A truncated Gaussian filter for data assimilation with inequality constraints: Application to the hydrostatic stability condition in ocean models - ScienceDirect
Export JavaScript is disabled on your browser. Please enable JavaScript to use all the features on this page., 2009, Pages 1-17Author links open overlay panelShow moreAbstractIn many data assimilation problems, the state variables are subjected to inequality constraints. These constraints often contain valuable information that must be taken into account in the estimation process. However, with linear estimation methods (like the Kalman filter), there is no way to incorporate optimally that kind of additional information. In this study, it is shown that an optimal filter dealing with inequality constraints can be formulated under the assumption that the probability distributions are truncated Gaussian distributions. The statistical tools needed to implement this truncated Gaussian filter are described. It is also shown how the filter can be adapted to work in a reduced dimension space, and how it can be simplified following several additional hypotheses. As an application, the truncated Gaussian assumption is shown to be adequate to deal with the condition of hydrostatic stability in ocean analyses. First, a detailed evaluation of the method is made using a one-dimensional z-coordinate model of the mixed layer: particular attention is paid to the parameterization of the probability distribution, the accuracy of the estimation and the sensitivity to the observation system. In a second step, the method is applied to a three-dimensional hybrid coordinate ocean model (HYCOM) of the Bay of Biscay (at a 1/15° resolution), to show that it is efficient enough to be applied to real size problems. These examples also demonstrate that the algorithm can deal with the hydrostatic stability condition in isopycnic coordinates as well as in z-coordinates.KeywordsData assimilationInequality constraintsReduced-order Kalman filterHybrid coordinate ocean modelsChoose an option to locate/access this article:Check if you have access through your login credentials or your institution.ororRecommended articlesCiting articles (0)道底wwWp9hy如何解决,是否p9hyCoM能再恢复_百度知道
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我们会通过消息、邮箱等方式尽快将举报结果通知您。TEMPORAL AND SPATIAL VARIABILITY OF NEARSHORE FRONTS IN THE YELLOW SEA AND ITS INFLUENCE ON SEDIMENT TRANSPORT AND DEPOSITION--《Marine Geology Frontiers》2015年07期
TEMPORAL AND SPATIAL VARIABILITY OF NEARSHORE FRONTS IN THE YELLOW SEA AND ITS INFLUENCE ON SEDIMENT TRANSPORT AND DEPOSITION
ZANG ZWANG HXUE ZBI NWU XZHANG YCollege of Marine Geosciences,Ocean University of CLouisiana State UKey Laboratory of Submarine Geosciences and Technology of Ministry of EQingdao Institute of Marine Geology,China Geological S
In-situ water temperature data collected during different seasons in 2010 and 2012was compared with HYCOM reanalysis data.The results illustrated that temperature data derived from HYCOM is applicable in the Yellow Sea.Based on the HYCOM datasets,temporal and spatial variability of the thermal front and mixing front in the Yellow Sea was analyzed in detail.The results showed that the thermal front appeared in fall,became strongest in winter and disappeared gradually in spring.Seasonal variability of mixing front in the Yellow Sea was related to monsoon.Mixing front appeared in the fall and well developed in the winter.Suspended sediment was concentrated in onshore side of the thermal front that constrained the offshore transport.The thermal front in Chengshantou coastal area corresponded to mud deposit in shape and location,as the depo-center(40mthick)was located at the onshore side of the thermal front while on the offshore side the mud thickness decreased sharply.The results indicated difference between locations of the thermal front and mixing front,as the mixing front was located at the west of the thermal front where strong mixing was unfavorable for sediment accumulation.At the east side of mixing front,suspended sediment concentration was high with low turbulence,which favored rapid sediment accumulation corresponding to the mud depo-center.The spatial differences and interaction between the thermal front and mixing front might be the dynamic mechanism dominating the formation of omega("Ω")-shaped mud deposits.
