0 Action vent @5 11`
C03	`11`	`X`	`ENG`	`@0 Wind effect @5 11`
C03	`11`	`X`	`SPA`	`@0 Acción viento @5 11`
C03	`12`	`2`	`FRE`	`@0 Mousson @5 12`
C03	`12`	`2`	`ENG`	`@0 monsoons @5 12`
C03	`12`	`2`	`SPA`	`@0 Monzón @5 12`
C03	`13`	`X`	`FRE`	`@0 Couche superficielle @5 13`
C03	`13`	`X`	`ENG`	`@0 Surface layer @5 13`
C03	`13`	`X`	`SPA`	`@0 Capa superficial @5 13`
C03	`14`	`X`	`FRE`	`@0 Température superficielle @5 14`
C03	`14`	`X`	`ENG`	`@0 Surface temperature @5 14`
C03	`14`	`X`	`SPA`	`@0 Temperatura superficial @5 14`
C03	`15`	`2`	`FRE`	`@0 Cartographie @5 15`
C03	`15`	`2`	`ENG`	`@0 cartography @5 15`
C03	`15`	`2`	`SPA`	`@0 Cartografía @5 15`
C03	`16`	`2`	`FRE`	`@0 Topographie @5 16`
C03	`16`	`2`	`ENG`	`@0 topography @5 16`
C03	`16`	`2`	`SPA`	`@0 Topografía @5 16`
C03	`17`	`X`	`FRE`	`@0 Vent Ouest @5 17`
C03	`17`	`X`	`ENG`	`@0 Westerly wind @5 17`
C03	`17`	`X`	`SPA`	`@0 Viento oeste @5 17`
C03	`18`	`X`	`FRE`	`@0 Rafale @5 18`
C03	`18`	`X`	`ENG`	`@0 Gust @5 18`
C03	`18`	`X`	`SPA`	`@0 Ráfaga @5 18`
C03	`19`	`X`	`FRE`	`@0 Variation interannuelle @5 19`
C03	`19`	`X`	`ENG`	`@0 Interannual variation @5 19`
C03	`19`	`X`	`SPA`	`@0 Variación interanual @5 19`
C03	`20`	`2`	`FRE`	`@0 Variabilité climatique @5 20`
C03	`20`	`2`	`ENG`	`@0 climate variability @5 20`
C03	`21`	`2`	`FRE`	`@0 Java @2 NG @5 21`
C03	`21`	`2`	`ENG`	`@0 Java @2 NG @5 21`
C03	`21`	`2`	`SPA`	`@0 Java @2 NG @5 21`
C03	`22`	`X`	`FRE`	`@0 Mer de Savu @2 NG @5 22`
C03	`22`	`X`	`ENG`	`@0 Savu Sea @2 NG @5 22`
C03	`22`	`X`	`SPA`	`@0 Mar de Savu @2 NG @5 22`
C03	`23`	`2`	`FRE`	`@0 Océan Indien @2 564 @5 23`
C03	`23`	`2`	`ENG`	`@0 Indian Ocean @2 564 @5 23`
C03	`23`	`2`	`SPA`	`@0 Océano Indico @2 564 @5 23`
C03	`24`	`2`	`FRE`	`@0 Mers d'Indonésie @2 NG @5 41`
C03	`24`	`2`	`ENG`	`@0 Indonesian Seas @2 NG @5 41`
C03	`24`	`2`	`SPA`	`@0 Mares de Indonesia @2 NG @5 41`
C03	`25`	`2`	`FRE`	`@0 Courant marin @5 42`
C03	`25`	`2`	`ENG`	`@0 ocean currents @5 42`
C03	`25`	`2`	`SPA`	`@0 Corriente marina @5 42`
C03	`26`	`X`	`FRE`	`@0 Climatologie dynamique @5 43`
C03	`26`	`X`	`ENG`	`@0 Dynamical climatology @5 43`
C03	`26`	`X`	`SPA`	`@0 Climatología dinámica @5 43`
C03	`27`	`2`	`FRE`	`@0 ITF @4 CD @5 96`
C03	`27`	`2`	`ENG`	`@0 Indonesian throughflow @4 CD @5 96`
C03	`27`	`2`	`SPA`	`@0 ITF @4 CD @5 96`
C07	`01`	`2`	`FRE`	`@0 Indonésie @2 NG`
C07	`01`	`2`	`ENG`	`@0 Indonesia @2 NG`
C07	`01`	`2`	`SPA`	`@0 Indonesia @2 NG`
C07	`02`	`2`	`FRE`	`@0 Extrême Orient @2 NG`
C07	`02`	`2`	`ENG`	`@0 Far East @2 NG`
C07	`02`	`2`	`SPA`	`@0 Extremo Oriente @2 NG`
C07	`03`	`2`	`FRE`	`@0 Asie @2 564`
C07	`03`	`2`	`ENG`	`@0 Asia @2 564`
C07	`03`	`2`	`SPA`	`@0 Asia @2 564`
C07	`04`	`X`	`FRE`	`@0 Mers d'Indonésie @2 NG`
C07	`04`	`X`	`ENG`	`@0 Indonesian Seas @2 NG`
C07	`04`	`X`	`SPA`	`@0 Mares de Indonesia @2 NG`
C07	`05`	`2`	`FRE`	`@0 Océan Pacifique Ouest @2 NG`
C07	`05`	`2`	`ENG`	`@0 West Pacific @2 NG`
C07	`06`	`2`	`FRE`	`@0 Océan Pacifique @2 564`
C07	`06`	`2`	`ENG`	`@0 Pacific Ocean @2 564`
C07	`06`	`2`	`SPA`	`@0 Océano Pacífico @2 564`
N21				`@1 298`
N44	`01`			`@1 OTO`
N82				`@1 OTO`

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Le document en format XML

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<term>Indonesian Seas</term>
<term>Indonesian throughflow</term>
<term>Interannual variation</term>
<term>Java</term>
<term>Kelvin wave</term>
<term>Local wind</term>
<term>Modeling</term>
<term>Mooring</term>
<term>Savu Sea</term>
<term>Speed measurement</term>
<term>Strait</term>
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<term>Surface layer</term>
<term>Surface temperature</term>
<term>Time series</term>
<term>Undercurrent</term>
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<term>climate variability</term>
<term>monsoons</term>
