基于MODIS的和田河夏季漫流监测分析

干旱区研究 ›› 2011, Vol. 28 ›› Issue (3): 438-443.

基于MODIS的和田河夏季漫流监测分析

左敏¹, 陈洪武^1,2, 王蕾², 冯志敏², 王海雷¹

1. 新疆大学资源与环境科学学院, 新疆乌鲁木齐 830046;
2. 新疆维吾尔自治区气候中心, 新疆乌鲁木齐 830002

收稿日期:2010-06-04 修回日期:2010-08-02 出版日期:2011-06-25 发布日期:2011-09-06
作者简介:左敏(1984-),女,河南周口人,在读硕士,从事资源与环境研究.E-mail:fzm_20000@sina.com
基金资助:
国家科技支撑计划课题"我国主要极端天气气候事件及重大气象灾害的监测、检测和预测关键技术研究(2007BAC29B02)"与"和田河河道及分流水体卫星遥感调查"项目资助

Monitoring and Analysis on Overflow in the Hotan River Basin Based on MODIS Data

ZUO Min¹, CHEN Hong-wu^1,2, WANG Lei², FENG Zhi-min², WANG Hai-lei¹

1. College of Resources and Environmental Sciences, Xinjiang University, Urumqi 830046, China;
2. Xinjiang Climate Center, Urumqi 830002, China

Received:2010-06-04 Revised:2010-08-02 Online:2011-06-25 Published:2011-09-06

摘要/Abstract

摘要： 在ENVI中采用目视解译和监督分类相结合的方法,以及ArcGIS的定位、量测、图层叠加,对和田河中下游夏季漫流状况进行监测分析。结果表明:① 和田河中下游漫流已经到了相当严重的程度。② 中游绿洲边缘和其他河段相比漫流较少,94.4%的监测日期内漫流面积均在35 km²以下,45%的监测日期里没有漫流痕迹。两河交汇处科什米什至古河道与和田河的交汇处,45%的监测日期内漫流面积均在35 km²以上,只有2004年8月5日和2008年7月29日的监测面积为0。古河道与和田河的交汇点至肖塔水文站漫流最严重,大部分监测日期都在 70 km²以上,最大的达到111 km²。③ 全流域共有漫流点10处,其中和田河主河道段左侧有4处,1个新增水域漫滩,右侧出现4处,1个新增水域漫滩;喀拉喀什河左侧出现1处。漫流主要发生于主河道上。

关键词: MODIS, 夏季, 漫流面积, 外溢水域, 监测分析, 和田河

Abstract: In this paper, the overflow in the middle and lower reaches of the Hotan River in summer was monitored and analyzed using the visual interpretation, supervised classification in ENVI 4.5 and functions of localization, measurement and layer overlay of ArcGIS 9.2. The results are as follows: (1) The overflow in the middle and lower reaches of the Hotan River was very serious, and the overflow in the irrigated areas in oasis should also be paid attention to; (2) Compared with other river sections, the overflow in the marginal zone of the oasis in the middle reaches was low, the overflow area was smaller than 35 km² at 94.4% monitoring dates, and there was no overflow at 45% monitoring dates. At the intersection of the section from Keshen Mishen to the old river channel and the Hotan River, the overflow areas were all larger than 35 km² at 45% monitoring dates except that there was no overflow on August 5, 2004 and July 29, 2008. Overflow along the river section from the intersection of the old river channel and the Hotan River to Xiaota was the most serious, the overflow area was larger than 70 km² in the most cases and 111 km² in maximum; (3) There were 10 overflow sites in total in the drainage basin, in which 4 overflow sites and 1 new floodplain were distributed along the left riverbank of the Hotan River, and 4 overflow sites and 1 new floodplain were distributed along the right one; there was also a overflow site on the left riverbank of the Karakax River. The overflow sites were mainly distributed along the mainstream of the Hotan River.

Key words: MODIS, summer, overflow, floodplain, monitoring and analyzing, Hotan River

中图分类号:

P343.1

左敏, 陈洪武, 王蕾, 冯志敏, 王海雷. 基于MODIS的和田河夏季漫流监测分析[J]. 干旱区研究, 2011, 28(3): 438-443.

ZUO Min, CHEN Hong-wu, WANG Lei, FENG Zhi-min, WANG Hai-lei. Monitoring and Analysis on Overflow in the Hotan River Basin Based on MODIS Data[J]. , 2011, 28(3): 438-443.

参考文献

[1] 蒋艳,夏军.塔里木河流域径流变化特征及其对气候变化的响应[J].资源科学,2007,29(3):45-52.[Jiang Yan,Xia Jun.The hydrological characteristics of runoff and its response to climatic change in Tarim[J].Resources Science,2007,29(3):45-52.]

[2] 傅丽昕.近50年塔里木河源流区气候变化及其对径流量的影响[D].乌鲁木齐:新疆农业大学,2008.[Fu Lixin.The Climatic Change and Its Influence on the Runoff in the Past 50 Years in the Three Water Resources of the Tarim River[D].Urumqi: Xinjiang Agricultural University,2008.]