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【Citations】
Chinese Journal Full-text Database
LIANG Shu xiu~(*1),SUN Zhao chen~1,NAKATSUJI Keiji~2,YAMANAKA Ryoichi~2(1.State Key Lab.of Coastal and Offshore Eng.,Dalian Univ.of Technol.,Dalian .Dept.of Civil Eng.,Osaka Univ.,Osaka 565 0871,Japan);[J];Journal of Dalian University of T2006-01
Wei Qinsheng1,2,3,Yu Zhigang1,Ran Xiangbin2,3,Zang Jiaye2,3(1.Key Laboratory of Marine Chemistry Theory and Technology,Ministry of Education,Ocean University of China,Qingdao .First Institute of Oceanography,State Oceanic Administration,Qingdao .Key Lab of Science and Engineering for Marine Ecological Environment,State Oceanic Administration,Qingdao 266061,China);[J];Advances in Earth S2011-02
WANG Yong-zhi1,2 QIAO Lu-lu3 YANG Zuo-sheng3 BAO Xian-wen3 ZHAO Mei-xun3 WANG Guan-suo1,4(1.The First Institute of Oceanography,SOA,Qingdao,Shandong .Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology,Ministry of Land and Resources,Qingdao,Shandong .College of Geo-Marine Sciences,Ocean University of China,Qingdao,Shandong .Key Lab of Marine Science & Numerical Modeling(MASNUM),Qingdao,Shandong 266061);[J];Acta Sedimentologica S2013-03
Liu A Yin X Lu Ming First Institute of Oceanography, NBO;[J];;1983-02
Zhao Baoren (Institute of Oceanology,Academia Sinica);[J];;1987-02
CHEN Hong-xia~(1,2),HUA Feng~(1,2),YUAN Ye-li~(1,2)(1.First Institute of Oceanography,SOA,Qingdao .Key Lab of Marine Science and Numerical Modeling,SOA,Qingdao 266061,China);[J];Advances in Marine S2006-04
Wang Xihou, Song Youqiang and Zhang JianminInst. of Mar. Environ. Prot. , SOA, Dalian 116023Han XishanInst. of Meteorol. Centre of Liaoning Prav. , Shenyang 110003Han Maolue, Wang Jianhua, Zhang Shuzhong and Jing BenyongDalian Central Station of Mar. O[J];Marine Science B1994-02
Tang Yuxiang Yao Lanfang (First Institute of Oceanography, SOA);[J];Transactions of Oceanology and L1989-02
Zhao Baoren (Institute of Oceanology, Academia Sinica, Qingdao);[J];Oceanologia Et Limnologia S1985-06
Qin Yunshan, Li Fan, Xu Shanmin(Institute of Oceanography, Academia Sinica, Qingdao)J. Milliman and R. Limeburner(Woods Hole Oceanographical Institution, U. S. A.);[J];Oceanologia Et Limnologia S1989-02
【Co-citations】
Chinese Journal Full-text Database
Zhu Wenting ( Tianjin University );[J];Urban Environment & Urban E1993-04
ZHAN Jin-gang1,2,WANG Yong1,XU Hou-ze1,HAO Xiao-guang1,LIU lin-tao11.Key Laboratory of Dynamic Geodesy,Chinese Academy of Sciences,Wuhan .Graduate University of the Chinese Academy of Sciences,Beijing 100039,C[J];Acta Geodaetica et Cartographica S2008-04
Yang Xiaolan
(Second Institute of Oceanography, SOA, Hangzhou, 310012);[J];DONGHAI MARINE SCIENCE;1998-01
GUO Zhigang,
YANG Zuosheng,
FAN Dejiang,
Pan Yanjun
(College of Marine Geoscience,Ocean University of China, Qingdao266003, China);[J];Acta Geographica S2003-04
LI Guosheng1, WANG Hailong1,2, DONG Chao1,2(1. Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China2. Graduate School of Chinese Academy of Sciences, Beijing 100039, China);[J];Acta Geographica S2005-05
SHI Chang-xing
, ZHANG Dian
, YOU Lian-yuan
, LI Bing-yuan
(1. Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing . Department of Geography, The University of Hong Kong,China);[J];Geographical R2003-01
WANG Fang1,2,LI Guo-sheng2(1.University of Calgary,Calgary,Alberta T2N1N4,C2.Institute of Geographic Sciences and Natural Resources Research,CAS,Beijing 100101,China);[J];Geographical R2007-06
LI Guo-sheng1,WANG Hai-long2(1.Institute of Geographic Sciences and Natural Resources Research,CAS,Beijing .Guangdong Electric Power Design Institute,Guangzhou 510663,China);[J];Geographical R2009-03
