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环渤海地区土地利用的时空变化分析
引用本文:朱会义,李秀彬,何书金,张明.环渤海地区土地利用的时空变化分析[J].地理学报,2001,11(3):253-260.
作者姓名:朱会义  李秀彬  何书金  张明
作者单位:中国科学院地理科学与资源研究所
基金项目:国家自然科学重点基金项目!( 49831 0 2 0 )&&
摘    要:根据1985和1995年2期TM影像资料,运用遥感影像机助解译方法、地理信息系统空间分析方法以及数理统计方法,全面分析了环渤海地区3省2市1985-1995年间分类土地利用的数量变化和空间变化特征,揭示了该区各类土地利用数量变化的幅度、速度和区域差异以及土地利用空间变化的主要类型、分布特征和区域方向,阐明了该区土地利用变化的区域特点,为土地可持续利用提供有效的决策支持。

关 键 词:环渤海地区  土地利用  时空变化  遥感影像  地理信息系统
文章编号:0375-5444(2001)03-0253-08
收稿时间:2001-02-20
修稿时间:1/2/2001 12:00:00 AM

Sand-dust storms in China: temporal-spatial distribution and tracks of source lands
QIU Xin-fa,ZENG Yan,MIAO Qi-long.Sand-dust storms in China: temporal-spatial distribution and tracks of source lands[J].Acta Geographica Sinica,2001,11(3):253-260.
Authors:QIU Xin-fa  ZENG Yan  MIAO Qi-long
Institution:1. Urban &;|Resource Department, Nanjing University, Nanjing 210009, China| 2. Department of Environmental Science, Nanjing Institute of Meteorology, Nanjing 210044, China
Abstract:Sand-dust storm is a special natural disaster that frequently occurs in deserts and their surrounding areas. With the data published on Surface Meteorological Monthly Bulletin and Surface Chart during 1971-1996, the temporal-spatial distribution and annual variation of sand-dust storms are analyzed on the basis of the case study of atmospheric processes. Furthermore, the tracks and source areas of sand-dust storms are determined with the aid of GIS. The results show that except some parts of Qinghai Province and Inner Mongolia as well as Beijing, sand-dust storms decrease apparently in time and space in recent decades in China. Sand-dust storms occur most frequently in spring, especially in April. According to their source areas, sand-dust storms are classified into two types, i.e., the inner-source and outer-source sand-dust storms. Most of the outer-source sand-dust storms move along the north and west tracks. The north-track outer-source sand-dust storms always intrude into China across the Sino-Mongolian border from Hami, a city in the eastern part of Xinjiang, to Xilin Gol, a league in Inner Mongolia, while the west-track ones intrude into China from both southern and northern Xinjiang. The source lands of inner-source sand-dust storms concentrate in the Taklimakan Desert and its surrounding areas in southern Xinjiang, southern part of the Junggar Basin in north of Xinjiang, the Hexi Corridor in western Gansu Province, the dry deserts of Inner Mongolia and the Qaidam Basin in Qinghai.
Keywords:the Bohai Rim  land use change  spatio  temporal analysis
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