近60年莱州湾东部砂质海岸地貌的时空动态

doi:DOI:10.3969/J.ISSN.0253-4193.2017.09.009

CORC > 烟台海岸带研究所 > 中国科学院烟台海岸带研究所 > 中科院海岸带环境过程与生态修复重点实验室 > 近岸生态与环境实验室

	近60年莱州湾东部砂质海岸地貌的时空动态
	战超 ; 于君宝 ; 王庆 ; 栗云召 ; 周迪
刊名	海洋学报
	2017-09-15
卷号	39 期号:9 页码:90-100
关键词	sandy coast shoreline subaqueous slope geomorphic evolution anthropogenic activities 砂质海岸海岸线水下岸坡地貌演变人类活动
ISSN号	0253-4193
DOI	DOI:10.3969/J.ISSN.0253-4193.2017.09.009
其他题名	Spatial and temporal dynamics of sandy coastal geomorphology in the east of Laizhou Bay over recent 60years
产权排序	(1) 中国科学院烟台海岸带研究所 ; (2) 鲁东大学滨海生态研究院 ; (3) 中国科学院大学
文献子类	Article
英文摘要	Based on the results of field surveys,the spatial and temporal dynamics of sandy coastal geomorphology along the eastern Laizhou Bay over the last 60years was investigated using the comprehensive methods of digital shoreline analysis,remote sensing and geographic information system technologies.The data mainly derived from the nautical charts,topographic maps and high resolution remote sensing images which measured and imaged in different periods.The results show that there are significant spatial-temporal variations in both the sandy coast shoreline migration and the subaqueous slope erosion-deposition evolution along the eastern Laizhou Bay.The alternate regulation of forward and backward for shoreline migration is caught in this study.There is a remarkable non-linear characteristic in the time process.The proportion of the erosional shoreline is fluctuated and phased from 1959to 2013.The average annual evolution rate of eroded coast is divided into two stages by 1985.The erosion rate decreased from the maximum value of 4.95m/a(during the period of 1959-1969)to minimum value 1.97m/a (1969-1985)at prophase.In the late period,the erosion rate increased from 1.97m/a to 4.43m/a(1985- 1998),and the coast was in serious erosion state since then.The characteristics of shoreline migration in four headland bays are not consistent with overall trend.At the same time,the scouring strips distribute alternating with the silting of the subaqueous slope.The trend of scouring and silting evolution was basically opposite in the same coast between the periods of 1959-1985and 1985-2008.Further analysis indicate that there are 5alternations of erosion and deposition and the changes of rate of erosion and siltation,under the control of geomorphic effects of anthropogenic activities such as sediment trapping by reservoirs,fishing culture in supratidal zone and coastal engineering, in the east of Laizhou Bay during recent 60years.
WOS关键词	Oceanography
WOS研究方向	Oceanography ; 海洋学
语种	中文
CSCD记录号	CSCD:6058434
内容类型	期刊论文
源URL	[http://ir.yic.ac.cn/handle/133337/24284]
专题	烟台海岸带研究所_近岸生态与环境实验室烟台海岸带研究所_海岸带信息集成与综合管理实验室烟台海岸带研究所_滨海湿地实验室
作者单位	1.中国科学院烟台海岸带研究所; 2.中国科学院大学 3.鲁东大学滨海生态研究院;
推荐引用方式 GB/T 7714	战超,于君宝,王庆,等. 近60年莱州湾东部砂质海岸地貌的时空动态[J]. 海洋学报,2017,39(9):90-100.
APA	战超,于君宝,王庆,栗云召,&周迪.(2017).近60年莱州湾东部砂质海岸地貌的时空动态.海洋学报,39(9),90-100.
MLA	战超,et al."近60年莱州湾东部砂质海岸地貌的时空动态".海洋学报 39.9(2017):90-100.