WANG Jian1,ZHAO Mei1,BAI Shi-biao1,GONG Xiao-hui1,ZHANG Mao-heng1,WU Yan-hong2,XIAO Jia-yi1(1.Department of Geography,Nanjing Normal University,Nanjing .Nanjing Institute of Limnology and Geography,CAS,Nanjing 210008,China);[J];Geographical R2009-05
gang1, YANG Zuo
sheng1, CHEN Zhi
lin2, MAO Deng1(1. College of Marine Geosciences, Ocean University of Qingdao, Qingdao 266003, C 2. Institute of Geosciences, Shengli Oil Administration Bureau, Dongying 275015, China);[J];G2001-05
China Proceedings of conference Full-text Database
Li Hong-Bo, Xiao Tian, Liu Gui-Mei, L(u|¨) Rui-Hua, Ding Tao
(Key laboratory of Marine Ecology and Environmental Science, Qingdao Institute of Oceanology,
Chinese Academy of Sciences, Qingdao 266071, CGraduate School, Chinese Academy of
Sciences, Beijing 100039, CFirst Institute of Oceanography, SOA, Qingdao 266061, C
Laboratory of Ocean Dynamic Processes and Satellite Oceanography, Second Institute of
Oceanography, SOA, Hangzhou 310012, China).;[A];[C];2004
CAI Yu-ting (Fisheries Research Institute of Fujian,Xiamen 361012,China);[A];[C];2009
Zhao Bao-hong1,1LIU Yu-di 1,2,Zhao Jia-hua1,Zhou Xiao-lin1 1 Institute of Meteorology,PLA University of Science and Technology,Nanjing
Institute of Oceanology,Chinese Academy Sciences,Qingdao 266071;[A];[C];2011
LI Yu-HAN MZHOU Yan-FAN Pei-Naval Submarine A;[A];[C];2014
Jianxing LXuefa SShulan Ge;Qingsong LZhengquan YGang YPaleomagnetism and Geochronology Laboratory (SKL-LE),Institute of Geology and Geophysics,Chinese Academy of SUniversity of Chinese Academy of SKey Laboratory of Marine Sedimentation and Environmental Geology,First Institute of Oceanography,State Oceanic A;[A];[C];2015
Liang Yi;Xingyong Ye;Junbing CYan Li;Hao LXulong WJinhua Du;Songling ZChenglong DState Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of SMSG Group,Sanya Institute of Deep-sea Science and Engineering,Chinese Academy of SZhejiang Institute of Hydrogeology and Engineering GSchool of Ocean Sciences,China University of GState Key Laboratory of Lake Science and Environment,Nanjing Institute of Geography and Limnology,Chinese Academy of SState Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment,Chinese Academy of SKey Laboratory of Marine Geology and Environment,Institute of Oceanology,Chinese Academy of S;[A];[C];2015
Yan ZHongbo ZChenglong DQingsong LState Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of SLaboratoire des Sciences du Climat et de l'Environment/IPSL,CEA/CNRS/UVSQ,Avenue de la Terrasse,91198 Gif-sur-Yvette cedex,FSchool of Geography Science,Nanjing Normal U;[A];[C];2015
Qin Li;Haibin Wu;Yanyan Yu;Aizhi SSlobodan B.Markovi?;Zhengtang GKey Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of SUniversity of Chinese Academy of SChair of Physical Geography, Faculty of Sciences, University of Novi S;[A];[C];2015
【Secondary Citations】
Chinese Journal Full-text Database
XIA Jie,GAO Hui-wang(Key Lab of Marine Environmental Science and Ecology Ministry of Education,Ocean University of China,Qingdao 266003,Shandong,China);[J];Journal of Safety and E2006-04
Lin Xianyu and Chu Yongan (General Hydrological Station of Zhejiang Province);[J];Donghai Marine S1984-04
YANG Hai-li1,ZHENG Yu-long1,HUANG Zhi2(1.Second Institute of Oceanography,SOA,Laboratory of Submarine Geosciences,SOA,Hangzhou .Xinglongtai Oil Field,Liaohe Branch Company,CNPC Panjin 124000,China);[J];Journal of Marine S2007-01
GUO Zhigang,
YANG Zuosheng,
FAN Dejiang,
Pan Yanjun
(College of Marine Geoscience,Ocean University of China, Qingdao266003, China);[J];Acta Geographica S2003-04
