Direct evidence of the South Java Current system in Ombai Strait
Identifieur interne : 003C68 ( PascalFrancis/Curation ); précédent : 003C67; suivant : 003C69Direct 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.
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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<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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<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>
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</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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