2018
DOI: 10.1088/1742-6596/979/1/012049
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Upwelling Dynamic Based on Satellite and INDESO Data in the Flores Sea

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Cited by 4 publications
(5 citation statements)
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“…Among them, the Flores Sea, where core SO217‐18540 was recovered, is one of the most biologically productive areas at low latitudes due to the seasonal occurrence of upwelling. Thus, vertical mixing plays a dominant role in controlling the interannual variability in the upper water column in this region (Gordon, 2005; Kurniawan et al., 2018) (Figure 1). The Flores upwelling and the better‐known Java‐Sumatra upwelling are driven by the Australian‐Indonesian winter monsoon (AIWM), which is part of the larger‐scale Austral‐Asian monsoon system.…”
Section: Regional Hydrological Backgroundmentioning
confidence: 99%
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“…Among them, the Flores Sea, where core SO217‐18540 was recovered, is one of the most biologically productive areas at low latitudes due to the seasonal occurrence of upwelling. Thus, vertical mixing plays a dominant role in controlling the interannual variability in the upper water column in this region (Gordon, 2005; Kurniawan et al., 2018) (Figure 1). The Flores upwelling and the better‐known Java‐Sumatra upwelling are driven by the Australian‐Indonesian winter monsoon (AIWM), which is part of the larger‐scale Austral‐Asian monsoon system.…”
Section: Regional Hydrological Backgroundmentioning
confidence: 99%
“…The Flores upwelling and the better‐known Java‐Sumatra upwelling are driven by the Australian‐Indonesian winter monsoon (AIWM), which is part of the larger‐scale Austral‐Asian monsoon system. During austral winter (June–September), southeast winds drive the surface water of the Flores Sea away from the coast, initiating the Flores upwelling and subsequently reducing both SST (27.6°C) and TT (22.9°C) and enhancing the ΔΤ (4.7°C) (Figure 2) (Gordon, 2005; Kurniawan et al., 2018). In contrast, the Flores upwelling ceases during austral summer (December‐March) due to the advection of surface water driven by northwest winds toward the coastal region, which results in increased SST (28.2°C) and TT (23.9°C) and decreased ΔΤ (4.3°C) (Figure 2) (Gordon, 2005; Kurniawan et al., 2018).…”
Section: Regional Hydrological Backgroundmentioning
confidence: 99%
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“…In addition, north of Labuan Bajo is the trajectory for transferring large water masses from the Pacific Ocean to the Indian Ocean, commonly referred to as the Indonesian Through Flow (ITF). According to Kurniawan, the temperature in the northern waters of Labuan Bajo is dominated by warm waters that occur in the western season, transition one, and transition two [7]. Meanwhile, the temperature of cold waters occurs in the east monsoon, where the wind blows over the sea surface faster than usual.…”
Section: Regional Seafloor and Oceanographic Settingmentioning
confidence: 99%