黄河三角洲岸线变迁对莱州湾流场和对虾早期栖息地的影响
The effects of the Huanghe River Delta on the circulation and transportation of larvae
-
摘要: 用高分辨率的三维陆架海模式对黄河三角洲岸线变迁前后渤海流场进行了数值模拟,探讨了环流对对虾卵子和幼体的输运作用.结果表明,三角洲岸线变迁只对黄河口附近环流,尤其是莱州湾流场有较大的影响,而对其他区域的环流影响很小.三角洲岸线变迁前,莱州湾主要呈一反气旋环流,水体从莱州湾的东部进入,在湾内呈顺时针方向运动,从湾的西北部流出.目前,受三角洲岸线外伸的影响,在黄河口出现一对显著的岬角旋涡对,东南部的流场与岸线变迁相反,为顺着岸流出湾外.这些环流主要是潮与局部地形相互作用所致.风和斜压作用会影响环流的强弱,但其分布格局相似.三角洲岸线变迁前,对虾的卵子和幼体受环流的输运,被带至莱州湾的西部近岸,与历史上的对虾早期栖息地相吻合.三角洲岸线变迁后,位于西北部的对虾的卵子和幼体被黄河口南部的岬角旋涡捕陷于流涡内,而位于东南部的对虾的卵子和幼体则被捕陷于刁龙嘴附近的流涡中,不利于对虾仔幼在莱州湾生长.研究结果从一个侧面说明了近年来莱州湾对虾早期栖息地逐渐消失的原因.Abstract: The Huanghe River has run the current path since its last change of path in 1976.The river delta intrudes into the Laizhou Bay significantly.The effects of the Huanghe River Delta on the circulation and transportation of the eggs and larvae were investigated with a fine resolution 3-D shelf ocean model(HAMSOM).The effects are local but very significant.Before the intrusion of delta,the anti-cyclonic circulation dominates in the Laizhou Bay. At present,the circulation is totally different from that before the intrusion.Apair of headland eddies at the Huanghe River mouth is very significant.The change of the circulation is mainly due to the inter action between tides and bathymetry.Wind and baroclinic forcings also play an important role on the circulation,but the basic pattern remains.The eggs and larvae are transported tow ards the west part of bay before the intrusion of delta,which coincides with the historical nursery ground.At present,the eggs and larvae are trapped in the headland eddies, which has disadvantage on the later stage of larvae.The results may explain to some extent for the lost of the nursery ground of Peneous Chinensis.
-
中国海湾志编纂委员会.中国海湾志,第十四分册(重要河口)[M].北京:海洋出版社,1998,799 赵保仁,庄国文,曹德明,等.渤海的环流、潮余流及其对沉积物分布的影响[J].海洋与湖沼,1995,26(5):466-473. 窦振兴,张存智,张砚峰.渤海风海流的数值计算[J].海洋学报,1986,8(5):527-533. 缪经榜,刘兴泉.北黄海和渤海冬季环流动力学数值实验[J].海洋学报,1989,11(1):15-22. 郑连远.三维潮致拉格朗日余流的数值计算及其在渤海中的应用[J].青岛海洋大学学报,1992,22(1):39-49. 王辉,苏志清,冯士,等.渤海三维风生-热盐-潮致Lagrange余流数值计算[J].海洋学报,1993,15(1):9-21 黄大吉,陈宗镛,苏纪兰.三维陆架海模式在渤海中的应用Ⅰ.潮流、风生环流及其相互作用[J].海洋学报,1996,18(5):1-13. 黄大吉,陈宗镛,苏纪兰.三维陆架海模式在渤海中的应用Ⅱ.温度的季节性变化[J]海洋学报,1996,18(6):8-17. 赵保仁,曹德明.渤海冬季环流形成机制动力学分析及数值研究[J].海洋与湖沼,1998,29(1):86-96. 黄祖珂.渤海的潮波系统及其变迁[J].青岛海洋大学学报,1991,21(2):1-12 乐肯堂,周参武.黄河口的变迁对滨海大陆架区流场变化的影响[J].海洋科学集刊,1995,36:93-109 邓景耀,叶昌臣,刘永昌渤黄海的对虾及其资源管理[M].北京:海洋出版社,1990. 李泽刚.黄河口附近海区水文要素基本特征[J].黄渤海海洋,2000,18(3):20-28. 邓景耀,庄志猛.中国对虾的种群动态特征[A].苏纪兰,唐启升等.中国海洋生态系统动力学研究Ⅱ.渤海生态系统动力学过程[C].北京:科学出版社,2002.44.
计量
- 文章访问数: 873
- HTML全文浏览量: 21
- PDF下载量: 969
- 被引次数: 0