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<term>Mesure vitesse</term>
<term>Courant superficiel</term>
<term>Sous courant</term>
<term>Modélisation</term>
<term>Série temporelle</term>
<term>Amarrage</term>
<term>Onde Kelvin</term>
<term>Onde forcée</term>
<term>Vent local</term>
<term>Action vent</term>
<term>Mousson</term>
<term>Couche superficielle</term>
<term>Température superficielle</term>
<term>Cartographie</term>
<term>Topographie</term>
<term>Vent Ouest</term>
<term>Rafale</term>
<term>Variation interannuelle</term>
<term>Variabilité climatique</term>
<term>Java</term>
<term>Mer de Savu</term>
<term>Océan Indien</term>
<term>Mers d'Indonésie</term>
<term>Courant marin</term>
<term>Climatologie dynamique</term>
<term>ITF</term>
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<keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Détroit</term>
<term>Cartographie</term>
<term>Océan Indien</term>
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<front><div type="abstract" xml:lang="en">Direct velocity measurements from 2004 through 2006 confirm the eastward flowing surface South Java Current (SJC) and its deeper Undercurrent (SJUC) crosses the Savu Sea to reach Ombai Strait, a main outflow portal of the Indonesian Throughflow (ITF). The extension of the South Java Current system into Ombai Strait was hinted at by earlier measurement and modeling studies, but the 3-year velocity time series from two moorings in Ombai Strait clearly show separate distinct cores of flow in the SJC and SJUC. The deeper SJUC is driven by Kelvin waves forced by intraseasonal and semi-annual winds in the equatorial Indian Ocean and, when present, is observed across the entire strait. Eastward flow in the surface SJC is near year-round, although it appears that the mechanisms responsible for this flow differ throughout the year. Both the wind-driven Ekman flow during the northwest monsoon and the strongest semi-annual Kelvin waves that have surface signatures can result in eastward surface layer flow across the entire strait. In contrast, during the southeast monsoon the SJC has a subsurface maximum eastward flow at 50-100 m depth in the northern part of Ombai Strait, while the westward ITF is at an annual maximum at the surface in the southern part of the strait. Surface temperature maps suggest the presence of a front during the southeast monsoon that seems to trap the SJC to within ˜10-15 km of the northern boundary of Ombai Strait. The SJC and the frontal location are related to a complex interplay between local wind-driven Ekman dynamics, the strong ITF flow and topography. Significant energy is found at short intraseasonal time scales (20-60 days) in the along-strait flow that is probably related to the short duration westerly wind bursts that drive the Kelvin waves into Ombai Strait. There is a distinct lack of energy at longer intraseasonal time scales (60-90 days) that is likely attributable to interannual climate variability.</div>
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</fA06>
<fA08 i1="01" i2="1" l="ENG"><s1>Direct evidence of the South Java Current system in Ombai Strait</s1>
</fA08>
<fA09 i1="01" i2="1" l="ENG"><s1>Modeling and Observing the Indonesian Throughflow</s1>
</fA09>
<fA11 i1="01" i2="1"><s1>SPRINTALL (Janet)</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>WIJFFELS (Susan)</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>MOLCARD (Robert)</s1>
</fA11>
<fA11 i1="04" i2="1"><s1>JAYA (Indra)</s1>
</fA11>
<fA12 i1="01" i2="1"><s1>GORDON (Arnold L.)</s1>
<s9>ed.</s9>
</fA12>
<fA12 i1="02" i2="1"><s1>KAMENKOVICH (Vladimir)</s1>
<s9>ed.</s9>
</fA12>
<fA14 i1="01"><s1>Scripps Institution of Oceanography, UCSD, 9500 Gilman Drive</s1>
