Freshening of the intermediate water of the South China Sea between the 1960s and the 1980s     

刘长建  王东晓  陈举  杜岩  谢强 《中国海洋湖沼学报》2012,30(6):1010-1015

Variation in intermediate water salinity in the South China Sea (SCS) between the 1960s and 1980s was studied using historical hydrographic data. The results demonstrate that the water was significantly fresher in the 1980s than in the 1960s, indicating that vertical mixing at intermediate water depth was reduced in the 1980s. This was partially because of the change of the SCS meridional overturning circulation (MOC) connecting local intermediate water with deep water. Data assimilation showed a 0.5Sv (1 Sv=10 6m 3/s) reduction in the strength of the MOC, which is about one third of the mean SCS MOC. Because the SCS MOC is linked to the Pacific Ocean, such an interdecadal variation in the intermediate water SCS may reflect anthropogenic climate change in the world ocean.  相似文献   

The South China Sea throughflow: linkage with local monsoon system and impact on upper thermal structure of the ocean   总被引：1，自引：0，他引：1  

刘钦燕  王东晓  谢强 《中国海洋湖沼学报》2012,30(6):1001-1009

The tendency of South China Sea throughflow (SCSTF) variation associated with the local monsoon system, and its impact on upper-layer thermal structure, are studied using the Simple Ocean Data Assimilation (SODA) dataset, combined with Ishii reanalysis data. Luzon Strait Transport (LST) is measured and used as an index for studying the SCSTF variation. Results show that LST had an increasing tendency over the last 50 years, mainly in summer and fall. The increasing tendency was 0.017 1 Sv/a in summer and 0.027 4 Sv/a in fall, as estimated by SODA, and 0.018 0Sv/a in summer and 0.018 9 Sv/a in fall, as estimated by "Island Rule" theory. LST increased by 0.53Sv in JJA (June-July-August) and 0.98Sv in SON (September-October-November) after climate shift, as inferred by SODA data. The average LST anomaly in JJA and SON is strongly related to the local monsoon system, especially to variability of the meridional wind stress anomaly after application of a 3-year running mean, with correlation coefficients 0.57 and 0.51, respectively. In addition to the basin-scale wind forcing, the local northeasterly wind stress anomaly in the SCS can push Pacific water entering the SCS more readily in JJA and SON after climate shift, and an SCSTF-associated cooling effect may favor subsurface cooling more frequently after climate shift.  相似文献   

Data assimilation for distributed hydrological catchment modeling via ensemble Kalman filter   总被引：4，自引：0，他引：4  

Xianhong Xie  Dongxiao Zhang 《Advances in water resources》2010

Catchment scale hydrological models are critical decision support tools for water resources management and environment remediation. However, the reliability of hydrological models is inevitably affected by limited measurements and imperfect models. Data assimilation techniques combine complementary information from measurements and models to enhance the model reliability and reduce predictive uncertainties. As a sequential data assimilation technique, the ensemble Kalman filter (EnKF) has been extensively studied in the earth sciences for assimilating in-situ measurements and remote sensing data. Although the EnKF has been demonstrated in land surface data assimilations, there are no systematic studies to investigate its performance in distributed modeling with high dimensional states and parameters. In this paper, we present an assessment on the EnKF with state augmentation for combined state-parameter estimation on the basis of a physical-based hydrological model, Soil and Water Assessment Tool (SWAT). Through synthetic simulation experiments, the capability of the EnKF is demonstrated by assimilating the runoff and other measurements, and its sensitivities are analyzed with respect to the error specification, the initial realization and the ensemble size. It is found that the EnKF provides an efficient approach for obtaining a set of acceptable model parameters and satisfactory runoff, soil water content and evapotranspiration estimations. The EnKF performance could be improved after augmenting with other complementary data, such as soil water content and evapotranspiration from remote sensing retrieval. Sensitivity studies demonstrate the importance of consistent error specification and the potential with small ensemble size in the data assimilation system.  相似文献   

北极涛动与北大西洋涛动的差异          下载免费PDF全文

杨小怡  王东晓 《气候变化研究进展》2006,2(2):82-84

根据北极涛动和北大西洋涛动指数的时间序列,选取两者差异较大的13个年份进行合成分析。结果表明：除北太平洋地区外,北极涛动与北大西洋涛动差异最显著的区域是西欧-地中海区域和亚洲东北部地区。北极涛动高指数阶段,对流层中层为纬向二波的驻波型,分别对应于极地-欧亚遥相关型和太平洋-北美遥相关型。同时,纬向平均纬向风偶极型使西风急流向极地偏移,与增强的中纬度经圈环流相互作用,引导对流层上层异常信号向下传播,形成高低空耦合机制。进一步分析发现,这种中纬度经圈环流异常和高低空耦合形势的差异主要表现在欧亚大陆地区;在北大西洋区域差异并不显著。  相似文献   

道路曲线放样方法的实验     

卢松耀  王东晓  王德征 《地理空间信息》2010,8(6):136-138,141

对曲线放样的常见方法进行了比较分析,提出了改进方法,结合实例对自由设站极坐标法、DGPS-RTK法曲线测设方法进行了深入讨论,给出了相应的数据处理方法和实验方法,实验结果表明DGPS-RTK技术使曲线放样精度更高,实现更便捷。  相似文献   

