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| 1 | 夏季对马暖流区黑潮水与陆架水的相互作用──兼论对马暖流的起源显示文摘根据1994年8月28日至9月7日韩国“Onnuri”号海洋调查船获得的CTD资料及在调查期间投放的11个卫星跟踪漂流浮标资料,分析研究了东海东北部黑潮水的分离及其与陆架水的相互作用,进而探讨了夏季的对马暖流的形成过程。 | 郭炳火 李兴宰 李载学. Korea Ocean research & Development Institute Ansan Korea) Abstract--The separation of the Kuroshio water in the northeaster | 1998 | 海洋学报1998，20，5： | 19 |
| 2 | On the Huanghai (Yellow) Sea circulation:a review by current measurements显示文摘The Huanghai (Yellow) Sea circulations suggested in the past were constructed mostly based on hydrographic data or simple numerical models, and were not rigorously compered with direct current measurements. Ourpresent understanding of the Huanghai Sea circulation is still very poor and superficial. To evaluate our present knowledge about the circulation and to sketch a more realistic circulation pattern, the previous studies on the circulation arebriefly reviewed and directly measured current data collected in the past are revisited. The Huanghai Sea Warm Current and the northeastward extension in summer of the Changjiang diluted water are paid more attention to, which arethe major currents of the basic circulation, and then attempted to sketch the Huanghai Sea circulation by synthesizinghydrography and current data. The Huanghai Sea circulation is not considered to be persistent since the thin water column, less than 100 m, responds quickly and sensitively to external driving forces. Directly measured current data showthat saline water originating from the Kuroshio water turns clockwise around Cheju-do throughout the year and eventually joins the Tsushima Warm Current at the western channel of the Korea Strait. This clockwise current is called theCheju Warm Current. The current data do not support the persistent existence of the Huanghai Sea Warm Current,which has ho believed to supply heat and salt to the Huanghai Sea throughout the year. However, a northward flowis generated intermittently during the weakening phase of cold air outbreaks in winter. The northeast extension of theChangjiang diluted water in summer is evidenced by satellite-tracked surface drifters. | Heung-Jae Lie(Physical Oceanography Dvision, Korea Ocean Research and Development Institute, P.O. Box 29, Ansan, 425 - 600Seoul, Korea) | 1999 | Acta Oceanologica Sinica1999，18，3： | 15 |
| 3 | Annealing behavior of 5083 Al alloy deformed at cryogenic temperature 显示文摘 | Ansan Kyunggi-Do | 2005 | Korea Journal of Materials Science2005，40，： | 1 |
| 4 | Influence of heterocyclic anils on corrosion inhibition and hydrogen permeation through mild steel in acid chloride environments显示文摘 | Quraishi M A Ahmad A Ansan M Q | 1997 | Corrosion Science1997，40，6： | 1 |
| 5 | Seasonal circulation in the southeastern Huanghai Sea显示文摘The seasonal circulation in the southeastern Huanghai Sea has been studied with hydrographic data,which were observed in February and June 1994 and bimonthly during 1970 - 1990, and numerical model results.Horizontal distributions of tempersture and salinity in 1994 are quite different due to strong tidal mixing so that weneed a analysis to see the real distributions of water masses. The mixing ratio analysis with the data of 1970 - 1990shows the connection of the waters in the west coasts of Korea Peninsula with warm and saline waters from the southin summer, which means northward inflows along the west coasts of Korea Peninsula in summer. With this flow, theseasonal circulations, which are deduced from the seasonal change of water mass distributions in the lower layer, arewarm inflows in winter and cold outflows in summer in the central Huanghai Sea, and cold outflows in winter andwarm inflows in summer along the west coasts of Korea Peninsula. The seasonall changed inflows might be theHuanghai Sea Warm Current. The monsoon winds can drive such circulations. However, summer monsoon winds areweak and irregular. As one of other possible dynamics, the variation of Kuroshio transport is numerically studied withallowing sea level fluctuations. Although it should be studied more, it possibly drives the summer circulations. The realcirculations seem to be driven by both of them. | Ig-Chan Pang(Department of Oceanography, Cheju National University, Cheju-do 690 - 756, Korea)Hong-Kil Rho(Deppartment of Fishery, Cheju National University, Cheju-do 690 - 756, Korea)Jae-Hak Lee (Korea Ocean Research and Development Institute, Ansan, P. | 1999 | Acta Oceanologica Sinica1999，18，3： | 1 |
| 6 | On the origin of the Tsushima Warm Current Water显示文摘OntheoriginoftheTsushimaWarmCurrentWater￥TangYuxiangandHeung-JaeLie(FirstinstituteOfOceanography,StateOceanicAdministration,Q... | Tang Yuxiang and Heung-Jae Lie (First institute Of Oceanography, State Oceanic Administration, Qingdao 266003, China2. Korea Ocean Research & Development Institute, Ansan, Korea) | 1996 | Acta Oceanologica Sinica1996，15，2： | 1 |
| 7 | Optic fiber-based dynamic pressure sinsor for WIM system显示文摘 | Yuan S Ansan F Liu X | 2005 | Sensors and Actuators A Physical2005，120，1： | 1 |
| 8 | New observations of Warrego Valles, Mars : evidence for precipitation and surface runoff 显示文摘 | Ansan V Mangold N | 2006 | Planetary and Space Science2006，54，： | 1 |
| 9 | Biochemical and morphological changes in herniated human intervertebral disc显示文摘 | Ansan R Tajima N Chosa E | 2001 | Orthop Sci2001，6，6： | 1 |
| 10 | New observations of Warrego Valleys, Mars : evidence for precipitation and surface runoff显示文摘 | Ansan V Mangold N | 2006 | Planetary and Space Science2006，，54： | 1 |
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