<s2>La Jolla, CA</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>Center forAustralian Weather and Climate Research, CSIRO Marine and Atmospheric Research</s1>
<s2>Hobart, TAS</s2>
<s3>AUS</s3>
<sZ>2 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>LOCEAN, Université Pierre et Marie Curie</s1>
<s2>Paris</s2>
<s3>FRA</s3>
<sZ>3 aut.</sZ>
</fA14>
<fA14 i1="04"><s1>Department of Marine Sciences and Technology, Bogor Agricultural University</s1>
<s2>Bogor</s2>
<s3>IDN</s3>
<sZ>4 aut.</sZ>
</fA14>
<fA15 i1="01"><s1>Lamont-Doherty Earth Observatory, Columbia University</s1>
<s3>USA</s3>
<sZ>1 aut.</sZ>
</fA15>
<fA15 i1="02"><s1>Department of Marine Science, The University of Southern Mississippi</s1>
<s3>USA</s3>
<sZ>2 aut.</sZ>
</fA15>
<fA20><s1>140-156</s1>
</fA20>
<fA21><s1>2010</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
</fA23>
<fA43 i1="01"><s1>INIST</s1>
<s2>17561</s2>
<s5>354000191685000030</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 2010 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>1 p.1/4</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>10-0455020</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Dynamics of atmospheres and oceans</s0>
</fA64>
<fA66 i1="01"><s0>GBR</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>Direct velocity measurements from 2004 through 2006 confirm the eastward flowing surface South Java Current (SJC) and its deeper Undercurrent (SJUC) crosses the Savu Sea to reach Ombai Strait, a main outflow portal of the Indonesian Throughflow (ITF). The extension of the South Java Current system into Ombai Strait was hinted at by earlier measurement and modeling studies, but the 3-year velocity time series from two moorings in Ombai Strait clearly show separate distinct cores of flow in the SJC and SJUC. The deeper SJUC is driven by Kelvin waves forced by intraseasonal and semi-annual winds in the equatorial Indian Ocean and, when present, is observed across the entire strait. Eastward flow in the surface SJC is near year-round, although it appears that the mechanisms responsible for this flow differ throughout the year. Both the wind-driven Ekman flow during the northwest monsoon and the strongest semi-annual Kelvin waves that have surface signatures can result in eastward surface layer flow across the entire strait. In contrast, during the southeast monsoon the SJC has a subsurface maximum eastward flow at 50-100 m depth in the northern part of Ombai Strait, while the westward ITF is at an annual maximum at the surface in the southern part of the strait. Surface temperature maps suggest the presence of a front during the southeast monsoon that seems to trap the SJC to within ˜10-15 km of the northern boundary of Ombai Strait. The SJC and the frontal location are related to a complex interplay between local wind-driven Ekman dynamics, the strong ITF flow and topography. Significant energy is found at short intraseasonal time scales (20-60 days) in the along-strait flow that is probably related to the short duration westerly wind bursts that drive the Kelvin waves into Ombai Strait. There is a distinct lack of energy at longer intraseasonal time scales (60-90 days) that is likely attributable to interannual climate variability.</s0>
</fC01>
<fC02 i1="01" i2="2"><s0>001E02B05</s0>
</fC02>
<fC02 i1="02" i2="2"><s0>001E02D10</s0>
</fC02>
