TAO Ying-Jia, GE Jian-Zhong, DING Ping-Xing. Design and application of saltwater intrusion forecastingsystem in the Changjiang Estuary[J]. Journal of East China Normal University(Natural Sc, 2016, 2016(2): 128-143.
[1]顾玉亮, 吴守培, 乐勤.北支盐水入侵对长江口水源地影响研究[J].人民长江,2003,34(4):13.[2]贺松林, 丁平兴, 孔亚珍.长江口南支河段枯季盐度变异与北支咸水倒灌[J].自然科展,2006,16(5):585587[3]沈焕庭, 茅志昌, 朱建荣.长江河口盐水入侵[M].北京:海洋出版社,2003.[4]郑晓琴,肖文军,于芸,等.基于径流和潮汐的长江口盐水入侵统计预测研究[J].海洋预报,2014,04:1823.[5]吴辉.长江河口盐水入侵研究——北支倒灌、深水航道工程和冬季季风的影响[D].上海:华东师范大学河口海岸科学研究院,2006.[6]李路.长江河口盐水入侵时空变化特征和机理[D].上海:华东师范大学河口海岸科学研究院,2011.[7]WU H,ZHU J R,CHOI B H. Links between saltwater intrusion and subtidal circulation in the Changjiang Estuary: A modelguided study [J]. Continental Shelf Research,2010,30:18911905.[8]LI L,ZHU J R,WU H. Impacts of wind stress on saltwater intrusion in the Yangtze Estuary [J].Science China Earth Sciences,2012,55(7): 11781192.[9]裘诚.长江河口盐水入侵对气候变化和重大工程的响应[D].上海:华东师范大学河口海岸科学研究院,2014.[10]林唐宇.横沙东滩淡水资源研究及长江盐水入侵预报模型[D].上海:华东师范大学河口海岸科学研究院,2014.[11]CHEN C,LIU H,BEARDSLEY R C.An unstructured grid,finitevolume,threedimensional,primitive equations ocean model:Application to coastal ocean and estuaries[J].Journal of Atmospheric and Oceanic Technology,2003,20(1):159186.[12]CHEN C,COWLES G,BEARDSLEY R C.An unstructured grid,finitevolumecoastal ocean model:FVCOM user manual[R].2nd ed. SMAST/UMASSD Technical Report060602,2006:45.[13]CHEN C,BEARDSLEY R C,COWLES G.An unstructured grid,finitevolumecoastal ocean model (FVCOM) system[J].Oceanography:Special Issue,2006,19(1):7889[14]UMLAUF L, BURCHARD H, BOLDING K. GOTM. Sourcecode and test case documentation.Version 3.2[R].MeereswissBer, 2005:63.[15]葛建忠.MultiScale FVCOM model system for the East China Sea and Changjiang estuary and its applications[D].上海:华东师范大学河口海岸科学研究院,2010.[16]海洋图集编委会.渤海黄海东海海洋图集[M].北京:海洋出版社,1993.[17]WILLMOTT C J. On the validation of models[J].Phys Geogr,1981(2):184194.