Influence of the upper mixed layer depth on Langmuir turbulence characteristics     

Li  Guojing  Dong  Changming  Pan  Jiayi  Devlin  Adam T.  Wang  Dongxiao 《中国海洋湖沼学报》2023,41(1):17-37

Journal of Oceanology and Limnology - The upper mixed layer depth (h) has a significant seasonal variation in the real ocean and the low-order statistics of Langmuir turbulence are dramatically...  相似文献   

Analysis of interdecadal variation of tropical Pacific thermocline based on assimilated data   总被引：5，自引：3，他引：2  

GU Dejun  WANG Dongxiao  LI Chunhui  WU Lixin 《海洋学报(英文版)》2004,23(1):61-72

1IntroductionAfterNittaandYamada(1989)andTren-berth(1990)haveinitiallydescribedthe1977climaticvariationovertheNorthPacificwithstep-likeshiftofwintermeansealevelpressurefield,thePacificinterdecadaloscillation(PDO)hasextensivelybeenstudied.TheworkaboutthecauseofPDOfromtheviewoftheNorthPacificincludesthermodynamicexplanationoflow-frequencysea-surfacetemperature(SST)affectedbyatmosphericrandomforcing(FrankignoulandHasselmann,1977),themeridionalchangeofthermaltransportbysubtropicalgyreandhen…  相似文献   

On the relationship between convection intensity of South China Sea summer monsoon and air-sea temperature difference in the tropical oceans   总被引：5，自引：4，他引：1  

LIN Ailan  LIANG Jianyin  GU Dejun  WANG Dongxiao 《海洋学报(英文版)》2004,23(2):267-278

The annual, interannual and inter-decadal variability of convection intensity of South China Sea (SCS) summer monsoon and air-sea temperature difference in the tropical ocean is analyzed, and their relationship is discussed using two data sets of 48-a SODA (simple ocean data assimilation) and NCEP/NCAR. Analyses show that in wintertime Indian Ocean (WIO), springtime central tropical Pacific (SCTP) and summertime South China Sea-West Pacific (SSCSWP), air-sea temperature difference is significantly associated with the convection intensity of South China Sea summer monsoon. Correlation of the inter-decadal time scale (above 10 a) is higher and more stable. There is inter-decadal variability of correlation in scales less than 10 a and it is related with the air-sea temperature difference itself for corresponding waters. The inter-decadal variability of the convection intensity during the South China Sea summer monsoon is closely related to the inter-decadal variability of the general circulation of the atmosphere. Since the late period of the 1970s, in the lower troposphere, the cross-equatorial flow from the Southern Hemisphere has intensified. At the upper troposphere layer, the South Asian high and cross-equatorial flow from the Northern Hemisphere has intensified at the same time. Then the monsoon cell has also strengthened and resulted in the reinforcing of the convection of South China Sea summer monsoon.  相似文献   

Advances in research of the mid-deep South China Sea circulation     

Wang  Dongxiao  Wang  Qiang  Cai  Shuqun  Shang  Xiaodong  Peng  Shiqiu  Shu  Yeqiang  Xiao  Jingen  Xie  Xiaohui  Zhang  Zhiwei  Liu  Zhiqiang  Lan  Jian  Chen  Dake  Xue  Huijie  Wang  Guihua  Gan  Jianping  Xie  Xinong  Zhang  Rui  Chen  Hui  Yang  Qingxuan 《中国科学:地球科学(英文版)》2019,62(12):1992-2004

The South China Sea(SCS) is a large marginal sea connecting the Indian and Pacific oceans.Under the factors of monsoons,strait transport,and varied bathymetry,the SCS presents a three-layer structure and strong diapycnal mixing which is far greater than that in the open ocean.Theoretical analysis and observations reveal that internal tides,internal solitary waves,and strong winds are the sources of the strong mixing in the northern SCS.A major consequence of the strong mixing is an active mid-deep circulation system.This system promotes exchange of water between the SCS and adjacent oceans,and also regulates the upper layer of wind-driven circulation,making the 3 dimensional SCS circulation clearly different from that in other tropical and subtropical marginal seas.The mass transport capacity of the mid-deep circulation has a substantial impact on marine sedimentation,the biogeochemical cycle,and other processes in the SCS.This paper summarizes the recent advances in middeep sea circulation dynamics of the SCS,and discusses the opportunities and challenges in this area.  相似文献   

基于高频地波雷达观测的粤西近海潮流潮能分析     

朱怀鑫  俎婷婷  李健  舒业强  陈举  王东晓 《热带海洋学报》2018,37(5):25-32

利用粤西海域高频地波雷达观测得到的表层海流资料进行潮流调和分析。结果表明: 粤西近海主要属于不正规半日分潮, 浅水分潮较强。以M₂分潮为例, 潮流运动形式主要为逆时针的往复流为主, 方向沿西北—东南方向。粤西近海的潮能主要由东部陆架输送进来, 潮能自东向西传播, 在大潮期间, 粤西的潮能出现向岸方向分量, 表现为从东南向西北方向传播, 在近岸区域潮能通量传播的方向会发生一个向岸的偏转。通过潮能收支方程计算潮能耗散, 发现粤西近海潮能耗散的高值区在西部岛屿密集区域, 与琼州海峡的存在和琼州海峡东北处地形变化存在明显的相关关系。  相似文献