<fC03 i1="01" i2="X" l="FRE"><s0>Détroit</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="ENG"><s0>Strait</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="SPA"><s0>Estrecho</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="X" l="FRE"><s0>Mesure vitesse</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG"><s0>Speed measurement</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA"><s0>Medida velocidad</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE"><s0>Courant superficiel</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="ENG"><s0>Surface current</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA"><s0>Corriente superficial</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="X" l="FRE"><s0>Sous courant</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG"><s0>Undercurrent</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA"><s0>Hipocorriente</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE"><s0>Modélisation</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG"><s0>Modeling</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA"><s0>Modelización</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE"><s0>Série temporelle</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG"><s0>Time series</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA"><s0>Serie temporal</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE"><s0>Amarrage</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG"><s0>Mooring</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA"><s0>Amarre</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE"><s0>Onde Kelvin</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG"><s0>Kelvin wave</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA"><s0>Onda Kelvin</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Onde forcée</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG"><s0>Forced wave</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Onda forzada</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE"><s0>Vent local</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG"><s0>Local wind</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA"><s0>Viento local</s0>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="X" l="FRE"><s0>Action vent</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="ENG"><s0>Wind effect</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="SPA"><s0>Acción viento</s0>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Mousson</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>monsoons</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Monzón</s0>
<s5>12</s5>
</fC03>
<fC03 i1="13" i2="X" l="FRE"><s0>Couche superficielle</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="X" l="ENG"><s0>Surface layer</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="X" l="SPA"><s0>Capa superficial</s0>
<s5>13</s5>
</fC03>
<fC03 i1="14" i2="X" l="FRE"><s0>Température superficielle</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="ENG"><s0>Surface temperature</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="SPA"><s0>Temperatura superficial</s0>
<s5>14</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Cartographie</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>cartography</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="SPA"><s0>Cartografía</s0>
<s5>15</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Topographie</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>topography</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Topografía</s0>
<s5>16</s5>
</fC03>
<fC03 i1="17" i2="X" l="FRE"><s0>Vent Ouest</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="X" l="ENG"><s0>Westerly wind</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="X" l="SPA"><s0>Viento oeste</s0>
<s5>17</s5>
</fC03>
<fC03 i1="18" i2="X" l="FRE"><s0>Rafale</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="X" l="ENG"><s0>Gust</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="X" l="SPA"><s0>Ráfaga</s0>
<s5>18</s5>
</fC03>
<fC03 i1="19" i2="X" l="FRE"><s0>Variation interannuelle</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="X" l="ENG"><s0>Interannual variation</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="X" l="SPA"><s0>Variación interanual</s0>