QI Jun1,2, LI Feng-ye1, SONG Jin-ming1 1. Key Laboratory of Marine Ecology and Environmental Science, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, C 2. Graduate School of Chinese Academy of Sciences, Beijing 100039, C[J];G2005-04
LIU Guimei (刘桂梅), WANG Hui(王辉), SUN Song(孙松), and HAN Boping(韩博平)
Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071
ICCES, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029 National Natural Science Foundation of China, Beijing 100085;[J];大气科学进展(英文版);2003-03
WU De-xing~1,LAN Jian~2(1.Key Laboratory of Oceanography,Qingdao .Department of Oceanography,Ocean University of China,Qingdao 266003,China);[J];Advances in Earth S2006-07
WEI Qinsheng1,2,Lü Xin′gang1,3,WANG Zongxing1,2,WANG Shouqiang1,2,ZANG Jiaye1,2(1.First Institute of Oceanography,State Oceanic Administration,Qingdao .Key Laboratory of Science and Engineering for Marine Ecological Environment,State Oceanic Administration,Qingdao .Key Laboratory of Marine Science and Numerical Modeling,State Oceanic Administration,Qingdao 266061,China);[J];Advances in Earth S2010-04
Liu G Yin Yi First Institute of Oceanography, NBO;[J];;1984-01
Zheng Y Ding L Tan Duo First Institute of Oceanography, NBO;[J];;1985-01
(C)2006 Tsinghua Tongfang Knowledge Network Technology Co., Ltd.(Beijing)(TTKN) All rights reservedA Coupled Regional Climate Model Simulation of Typhoon Son-Tinh with Increased Horizontal Resolutions--《Periodical of Ocean University of China》2015年03期
A Coupled Regional Climate Model Simulation of Typhoon Son-Tinh with Increased Horizontal Resolutions
WAN Xiu-QMA Wei-WWU De-XLI Ming-KOcean University of China,College of Physical and Environmental OOcean University of China,The Key Laboratory of Physical Oceanography,Ministry of E
Numerical model is one of the main means to study typhoon process,and how to improve the precision of typhoon simulation has become more important.Although considerable progress has been made in our understanding of the dynamic and thermodynamic mechanisms of typhoon process,there is still long way to go to simulate and predict typhoon in reality.Based on a regional coupled model developed recently in Ocean University of China,we set up a series of numerical experiments to simulate typhoon Son-Tinh occurred in South China Sea in 2012 with increased horizontal model resolutions.The NCEP FNL Operational Global Analysis data and HYCOM Global Analysis data are applied as initial and boundary conditions to all the experiments.The results indicate that air-sea coupling and higher resolution can improve the model capability to simulate typhoon process.The oceanic responses to typhoon are also discussed.
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ZHANG Xiaoyan WANG B JI Zhongzhen Qingnong XIAO , and ZHANG Xin
LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029 Mesoscale and Microscale Meteorology, National Center for Atmospheric Research, Boulder, Colorado, USA;[J];大气科学进展(英文版);2003-04
Chen Lianshou and Meng Zhiyong (Chinese Academy of Meteorological Setences, Beijing 100081);[J];Chinese Journal of Atmospheric S2001-03
ZENG Zhi-hua1-2,CHEN Lian-shou3(1.Nanjing University of Information Science and Technology,Nanjing 210044,C 2.Shanghai Typhoon Institute,Laboratory of Typhoon Forecast Technique/China Meteorological Administration, Shanghai 200030,C 3.Chinese Academy of Meteorological Sciences,China Meteorological Administration,Beijing 100081,China);[J];Plateau M2011-06
Liu Ningwei Wang Feng'an(Institute of Atmospheric Environment,CMA,Shenyang 110016);[J];Meteorological Science and T2006-04
Chen Yuling 1 Zhou Jun 2 Ma Fenhua 2 (1 Department of Physical Sciences,NIM ,Nanjing 210044) (2 Department of Atmospheric Sciences,NIM,Nanjing 210044);[J];Scientia Meteorologica S2005-03
