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| 1 | Evidence for water exchange between the South China Sea and the Pacific Ocean through the Luzon Strait显示文摘An analysis of historical oxygen data provides evidence on the water exchange between the South China Sea(SCS)and the Pacific Ocean(PO).In the vicinity of the Luzon Strait(LS),the dissolved oxygen concentration of sea water is found to be lower on the Pacific side than on the SCS side at depths between 700 and 1500 rn(intermediate layer),while the situation is reversed above 700 rn(upper layer)and below 1 500 rn(deep layer).The evidence suggests that water exits the SCS in the intermediate layer but enters it from the Pacific in both the upper and the deep layers,supporting the earlier speculation that the Luzon Strait transport has a sandwiched structure in the vertical.Within the SCS basin,the oxygen distribution indicates widespread vertical rnovernent,including the upwelling in the intermediate layer and the downwelling in the deep layer. | Qu Tangdong(曲堂栋) | 2002 | Acta Oceanologica Sinica2002，21，2： | 40 |
| 2 | Advances in research on the deep South China Sea circulation显示文摘Deep sea circulation is important for world climate and has been a substantial research area in ocean science, leading to various breakthroughs and discoveries. With the rapid advance in research on ocean science, these matters have received increasing attention from the oceanography community. In this article, we attempt to convey the progress made in recent years. We first provide an overview of existing observations, theories, and simulations of deep South China Sea circulation. Finally, we discuss remaining issues. | TIAN JiWei QU TangDong | 2012 | Chinese Science Bulletin2012，57，24： | 17 |
| 3 | Review on observational studies of western tropical Pacific Ocean circulation and climate显示文摘The Western Tropical Pacific(WTP) Ocean holds the largest area of warm water(>28℃) in the world ocean referred to as the Western Pacific Warm Pool(WPWP),which modulates the regional and global climate through strong atmospheric convection and its variability.The WTP is unique in terms of its complex 3-D ocean circulation system and intensive multiscale variability,making it crucial in the water and energy cycle of the global ocean.Great advances have been made in understanding the complexity of the WTP ocean circulation and associated climate impact by the international scientific community since the 1960 s through field experiments.In this study,we review the evolving insight to the 3-D structure and multi-scale variability of the ocean circulation in the WTP and their climatic impacts based on in-situ ocean observations in the past decades,with emphasis on the achievements since 2000.The challenges and open que stions remaining are reviewed as well as future plan for international study of the WTP ocean circulation and climate. | HU Dunxin WANG Fan SPRINTALL Janet WU Lixin RISER Stephen CRAVATTE Sophie GORDON Arnold ZHANG Linlin CHEN Dake ZHOU Hui ANDO Kentaro WANG Jianing LEE Jae-Hak HU Shijian WANG Jing ZHANG Dongxiao FENG Junqiao LIU Lingling VILLANOY Cesar KALUWIN Chalapan QU Tangdong MA Yixin | 2020 | Journal of Oceanology and Limnology2020，38，4： | 3 |
| 4 | Multiple satellite missions confirming the theory of seasonal oceanic variability in the northern North Pacific显示文摘 | Song Y T Qu Tangdong | 2011 | Marine Geodesy2011，34，： | 1 |
| 5 | Thermohaline circulation in thedeep South China Sea basin inferred from oxygendistributions显示文摘 | LI LI QU TANGDONG 2006 | 2006 | Journal of Geophysical Research2006，111，5： | 1 |
| 6 | Anintroduction to the South China Sea throughflow: its dynamics,variability, and application for climate显示文摘 | QU TANGDONG SONG Y T YAMAGATA T 2009 | 2009 | Dynamics ofAtmospheres and Oceans2009，47，1： | 1 |
| 7 | Intrusion of the North Pacific waters into the South China Sea显示文摘 | Qu Tangdong Mitsudera H Yamagata T | 2000 | Journal of Geophysical Research2000，105，3： | 1 |
| 8 | Impacts of the South China Sea Throughflow on seasonal and interannual variations of the Indonesian Throughflow显示文摘 | Tomoki Tozuka Tangdong Qu Yukio Masumoto Toshio Yamagata | 2008 | Dynamics of Atmospheres and Oceans2008，，1： | 1 |
| 9 | An introduction to the South China Sea throughflow: Its dynamics, variability, and application for climate显示文摘 | Tangdong Qu Y. Tony Song Toshio Yamagata | 2008 | Dynamics of Atmospheres and Oceans2008，，1： | 1 |
| 10 | Intrusion of the North Pacific waters into the South China Sea显示文摘 | QU TANGDONG MITISUDERA H YAMAGATA T | 2000 | Journal of Geophysical Research2000，105，3： | 1 |
| 11 | Can Luzon Strait transport play a role in conveying the impact of ENSO to the South China? 显示文摘 | QU TANGDONG Kim Y Y YAREMCHUK M | 2004 | Journal of Climate2004，17，： | 1 |
| 12 | Upper-layer circulation in the South Chi-na Sea显示文摘 | QU TANGDONG | 2000 | J Phys Oceanogr2000，30，14： | 1 |
| 13 | On the western boundary currents in the Philippine Sea显示文摘 | Qu Tangdong Mitsuder H Yamagata T | 1998 | J Geophys Res-Oceans1998，103，： | 1 |
| 14 | The bifurcation of the north equatorial current in the Pacific 显示文摘 | Qu Tangdong Roger Lukas | 2003 | Journal of Physical Oceanorgaphy2003，33，： | 1 |
| 15 | A North Pacific decadal variability in subduction rate显示文摘 | Qu Tangdong Chen Ju | 2009 | Geophysical Research Letters2009，36，22： | 1 |
| 16 | What governs the North Atlantic salinity maximum in a global GCM?显示文摘 | Qu Tangdong Gao Shan Fukumori I | 2011 | Geophysical Research Letters2011，38，07： | 1 |
| 17 | Upper-layer circulation in the South China Sea显示文摘 | Qu Tangdong | 2000 | Journal of Physical Oceanography2000，30，： | 1 |
| 18 | A fresh look at the deepwater overflow in the Luzon Strait显示文摘On the basis of the latest version of a U.S. Navy generalized digital environment model(GDEM-V3.0) and World Ocean Atlas(WOA13), the hydraulic theory is revisited and applied to the Luzon Strait, providing a fresh look at the deepwater overflow there. The result reveals that:(1) the persistent density difference between two sides of the Luzon Strait sustains an all year round deepwater overflow from the western Pacific to the South China Sea(SCS);(2) the seasonal variability of the deepwater overflow is influenced not only by changes in the density difference between two sides of the Luzon Strait, but also by changes in its upstream layer thickness;(3) the deepwater overflow in the Luzon Strait shows a weak semiannual variability;(4) the seasonal mean circulation pattern in the SCS deep basin does not synchronously respond to the seasonality of the deepwater overflow in the Luzon Strait.Moreover, the deepwater overflow reaches its seasonal maximum in December(based on GDEM-V3.0) or in fall(October–December, based on the WOA13), accompanied by the lowest temperature of the year on the Pacific side of the Luzon Strait. The seasonal variability of the deepwater overflow is consistent with the existing longest(3.5 a) continuous observation along the major deepwater passage of the Luzon Strait. | ZHU Yaohua SUN Junchuan WEI Zexun WANG Yonggang FANG Guohong QU Tangdong | 2017 | Acta Oceanologica Sinica2017，36，5： | 0 |
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