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20世纪40年代初以来渤海形态变化特征

  • 宋洋 ,
  • 张华 ,
  • 侯西勇
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  • 1 中国科学院烟台海岸带研究所 中国科学院海岸带环境过程与生态修复重点实验室, 山东 烟台 264003;
    2 中国科学院大学, 北京 100049

收稿日期: 2017-09-01

  修回日期: 2017-12-22

  网络出版日期: 2018-11-15

基金资助

中国科学院烟台海岸带研究所自主部署项目(YICY755011031)、中国科学院重点部署项目(KZZD-EW-14)、中国科学院战略性先导科技专项(XDA11020305)和国家自然科学基金(31461143032)资助

Shape changes of Bohai Sea since the early 1940s

  • SONG Yang ,
  • ZHANG Hua ,
  • HOU Xiyong
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  • 1 Key Laboratory of Coastal Environmental Processes and Ecological Remediation of Chinese Academy of Sciences, Yantai Institute of Coastal Zone Research, Chinese Academy of Sciences, Yantai 264003, Shandong, China;
    2 University of Chinese Academy of Sciences, Beijing 100049, China

Received date: 2017-09-01

  Revised date: 2017-12-22

  Online published: 2018-11-15

摘要

20世纪中期以来中国沿海经历了多次围填海热潮,2000年以来环渤海区域大规模围填海已使其成为近期中国围填海的重点区域。利用地形图、海图和遥感影像等资料获取的渤海多时相的平面重心、立体重心、海岸线、低潮线、等深线、海区面积和海区体积等指标变化信息,系统揭示渤海形态的长期变化特征。结果表明:近70年来,渤海面积不断萎缩,岸线普遍向海扩张,导致渤海的平面重心总体向东偏北方向移动,但渤海的平面周长总体呈增加趋势,平面形状趋于复杂;近50年来,渤海体积总体呈下降趋势,立体重心的位置趋于变深。自然条件下的河口三角洲发育和人类围填海活动是渤海形态变化的主要原因,但渤海形态变化的驱动力已由早期的以自然因素为主转变为近期的以人类活动因素为主。

本文引用格式

宋洋 , 张华 , 侯西勇 . 20世纪40年代初以来渤海形态变化特征[J]. 中国科学院大学学报, 2018 , 35(6) : 761 -770 . DOI: 10.7523/j.issn.2095-6134.2018.06.007

Abstract

China has experienced several booms in sea reclamation since the mid-20th century. The reclamation in Bohai Rim expanded dramatically in a scale much larger than in other coastal zones in China, especially since 2 000. Therefore, based on topographic maps, nautical charts, and multi-temporal remote sensing imageries, the two-dimensional centroid, three-dimensional centroid, shoreline, low tide line, depth contour, bay area, and water volume of Bohai Sea since the 1940s were extracted and analyzed to reveal the tendencies, characters, and driving factors of long-term shape changes of Bohai Sea. The results indicate that, during the past 70 years, the area of Bohai Sea decreased continuously and that shoreline, low tide line, and 5 m isobaths shifted toward the sea in most coastal areas. Consequently, the two-dimensional centroid of Bohai Sea moved northeastward significantly, while the perimeter increased remarkably and the geometric shape became complicated. During the past 50 years, overall, the volume of Bohai Sea declined and the three-dimensional centroid dived significantly. The development of estuary delta and sea reclamation were the fundamental driving forces of long-term shape changes of Bohai Sea. However, the human forces have gradually exceeded the natural forces.

