ZHU Jian-rong, WU Hui. Numerical simulation of the longest continuous days unsuitable for water intake in the Dongfengxisha reservoir of the Changjiang Estuary[J]. Journal of East China Normal University(Natural Sc, 2013, 2013(5): 1-8, 26.
[1] 朱建荣,傅利辉,吴辉. 风应力和科氏力对长江河口没冒沙淡水带的影响[J]. 华东师范大学学报:自然科学版,2008(6):1-8.[2] 项印玉,朱建荣,吴辉. 冬季陆架环流对长江河口盐水入侵的影响[J].自然科学进展,2009,19(2):192-202.[3] WU H, ZHU J R, CHOI B H. Links between saltwater intrusion and subtidal circulation in the Changjiang Estuary: A model- guided study[J]. Continental Shelf Research, 2010, 30:1891-1905.[4] LI L, ZHU J R, WU H, et al. A numerical study on the water diversion ratio of the Changjiang Estuary during the dry season[J]. Chinese Journal of Oceanology and Limnology, 2010, 28 (3):700-712.[5] 朱建荣,吴辉,顾玉亮. 长江河口北支倒灌盐通量数值分析[J]. 海洋学研究,2011,29(3):1-7.[6] LI L, ZHU J R, WU H. Impacts of wind stress on saltwater intrusion in the Yangtze Estuary[J]. Sci China Earth Sci, 2012, 55(7):1178-1192.[7] QIU C, ZHU J R, GU Y L. Impact of seasonal tide variation on saltwater intrusion in the Changjiang River estuary[J]. Chinese Journal of Oceanology and Limnology, 2012, 30(2):342-351.[8] XU K, ZHU J R, GU Y L. Impact of the eastern Water Diversion from the South to the North Project on the saltwater intrusion in the Changjiang Estuary[J]. Acta Oceanol Sin, 2012, 31(3):47-58.[9] 海洋图集编委会.渤海黄海东海海洋图集(水文)[M].北京:海洋出版社,1992,13-168.[10] 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,2003,15-74.[11] 陈西庆,张二凤,李道季,等.长江枯季入海流量变化趋势的初步研究[M]//陈吉余、陈西庆、陈美法.南水北调(东线)对长江口生态环境影响及其对策.上海:华东师范大学出版社, 2003:120-128.[12] 张二风, 陈西庆. 长江(大通-徐六泾)抽引水工程初步调查及其对枯季入海流量的影响对策[M]//陈吉余、陈西庆、陈美法.南水北调(东线)对长江口生态环境影响及其对策.上海:华东师范大学出版社, 2003:205-214.