[3] 刘海涛,张向军,李绣东,等.和田河流域1954-2007年气温及降水气候特征分析[J].沙漠与绿洲气象,2009,3(4):25-29.[Liu Haitao,Zhang Xiangjun,Li Xiudong,et al.Climatic characteristics of temperature and precipitation in Hetian River Basin during 1954-2007[J].Desert and Oasis Meteorology,2009,3(4):25-29.]

[4] 黄领梅,沈冰,宋孝玉,等.和田河流域地表径流变化分析[J].沈阳农业大学学报,2004,35(5/6):513-515.[Huang Lingmei,Shen Bing,Song Xiaoyu,et al.Characteristics of surface water resources in Hetan River Basin[J].Journal of Shenyang Agricultural University,2004,35(5/6):513-515.]

[5] 胡顺福.和田河流域水文特征及区域水资源评价[J].干旱区研究,1991,8(2):61-70.[Hu Shunfu.Hydrologica1 characteristics and rgiona1 water resources assessment in Hetian River Basin[J].Arid Zone Research,1991,8(2):61-70.]

[6] 张晓伟,沈冰,黄领梅.和田河年径流变化规律研究[J].自然资源学报,2007,22(6):975-979.[Zhang Xiaowei,Shen Bing,Huang Lingmei.Study on the variation law of the annual runoff in Hetian River[J].Journal of Natural Resources,2007,22(6):975-979.]

[7] 龚岸桥.和田河肖塔站水沙特性及水位流量关系的初步研究[J].塔里木农垦大学学报,1997,9(2):15-20.[Gong Anqiao.Studies on properties of sediment and the relation between water level and flow of Xiaota hydrologic station of the Hetian River[J].Journal of Talimu University Agricultural Reclamation,1997,9(2):15-20.]

[8] 黄领梅,沈冰.和田河地表径流动态变化趋势分析[J].水土保持学报,2000,14(6):84-87.[Huang Lingmei,Shen Bing.Analysis of the dynamic change trend of surface runoff in Hetian River Basin[J].Journal of Soiland Water Conservation,2000,14(6):84-87.]

[9] 陈亚宁,郝兴明,徐长春.新疆塔里木河流域径流变化趋势分析[J].自然科学进展,2007,20(2):205-207.[Chen Yaning,Hao Xingming,Xu Changchun.Analysis of runoff change trend of the Tarim River Basin in Xinjiang[J].Progress in Natural Science,2007,20(2):205-207.]

[10] 吴益.和田河流域径流过程分析与模拟[D].南京:河海大学,2006.[Wu Yi.Analysis and Simulation of Runoff Process of the Hetian River[D].Nanjing:Hehai University,2006.]

[11] 黄领梅,沈冰,莫淑红,等.新疆和田河年径流量变化的定量估算[J].西安理工大学学报,2005,21(3):289-292.[Huang Lingmei,Shen Bing,Mo Shuhong,et al.Quantitative estimation of annual runoff variation from the Hetian River in Xinjiang[J].Journal of X[i'an University of Technology,2005,21(3):289-292.]

[12] 王让会,樊自立.遥感和地理信息系统在塔里木河流域洪水监测中的应用[M].北京:中国环境科学出版社,1998:109-113.[Wang Ranghui,Fan Zili.Applatiom of RS and GIS to Floor Monitoring in the Tarim River Basin[M].Beijing: China Environmental Science Press,1998:109-113.]

[13] 王学全,高前兆.塔克拉玛干沙漠降水入渗和径流补给试验观测[J].干早区资源与环境,1998,12(4): 112-118.[Wang Xuequan,Gao Qianzhao.The precipitation infltration and runoff recharging experment observation in the Taklmakan Desert[J].Journal of Arid Land Resources and Environment,1998,12(4):112-118.]

[14] 樊自立,马映军.干旱区水资源开发及合理利用的几个问题[J].干旱区研究,2000,17(3):6-11.[Fan Zili,Ma Yingjun.Some issues about the exploitation and rational utilization of water resources in the arid areas[J].Arid Zone Research,2000,17(3):6-11.]

[15] 刘腊山,黄骁勇.新疆和田河流域节水改造工程实施的生态环境效应初步分析[J].水利学报,2005(增刊):478-480.[Liu Lashan,Huang Xiaoyong.Preliminary analysis of eco-environmental effect since project of water-saved Hetian River Basin[J].Journal of Hydraulic Engineering,2005(Suppl.):478-480.]

[16] 郑仰奇.和田河流域水资源保护规划研究[D].西安:西安理工大学,2005.[Zheng Yangqi.Study on Water Resources Protection Planning of Hetian River Basin[D].X[i'an:X[i'an University of Technology,2005.]

[17] 饶瑞符.塔里木河的变迁与整治[M].北京:中国环境科学出版社,1998:184-193.[Rao Rifu.Vicissitudes and Renovating of the Tarim River[M].Beijing: China Environmental Science Press,1998:184-193.]

[18] 宋郁东,樊自立,雷志栋,等.中国塔里木河水资源与生态问题研究[M].乌鲁木齐:新疆人民出版社,2000.[Song Yudong,Fan Zili,Lei Zhidong,et al.Study on Water Resource and Ecological Issue of the Tarim River in China[M].Urumqi:Xinjiang Peopl[e's Publishing House,2000.