首页> 外文会议>Conference on Earth Resources and Environmental Remote Sensing/GIS Applications >Spatial and temporal characteristics of aridity conditions in Tarim Basin, China
【24h】

Spatial and temporal characteristics of aridity conditions in Tarim Basin, China

机译:塔里木盆地干旱条件的时空特征

获取原文

摘要

Arid ecosystems are very sensitive to a variety of physical, chemical and biological degradation processes. Tarim Basin, the biggest endorheic basin in the Central Asia continent, is considered as one of the least water-endowed regions in the world and arid and semi-arid environmental conditions are dominant. For the purposes of the convention, arid, semi-arid and dry sub-humid areas were defined as 'areas, other than polar and sub-polar regions, in which the ratio of annual precipitation to potential evapotranspiration falls within the range from 0.05 to 0.65.' In this study, the Aridity Index (AI), the ratio of precipitation and land surface temperature, was also adopted as the base method for determining dry land types and thereby delineating boundaries and showing changes of aridity conditions in Tarim Basin. Here, precipitation is from TRMM/PR, and land surface temperature is from Modis LST. To analyze the spatial and temporal variations of arid environmental conditions in Tarim basin, we calculated the yearly aridity index (the ratio of total yearly rainfall to yearly mean Land Surface Temperature) based on the accumulated monthly precipitation and the monthly Land Surface Temperature in growing season for the period 2000-2009. The results indicated it is possible to work out an aridity index map with more detailed spatial patterns, which is valuable for identifying human impacts by associated with vegetation and soil moisture characters.
机译:干旱的生态系统对各种物理,化学和生物降解过程非常敏感。塔里木盆地是中亚大陆最大的背胶盆地,被认为是世界上水资源匮乏的地区之一,干旱和半干旱的环境条件占主导地位。为了该公约的目的,干旱,半干旱和干燥的半湿润地区被定义为“极地和亚极地地区以外的地区”,其中年降水量与潜在蒸散量之比在0.05至0.65。”在这项研究中,干旱指数(AI),即降水与地表温度的比率,也被用作确定干旱土地类型的基本方法,从而勾勒出边界并显示了塔里木盆地的干旱条件的变化。在这里,降水来自TRMM / PR,而地表温度则来自Modis LST。为了分析塔里木盆地干旱环境条件的时空变化,我们基于累积的月降水量和生长季节的月地面温度,计算了年干旱指数(年降水总量与年平均地表温度之比)。 2000-2009年期间。结果表明,有可能制定出具有更详细空间模式的干旱指数图,这对于与植被和土壤水分特征相关联的人为影响识别具有重要意义。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号