<s5>19</s5>
</fC03>
<fC03 i1="20" i2="2" l="FRE"><s0>Variabilité climatique</s0>
<s5>20</s5>
</fC03>
<fC03 i1="20" i2="2" l="ENG"><s0>climate variability</s0>
<s5>20</s5>
</fC03>
<fC03 i1="21" i2="2" l="FRE"><s0>Java</s0>
<s2>NG</s2>
<s5>21</s5>
</fC03>
<fC03 i1="21" i2="2" l="ENG"><s0>Java</s0>
<s2>NG</s2>
<s5>21</s5>
</fC03>
<fC03 i1="21" i2="2" l="SPA"><s0>Java</s0>
<s2>NG</s2>
<s5>21</s5>
</fC03>
<fC03 i1="22" i2="X" l="FRE"><s0>Mer de Savu</s0>
<s2>NG</s2>
<s5>22</s5>
</fC03>
<fC03 i1="22" i2="X" l="ENG"><s0>Savu Sea</s0>
<s2>NG</s2>
<s5>22</s5>
</fC03>
<fC03 i1="22" i2="X" l="SPA"><s0>Mar de Savu</s0>
<s2>NG</s2>
<s5>22</s5>
</fC03>
<fC03 i1="23" i2="2" l="FRE"><s0>Océan Indien</s0>
<s2>564</s2>
<s5>23</s5>
</fC03>
<fC03 i1="23" i2="2" l="ENG"><s0>Indian Ocean</s0>
<s2>564</s2>
<s5>23</s5>
</fC03>
<fC03 i1="23" i2="2" l="SPA"><s0>Océano Indico</s0>
<s2>564</s2>
<s5>23</s5>
</fC03>
<fC03 i1="24" i2="2" l="FRE"><s0>Mers d'Indonésie</s0>
<s2>NG</s2>
<s5>41</s5>
</fC03>
<fC03 i1="24" i2="2" l="ENG"><s0>Indonesian Seas</s0>
<s2>NG</s2>
<s5>41</s5>
</fC03>
<fC03 i1="24" i2="2" l="SPA"><s0>Mares de Indonesia</s0>
<s2>NG</s2>
<s5>41</s5>
</fC03>
<fC03 i1="25" i2="2" l="FRE"><s0>Courant marin</s0>
<s5>42</s5>
</fC03>
<fC03 i1="25" i2="2" l="ENG"><s0>ocean currents</s0>
<s5>42</s5>
</fC03>
<fC03 i1="25" i2="2" l="SPA"><s0>Corriente marina</s0>
<s5>42</s5>
</fC03>
<fC03 i1="26" i2="X" l="FRE"><s0>Climatologie dynamique</s0>
<s5>43</s5>
</fC03>
<fC03 i1="26" i2="X" l="ENG"><s0>Dynamical climatology</s0>
<s5>43</s5>
</fC03>
<fC03 i1="26" i2="X" l="SPA"><s0>Climatología dinámica</s0>
<s5>43</s5>
</fC03>
<fC03 i1="27" i2="2" l="FRE"><s0>ITF</s0>
<s4>CD</s4>
<s5>96</s5>
</fC03>
<fC03 i1="27" i2="2" l="ENG"><s0>Indonesian throughflow</s0>
<s4>CD</s4>
<s5>96</s5>
</fC03>
<fC03 i1="27" i2="2" l="SPA"><s0>ITF</s0>
<s4>CD</s4>
<s5>96</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Indonésie</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Indonesia</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Indonesia</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE"><s0>Extrême Orient</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG"><s0>Far East</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="SPA"><s0>Extremo Oriente</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="03" i2="2" l="FRE"><s0>Asie</s0>
<s2>564</s2>
</fC07>
<fC07 i1="03" i2="2" l="ENG"><s0>Asia</s0>
<s2>564</s2>
</fC07>
<fC07 i1="03" i2="2" l="SPA"><s0>Asia</s0>
<s2>564</s2>
</fC07>
<fC07 i1="04" i2="X" l="FRE"><s0>Mers d'Indonésie</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="04" i2="X" l="ENG"><s0>Indonesian Seas</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="04" i2="X" l="SPA"><s0>Mares de Indonesia</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="05" i2="2" l="FRE"><s0>Océan Pacifique Ouest</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="05" i2="2" l="ENG"><s0>West Pacific</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="06" i2="2" l="FRE"><s0>Océan Pacifique</s0>
<s2>564</s2>
</fC07>
<fC07 i1="06" i2="2" l="ENG"><s0>Pacific Ocean</s0>
<s2>564</s2>
</fC07>
<fC07 i1="06" i2="2" l="SPA"><s0>Océano Pacífico</s0>
<s2>564</s2>
</fC07>
<fN21><s1>298</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
</inist>
</record>

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	Serveur d'exploration sur les relations entre la France et l'Australie
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Serveur d'exploration sur les relations entre la France et l'Australie

Direct evidence of the South Java Current system in Ombai Strait

Direct evidence of the South Java Current system in Ombai Strait

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