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DOI10.1029/2020JC016608
Observed Water Exchange Between the South China Sea and Java Sea Through Karimata Strait
Xu T.F.; Wei Z.X.; Susanto R.D.; Li S.J.; Wang Y.G.; Wang Y.; Xu X.Q.; Agustiadi T.; Trenggono M.; Sulistyo B.; Setiawan A.; Kuswardani A.; Fang G.H.
发表日期2021
ISSN21699275
卷号126期号:2
英文摘要Volume, heat and freshwater transports from the South China Sea (SCS) to the Java Sea through the Karimata Strait are estimated based on direct measurements of current, temperature, salinity, and satellite observations. Subject to strong seasonal variability, the volume, heat, freshwater transports are −1.98 ± 0.23 Sv (1 Sv = 106 m3/s), −209.68 ± 15.19 TW (1 TW = 1012 W), −99.87 ± 15.11 mSv (1 mSv = 10-3 Sv) in boreal winter, and 0.47 ± 0.20 Sv, 61.06 ± 15.46 TW, 31.67 ± 8.76 mSv in boreal summer, respectively (negative transport defined from SCS to Java Sea). The annual mean volume, heat and freshwater transports are −0.78 ± 0.12 Sv, −77.31 ± 4.99 TW, and −30.87 ± 6.15 mSv, respectively. The freshwater transport through Karimata Strait is as large as 42% of rainfall input to the entire Indonesian seas in boreal winter, thereby modulating the Indonesian Throughflow (ITF) through the “freshwater plug” effect in the Makassar Strait. The interannual variability of the transports is not significantly correlated to the Indian Ocean Dipole and El Niño-Southern Oscillation. There is a significant decreasing trend of volume and heat transports from the SCS to Java Sea over the period of 1997–2015, with a reduction of 0.26 Sv and 15 TW, respectively. The freshwater transport decreases 12.29 mSv by 2016 compared with that in 2009, equivalent to 33.2%–49.72% of the annual mean freshwater transport during 2009–2016. This decreasing trend would play contradictory roles in the decadal trend of ITF transport by building a “freshwater plug” in the southern Makassar Strait and a ‘buoyant plume’ in the Indo-Australian Basin, respectively. © 2021. American Geophysical Union. All Rights Reserved.
英文关键词Indonesian seas | Indonesian Throughflow | Karimata Strait | South China Sea Throughflow | water transport
语种英语
来源期刊Journal of Geophysical Research: Oceans
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/186491
作者单位First Institute of Oceanography, Ministry of Natural Resources of China, Qingdao, China; Laboratory for Regional Oceanography and Numerical Modeling, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao, China; Key Laboratory of Marine Science and Numerical Modeling, Ministry of Natural Resources, Qingdao, China; Department of Atmospheric and Oceanic Science, University of Maryland, College Park, MD, United States; Faculty of Earth Sciences and Technology, Bandung Institute of Technology, Bandung, Indonesia; South China Sea Marine Survey and Technology Center, State Oceanic Administration, Guangzhou, China; Agency for Marine and Fisheries Research and Human Resources, Ministry of Marine Affairs and Fisheries, Jakarta, Indonesia; Department of Marine Science, Faculty of Fisheries and Marine Science, Jenderal Soedirman University, Purwokerto, Indonesia; Ministry of Marine Affairs and Fisheries, Jakarta, Indonesia
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Xu T.F.,Wei Z.X.,Susanto R.D.,et al. Observed Water Exchange Between the South China Sea and Java Sea Through Karimata Strait[J],2021,126(2).
APA Xu T.F..,Wei Z.X..,Susanto R.D..,Li S.J..,Wang Y.G..,...&Fang G.H..(2021).Observed Water Exchange Between the South China Sea and Java Sea Through Karimata Strait.Journal of Geophysical Research: Oceans,126(2).
MLA Xu T.F.,et al."Observed Water Exchange Between the South China Sea and Java Sea Through Karimata Strait".Journal of Geophysical Research: Oceans 126.2(2021).
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