参考文献

[1] 徐晓达,曹志敏,张志珣,等. 渤海地貌类型及分布特征[J]. 海洋地质与第四纪地质, 2014, 34(6):171-179.
[2] 盖美,张丽平,田成诗. 环渤海经济区经济增长的区域差异及空间格局演变[J]. 经济地理, 2013, 33(4):22-28.
[3] 马万栋,吴传庆,殷守敬,等. 环渤海围填海遥感监测及对策建议[J]. 环境与可持续发展, 2015, 40(3):63-65.
[4] 王勇智,吴頔,石洪华,等. 近十年来渤海湾围填海工程对渤海湾水交换的影响[J]. 海洋与湖沼, 2015, 46(3):471-480.
[5] Hou X Y, Wu T, Hou W, et al. Characteristics of coastline changes in mainland China since the early 1940s[J]. Science China Earth Sciences, 2016, 59(9):1791-1802.
[6] 李亚宁,王倩,郭佩芳,等. 近20a来渤海岸线演替及其开发利用策略[J]. 海洋湖沼通报, 2015(3):32-38.
[7] 程钰,刘凯,徐成龙,等. 山东半岛蓝色经济区人地系统可持续性评估及空间类型比较研究[J]. 经济地理, 2015, 35(5):118-125.
[8] 高文斌,刘修泽,段有洋,等. 围填海工程对辽宁省近海渔业资源的影响及对策[J]. 大连水产学院学报, 2009, 24(S1):163-166.
[9] 胡聪,于定勇,赵博博. 天津滨海新区围填海工程对海洋资源影响评价[J]. 海洋环境科学, 2014, 33(2):214-219.
[10] 胡聪,于定勇,赵博博. 围填海工程对海洋资源影响评价:以曹妃甸为例[J]. 城市环境与城市生态, 2014, 27(1):42-46.
[11] 叶小敏,丁静,徐莹,等. 渤海湾近30年海岸线变迁与分析[J]. 海洋开发与管理, 2016, 33(2):56-62.
[12] 李仕涛,王诺,张源凌,等. 30a来渤海填海造地对海洋生态环境的影响[J]. 海洋环境科学, 2013, 32(6):926-929, 938.
[13] Jiang L,Wu S H,Yang Q H, et al. Spatial distribution and temporal evolution of sediment transport pathway of deltaic deposits in a rift basin:an example from Liaodong Bay Sub-basin, Bohai Bay, China[J]. Australian Journal of Earth Sciences, 2016, 63(4):469-483.
[14] Zhu L,Wu J,Xu Z, et al. Coastline movement and change along the bohai sea from 1987 to 2012[J]. Journal of Applied Remote Sensing, 2014, 8(1):083585.
[15] 王诺,许雪青,吴暖,等. 渤海污染风险与生态系统功能价值评价研究[J].海洋湖沼通报, 2015, 24(1):167-174.
[16] 夏东兴,刘振夏. 中国海湾的成因类型[J]. 海洋与湖沼, 1990, 21(2):185-191.
[17] 侯西勇,毋亭,王远东,等. 20世纪40年代以来多时相中国大陆岩线提取方法及精度评估[J]. 海洋科学, 2014, 38(11):66-73.
[18] 侯西勇,侯婉,毋亭. 20世纪40年代初以来中国大陆沿海主要海湾形态变化[J].地理学报, 2016, 71(1):118-129.
[19] 徐雷诺. 我国各种高程系之间的换算及应用[J]. 治淮, 2009(10):44-45.
[20] 吴家乃,朱梅心. 论我国高程基准面问题[J]. 河海大学学报, 1991, 19(1):59-64.
[21] David T I, Mukesh M V, Kumaravel S, et al. Long-and short-term variations in shore morphology of Van Island in gulf of Mannar using remote sensing images and DSAS analysis[J]. Arabian Journal of Geosciences, 2016,9(20):756-763.
[22] Wang Y D, Hou X Y, Jia M M, et al. Remote detection of shoreline changes in eastern bank of Laizhou Bay, North China[J]. Journal of the Indian Society of Remote Sensing, 2014, 42(3):621-631.
[23] 刘蕾,臧淑英,邵田田,等. 基于遥感与GIS的中国湖泊形态分析[J]. 国土资源遥感, 2015, 27(3):92-98.
[24] 李玉冰,郝永杰,刘恩海. 多边形重心的计算方法[J]. 计算机应用, 2005, 25(S1):391-393.
[25] 乔伟峰,刘彦随,王亚华,等. 城市三维重心算法与实验分析:以南京市为例[J]. 地理信息科学, 2015, 17(3):268-273.
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