Fei Jianfang1 Huang Xiaogang1 Cheng Xiaoping1 Zheng Jing2(1 Institute of Meteorology,PLA University of Science and Technology,Nanjing 211101,China)(2 73061Troop of PLA,Jiangsu Xuzhou 221008,China);[J];Scientia Meteorologica S2010-05
Zhao Ping (Chinese Academy of Meteorological Sciences, Beijing 100081);[J];Acta Meteorologica S2003-06
HA HyeKyeong1,2,3,WANG Zhen-hui1,2,KIM Jeoung-Yun1,4,3,NIU Sheng-Jie1,SUH AeSook3 (1.Jiangsu Key Laboratory of Meteorological Disaster,NUIST,Nanjing .School of Remote Sensing,NUIST,Nanjing .Korea Meteorological Administration,Seoul 156-720,K4.Key Laboratory of Atmospheric Physics and Atmospheric Environment,NUIST,Nanjing 210044,China);[J];Journal of Tropical M2009-04
LIN Fang-ni1,2,WAN Qi-lin1,GUAN Zhao-yong1 (1.Nanjing university of information Science & Technology,Nanjing 210044,C 2.Institute of Tropical and Marine Meteorology,CMA,Guangzhou 510080,China);[J];Journal of Tropical M2011-02
LIAO Jing-biao1,2,WANG Xue-mei1,XIA Bei-cheng1,WANG Ti-jian2,WANG Zhi-ming1(1.School of Environmental Science and Engineering,Sun Yat-Sen University,Guangzhou 510275,China)(2.School of Atmospheric Sciences,Nanjing University,Nanjing 210093,China);[J];Journal of Tropical M2012-04
【Co-citations】
Chinese Journal Full-text Database
PAN Jun et al (Atmospheric Science Department,Physics School of Peking University,Beijing 100871);[J];Journal of Anhui Agricultural S2010-22
WANG Yuan-chao et al(Yulin Meteorological Bureau in Guangxi,Yulin,Guangxi 537000);[J];Journal of Anhui Agricultural S2010-34
LU Bing 1,WANG Bin 1,and ZHAO Ying 2 1 State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,China 2 Institute of Sciences,University of Science and Technology of the Chinese People's Liberation Army,Nanjing 211101,C[J];大气和海洋科学快报(英文版);2011-04
WANG Shu-Dong 1,2,LIU Juan-Juan 2,and WANG Bin 2 1 Meteorological Observation Centre,China Meteorological Administration,Beijing 100081,China 2 Laboratory of Numerical Modeling for Atmospheric Sciences & Geophysical fluid dynamics (LASG),Institute of Atmospheric Physics (IAP),Chinese Academy of Sciences,Beijing 100029,C[J];大气和海洋科学快报(英文版);2011-05
ZHANG Qinghong
1)Department of Atmospheric Science,Peking University, Beijing 100871;
2)Weather Centre,Northeast Air Traffic Administration Bureau,Shenyang,110169);[J];Acta Scicentiarum Naturalum Universitis P2004-01
DAI Zhanpeng,ZHANG Qinghong? Department of Atmospheric and Oceanic Sciences,School of Physics,Peking University,Beijing 100871;?;[J];Acta Scientiarum Naturalium Universitatis P2011-02
CHEN Zhao-hui1,CHENG Shui-yuan1,SU Fu-qing2,GAO Qing-xian2(1.College of Environmental and Energy Engineering,Beijing University of Technology,Beijing .Chinese Research Academy of Environmental Sciences,Beijing 100012,China);[J];Journal of Beijing University of T2010-02
HOU Jian-zhong1,NING Zhi-qian1,XIE Shuang-ting1,DENG Ai-jun2 (1.Shaanxi Bureau of Meteorology,Xi'an .Pennsylvanian State University,PA 16802,US);[J];Journal of Chengdu University of Information T2007-05
HOU Jian-zhong1,XU Xin-tian1,ZHANG Xiao-ling2,LI Ming1,DUAN Chang-hui1(1.Shaanxi Bureau of Meteorology,Xi'an .National Meteorological Center,Beijing 100081,China);[J];Journal of Chengdu University of Information T2008-05
ZENG Xin-xin, HUANG Xin-qing, TENG Dai-gao(Meteorological Observatory of Zhejiang Province, Hangzhou 310017, China);[J];Journal of Marine S2010-01
China Proceedings of conference Full-text Database
HU Shu~(1,2) LI Ying~1 WEI Na~2 1 Oceanic Hydrologic Center of Navy,Beijing
State Key Laboratory of Severe Weather,Chinese Academy of Meteorological Sciences,Beijing 100082;[A];[C];2012
