|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | Study on interaction between the coastal water, shelf water and Kuroshio water in the Huanghai Sea and East China Sea显示文摘The main processes of interaction between the coastal water, shelf water and Kuroshiowater in the Huanghai Sea (HS) and East China Sea (ECS) are analyzed based on the observation andstudy results in recent years. These processes include the intrusion of the Kuroshio water into the shelfarea of the ECS, the entrainment of the shelf water into the Kuroshio, the seasonal process in the south-em shelf area of the ECS controlled alternatively by the Taiwan Strait water and the Kuroshio water in-truding into the shelf area, the interaction between the Kuroshio branch water, shelf mixed water andmodified coastal water in the northeastern ECS, the water-exchange between the HS and ECS and thespread of the Changjiang diluted water. | Binghuo Guo, Xiaomin Hu, Xuejun Xiong, Renfeng Ge First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China | 2003 | Acta Oceanologica Sinica2003，22，3： | 15 |
| 2 | Role of Kuroshio frontal eddy in exchange between shelf water and Kuroshio water in East China Sea显示文摘Basic patterns of the reversal of the Kuroshio water toward the shelf, intrusion of the shelf mixed waterinto the Kuroshio and uplifting of the near-bottom nutrient-rich water into the upper layer by the pumping of the frontal eddy are analyzed on the basis of satellite infrared images and hydrologic, chemical and biological observations. Results show that the Kuroshio frontal eddies play a very important role in the exchange between the shelf water and the Kuroshio water. The estimation of the average volume transports for three frontal eddy events indicates that the shelf mixed water entrained by an eddy into Kuroshio is 0.44×10~6 m3/s and the reversal Kuroshio water onto the shelf region only 0.04×10~6 m3/s. Along the whole shelf edge, the volume transport of the shelf mixed water entrained by the eddies into the Kuroshio is 1.8×10~6 m3/s. The nutrient (NO3-N) flux pumped to the euphotic zone and input to the continental shelf through a column with 1 m wide is 974 μmol/(s·m) when there is frontal eddy and only 79 μmol/(s·m) in the case of no frontal eddy. Yearly nutrient (NO3-N) flux input to the shelf area caused by the frontal eddy is 1.7×10~5 t/a. | Guo Binghuo and Ge Renfeng First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China | 1997 | Acta Oceanologica Sinica1997，16，1： | 9 |
| 3 | Marine hydrographic spatial-variability and its cause at the northern margin of the Amery Ice Shelf显示文摘Conductivity,temperature and depth(CTD) data collected along a zonal hydrographic section from the northern margin of the Amery Ice Shelf on 25-27 February 2008 by the 24th Chinese National Antarctic Research Expedition (CHINARE) cruise in the 2007/2008 austral summer are analyzed to study thermohaline structures.Analysis reveals warm subsurface water in a limited area around the east end of the northern margin,where the temperature,salinity and density have east-west gradients in the surface layer of the hydrographic section.The localization of the warm subsurface water and the causes of the CTD gradients in the surface layer are discussed.In addition,the results from these CTD data analyses are compared with those from the 22nd CHINARE cruise in the 2005/2006 austral summer.This comparison revealed that the thermoclines and haloclines had deepened and their strengths weakened in the 2007/2008 austral summer.The difference between the two data sets and the cause for it can be reasonably explained and attributed to the change in ocean-ice-atmosphere interactions at the northern margin of the Amery Ice Shelf. | GE RenFeng DONG ZhaoQian CHEN HongXia LIU Na SHI JiuXing PU ShuZhen | 2011 | Advances in Polar Science2011，22，2： | 3 |
| 4 | Analysis of the high and low temperature centers and their relation with circulations in the East China Sea显示文摘Three warm currents,the Kuroshio,its shelf intrusion branch in the northeast of Taiwan and the Taiwan Warm Current(hereafter TWC),dominate the circulation pattern in the East China Sea (hereafter ECS).Their origination,routes and variation in winter and summer are studied.Their relationship with four major high and low temperature centers is analyzed.Differing from the previous opinion,we suggest that the four major centers are generated to a great extent by the interaction of the currents in the ECS.In summer,a cold water belt in the northeast of Taiwan is preserved from winter between the Kuroshio and the TWC.The shelf intrusion branch of the Kuroshio separates the water belt,and two low temperature centers generate in the northeast of Taiwan.In the southern ECS,the TWC transports more heat flux northward to form a warm pool.But it is separated in the lower layer by the cold water driven by the intrusion branch of the Kuroshio.So the TWC and the intrusion branch of the Kuroshio play a dominating role to generate the high temperature center.The interaction among the eastward TWC,the northward Tsushima Warm Current(hereafter TSWC)and the southward Su Bei Coastal Flow(hereafter SBCF)generates the low temperature center in the northern ECS.In winter,the strengthening of the shelf intrusion branch of the Kuroshio obscures the two low temperature centers in the northeast of Taiwan.For the weakening of the TWC,the high temperature center in the southern ECS vanishes,and the low temperature center in the northern ECS shifts to south. | YANG Yongzeng QIAO Fangli XIA Changshui GE Renfeng | 2009 | Acta Oceanologica Sinica2009，28，2： | 0 |
您所在的机构暂未开通此部分的功能，请联系管理员