Please wait a minute...
img

Wechat

Adv search
JOURNAL OF DESERT RESEARCH  2015, Vol. 35 Issue (3): 783-791    DOI: 10.7522/j.issn.1000-694X.2014.00043
    
Lake Evolution and Effect Analysis of Meadow-dunes Area in the Horqin Sandy Land in 1986-2013
Jia Ke1, Liu Tingxi1, Lei Huimin2, Duan Limin1, Luo Yanyun1, Zhang Shengwei1, Tong Xin1, Sun Li1
1. College of Water Conservancy and Civil Engineering, Inner Mongolia Agricultural University, Huhhot 010018, China;
2. Department of Hydraulic Engineering, Tsinghua University, Beijing 100084, China
Download:  PDF (4013KB) 
Export:  BibTeX | EndNote (RIS)      
Abstract  

Lake changes sensitively recorded the messages of climate change. The Horqin typical sandy meadow area is chosen as the study area. The lake area information from 1986 to 2013 were extracted to analyze the variation law and spatial distribution characteristics using the multi temporal TM/ETM+ remote sensing images, based on remote sensing and GIS technology. The simulation and analysis of the lake area were performed using multivariate statistical analysis method combining with factors of precipitation, evaporation and the human activity effect time factor t. The results showed that: ①The numbers and area of lake in the study area have changed (increased or decreased) in the last 30 years, and the trends showed a strong positive correlation with the rainfall, while showed a negative correlation with evaporation, the influence of human activities to the small lake area was not significant, the lake area tended to shrink as time goes by, which was mainly attributed to the drying climate;②The lakes area in the year of t showed a strong correlation with the lake area of previous year, precipitation, and evaporation in the year of t, which can be simulated with the linear equations and nonlinear equations; ③the typical research area-the Wang Bahaga Lake, showed to be decreased during 1986-2013, but there were both atrophied and expanded in different directions: the I, II, V, VI region atrophied, while other regions expanded, the II, III, IV, VIII were dominant mutation direction, followed by the direction of VI, the other direction changed slowly. The region was marked as Ⅰ-Ⅷ by dividing the lake with every 45°, starting from north, clockwise. The results not only provided the technical support for the healthy maintain of Horqin sandy land ecosystem, but also could be a guidance for other similar lake areas.

Key words:  Horqin Sandy Land      meadow dunes area      remote sensing      lake evolution      impact analysis     
Received:  02 March 2014      Published:  20 May 2015
ZTFLH:  TV882.9  

Cite this article: 

Jia Ke, Liu Tingxi, Lei Huimin, Duan Limin, Luo Yanyun, Zhang Shengwei, Tong Xin, Sun Li. Lake Evolution and Effect Analysis of Meadow-dunes Area in the Horqin Sandy Land in 1986-2013. JOURNAL OF DESERT RESEARCH, 2015, 35(3): 783-791.

URL: 

http://www.desert.ac.cn/EN/10.7522/j.issn.1000-694X.2014.00043     OR     http://www.desert.ac.cn/EN/Y2015/V35/I3/783

[1] 胡汝骥, 姜逢清, 王亚俊, 等.论中国干旱区湖泊研究的重要意义[J].干旱区研究, 2007, 24(2):137-140.
[2] 丁永建, 刘时银, 叶柏生, 等.近50 a中国寒区与旱区湖泊变化的气候因素分析[J].冰川冻土, 2006, 28(5):623-632.
[3] 熊波, 陈学华, 宋孟强, 等.基于RS和GIS的沙漠湖泊动态变化研究--以巴丹吉林沙漠为例[J].干旱区资源与环境, 2009, 23(8):91-98.
[4] 朱震达, 吴正, 刘恕, 等.中国沙漠概论[M].北京:科学出版社, 1980:73-76.
[5] Yong X P, Liu T S, Xiao H L.Evolution of megadunes and lakes in the Badain Jaran Desert, Inner Mongolia, China during the last 31 000 years[J].Quaternary International, 2003, 10(4):99-112.
[6] 张振瑜, 王乃昂.近40 a巴丹吉林沙漠腹地湖泊面积变化及其影响因素[J].中国沙漠, 2012, 32(6):1743-1750.
[7] 马龙, 吴敬禄.近50年来内蒙古河套平原气候及湖泊环境演变[J].干旱区研究, 2010, 27(6):871-878.
[8] 许诗, 刘志明.1986-2008年吉林省湖泊变化及驱动力分析[J].湖泊科学, 2010, 22(6):901-909.
[9] 于瑞宏, 许有鹏, 刘廷玺, 等.应用多光谱遥感信息反演干旱区浅水湖泊水深[J].水科学进展, 2009, 20(1):111-118.
[10] 拉巴.拉巴卓玛, 陈涛, 等.基于MODIS影像的西藏典型内陆湖泊变化研究及成因分析[J].气象与环境科学, 2011, 34(3):37-41.
[11] 万玮, 肖鹏峰, 冯学智, 等.近30年来青藏高原羌塘地区东南部湖泊变化遥感分析[J].湖泊科学, 2010, (6): 874-881.
[12] 张振瑜, 王乃昂, 马宁, 等.近40 a巴丹吉林沙漠腹地湖泊面积变化及影响因素[J].中国沙漠, 2012, 32(6):1743-1750.
[13] 许诗, 刘志明, 王宗明, 等.1986-2008年吉林省湖泊变化及驱动力分析[J].湖泊科学, 2010, 22(6):901-909.
[14] 边多, 边巴次仁, 拉巴, 等.1975-2008年西藏色林错湖泊面积变化对气候变化的响应[J].地理学报, 2010, 65(3):313-319.
[15] Bai J, Chen X, Yang L, et al.Monitoring variations of inland lakes in the arid region of Central Asia[J].Frontiers of EarthScience in China, 2012, 6(2):147-156.
[16] 周哲, 杨小平.近30年来内蒙古东部达赉诺尔湖泊地区沙漠化与湿地演变初探[J].第四纪研究, 2004, 24(6):679-2004.
[17] 弋双文, 鹿化煜, 曾琳, 等.末期盛冰期以来科尔沁沙地古气候变化及其边界重建[J].第四纪研究, 2013, 33(2):206-218.
[18] 白洁, 陈曦, 杨均力, 等.1975-2007年中亚干旱区内陆湖泊面积变化遥感分析[J].湖泊科学, 2011, 23(1):80-88.
[19] 王志辉, 易善桢.不同指数模型法在水体遥感提取中的比较研究[J].科学技术与工程, 2007, 7(4):534-538.
[20] McFeeters S K.The use of normalized difference water index (NDWI) in the delineation of open water features[J].International Journal of Remote Sensing, 1996, 17(7):1425-1432.
[21] 董芳.基于陆地卫星TM/ETM+和GIS的济南城区扩展动态监测研究[D].山东泰安:山东农业大学, 2003.
[22] 蒋德明, 刘志民.科尔沁沙地生态环境及其可持续管理--科尔沁沙地生态考察报告[J].生态学杂志, 2004, 23(5):179-185.
[23] 曾德慧, 姜凤岐.整治"三滥"是从源头遏制生态脆弱地区土地荒漠化的必由之路--以科尔沁沙地为例[J].生态学杂志, 2006, 25(12):1540-1543.
[24] 常学礼, 赵学勇, 王玮, 等.科尔沁沙地湖泊消涨对气候变化的响应[J].生态学报, 2013, 33(21):7002-7012.
No Suggested Reading articles found!