Huizhong He1 Minghu Cheng2 Fengxian Zhou3 1 State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing
Chinese Academy of Meteorological Sciences, Beijing
Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100080;[A];[C];2005
Wei Ying-zhi1,2, Tang Da-zhang2 Xu Jian-min3, Wu Chen-feng1
(1. Xiamen Meteorological Bureau, Xiamen 361012, Fujian C 2. Nanjing University of Information Science and Technology, Nanjing 210044, C 3. National Satellite Meteorological Center, Beijing 100081, China );[A];[C];2005
Ye Chengzhi1 Chenri2 Xu Aihua3 Pan Zhixiang4 (1. Institute of Heavy Rain,CMA,Wuhan) (2.LASG; 3. Jiangxi Meteorological Office, 4. Hunan Meteorological Office,Changsha );[A];[C];2005
ZHANG Hong, Liang Shengjun, Hou Jianzhong (Shaanxi Meteorological Observatory, Xian, Shaanxi 710015);[A];[C];2005
Yu Zhenshou1 Ji Chunxiao2 Wang Zhongdong1 Lou Liyin1 Wu Mengchun1 (1.Wenzhou Meteorological Bureau, Wenzhou,325003) (2.Zhejiang Research Institute of Meteorology,Hangzhou,310002);[A];[C];2005
Zhou Fengcai1 Zhang Xijun2
1 Shanghai Meteorological Center, Air Traffic Management Bereau of East China, Shanghai
Institute of Meteorology, PLA University of Science and Engineering, Nanjing 211101;[A];[C];2006
Huang Yanyan, Yan Jinghua, Meng Weiguang, Wan Qilin
(Institute of Tropical and Marine Meteorology, CMA, Guangzhou 510080 );[A];[C];2008
ZHANG Jian-Hai YU Zhong-Kai (Shaoxing Meteorological bureau,shaoxing 312000, China);[A];[C];2008
LI Gang1, WANG Tie1 TAN Yan-ke1 FENG Wen-tian2 (1. Institute of Meteorology, PLA Univ.of Sci&Tech., Nanjing 211101,C(2. No.66393 Troops of PLA,071000,China);[A];[C];2009
【Secondary Citations】
Chinese Journal Full-text Database
Fei Jianfang and Lu HanchengAir Force Institute of Meteorology,Nanjing 211101;[J];大气科学进展(英文版);1996-04
ZHANG Xiaoyan WANG B JI Zhongzhen Qingnong XIAO , and ZHANG Xin
LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029 Mesoscale and Microscale Meteorology, National Center for Atmospheric Research, Boulder, Colorado, USA;[J];大气科学进展(英文版);2003-04
ZENG Zhihua 1,2 , Yuqing WANG 3 , DUAN Yihong 4 , CHEN Lianshou 5 , and GAO Zhiqiu 2 1 Laboratory of Typhoon Forecast Technique, Shanghai Typhoon Institute/ China Meteorological Administration, Shanghai
The State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing
International Pacific Research Center and Department of Meteorology, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, Honolulu, HI 96822, USA 4 National Meteorological Center, China Meteorological Administration, Beijing
Chinese Academy of Meteorological Sciences, China Meteorological Administration, Beijing 100081;[J];大气科学进展(英文版);2010-02
Chen Lianshou (Chinese Academy of Met6orological Science,Beijing 100081)and Luo Zhexian(Naming institute of Meteorology,Naming 210044);[J];大气科学进展(英文版);1995-02
Wang Donghai and Zhou Xiaoping(Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100080);[J];Chinese Journal of Atmospheric S1994-01
Zhu Hongyan, Chen Lianshou and Xu Xiangde (Chinese Academy of Meteorological Sciences, Beijing 100081);[J];SCIENTIA ATMOSPHERICA SINICA;2000-05
Chen Lianshou and Meng Zhiyong (Chinese Academy of Meteorological Setences, Beijing 100081);[J];Chinese Journal of Atmospheric S2001-03
Luo Zhexian (Naming Institute of Meteorology, Nanjing 210044);[J];SCIENTIA ATMOSPHERICA SINICA;1994-05
Zhai G Gao K Yu Zhangxiao and Tu Caihong (Department of Geography, Hangzhou University, Hangzhou 310028);[J];SCIENTIA ATMOSPHERICA SINICA;1995-04
Luo ZChen Lianshou (Nanjing Institute of Meteorology, Nanjing 210044) (Academy of Meteorological Science, Beijing 100081 );[J];SCIENTIA ATMOSPHERICA SINICA;1995-06
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