一种估算陆架上升流流速的新方法     

庞重光  胡敦欣  白学志  雷坤 《海洋科学》2002,26(8):67-71

依据海水中悬浮物垂直通量的计算公式 ,提出了一种利用悬浮物含量、垂直通量和静水沉速估算海水垂向流速的新方法。当悬浮物静水沉速未知时 ,可用判别方法对海水是否存在显著垂向流动做基本判断。同时采用估算及判别方法对东海9404航次两连续站111和410的实测资料进行分析 ,得出了410站的海水不存在显著的上升流动 ,而111站的海水不仅存在上升流动 ,流速约为2.6×10 3cm/s ,而且在时均情况下 ,上升流不能达到表层的结果。此判断结果与以往的观测和结论以及本次观测结果相吻合。  相似文献   

Interannual variability of transport and bifurcation of the North Equatorial Current in the tropical North Pacific Ocean   总被引：1，自引：0，他引：1  

翟方国  胡敦欣 《中国海洋湖沼学报》2012,30(1):177-185

The relationship of the interannual variability of the transport and bifurcation latitude of the North Equatorial Current (NEC) to the El Ni o-Southern Oscillation (ENSO) is investigated. This is done through composite analysis of sea surface height (SSH) observed by satellite altimeter during October 1992-July 2009, and correspondingly derived sea surface geostrophic currents. During El Nio/La Ni a years, the SSH in the tropical North Pacific Ocean falls/rises, with maximum changes in the region 0-15°N, 130°E-160°E. The decrease/increase in SSH induces a cyclonic/anticyclonic anomaly in the western tropical gyre. The cyclonic/anticyclonic anomaly in the gyre results in an increase/decrease of NEC transport, and a northward/southward shift of the NEC bifurcation latitude near the Philippine coast. The variations are mainly in response to anomalous wind forcing in the west-central tropical North Pacific Ocean, related to ENSO events.  相似文献   

ON LONG-WAVE BREAKING Ⅰ.CONSIDERING nTH POWER BOTTOM FRICTION     

田纪伟  娄顺里  胡敦欣  李鸿雁  张法高 《中国海洋湖沼学报》1995,(2)

Longwave breaking is the agent for many important upper ocean layer processes including the trans-fer of horizontal momentum. In a previous study on the process of longwave breaking, only linear bot-tom friction was considered.In this paper, we discuss the longwave breaking phenomena in the moregeneral case of nth power bottom friction. Using the theory of blowup of solution,the criterion for thetime and location of the longwave breaking can be obtained.  相似文献   

OUTFLOW OF SUSPENDED MATERIALS FROM THE CHANGJIANG RIVER MOUTH     

彭马川  胡敦欣 《中国海洋湖沼学报》1997,15(3):258-263

ImODUrmNJ0GFS(JointGlobaldrinFLuxStudy:l99()-2OO()isaworldwidenawhprogramfocusingontheoasns'buharolewhentheC0,prmtageintheairincreasesandtheatmOspheretemPeraturebo.ThefluxofsuspendedrnateriaIs(SM)intheEastChinaScaisboortanttotheworld'srnatterchaltfon,astheChangiiangRiver,thelargestriverinAsia,dischargesbillionsoftOnsoftheidWhterintoit.ManystudAshavebocondtalonSMmovementncarChina'scoastalseas.Yang(l983)studiedthefine%rainedsededtSfromtheChangiiangandHuangheRiversWhileQin(l983)fo…  相似文献   

VARIABILITY OF THERMOHALINE STRUCTURE AT 4°S,156°E DURING TOGA COARE IOP     

冯明  胡敦欣 《中国海洋湖沼学报》1995,(1)

The thermohaline structure at 4 °S, 156 °E was analyzed based on CTD data acquired during theTOGA COARE Intensive Observing Period(IOP) from November,1992 to February,1993. The ocean re-sponses during two Madden-Julian Oscillation(MJO)events were preliminarily studied based onmeteorological field observation.The main water masses at the observation point were Tropical SurfaceWater, Southern Subtropical Lower Water and Southern Intermediate Water from surface downward. Therewas good correlation of sea surface temperature with the wind field,and of the surface salinity with windspeed and rainfalls. Both of the two surface variables were also modulated by upwelling caused by west-erly winds at the observation point. The isohaline layer was not always shallower than the isothermal lay-er in this observation and could be considered as the lower limit of the diurnal variation of theisothermal layers in most cases. The existence of large variations of the maximum salinity core is sug-gested to be related to t  相似文献   

EMPIRICAL ORTHOGONAL MODES IN THE WESTERN PACIFIC     

崔茂常  胡敦欣 《中国海洋湖沼学报》1990,(4)

The method of empirical orthogonal modes has been widely used since the 1970's in physical oceanography to study and rebuild vertical structures of ocean dynamic factors. Because of the dominance of the low modes, the dynamic profile data can be largely reduced.Up to now, all expressions of empirical orthogonal modes are numerical. In this study, an analytic expression for empirical orthogonal ocean modes is constructed for convenient use whereby any numerical expressions can be repeated.The features of the normal modes decomposed from the buoyance frequency profiles obtained in October of 1986,1987 and 1988 by the R/V Science 1 in the western Pacific are quantitatively examined in this study.  相似文献