首页> 外文会议>American Society for Photogrammetry and Remote Sensing Annual Conference >THE LONG-TERM HYDROLOGICAL IMPACT ASSESSMENT OF LAND USE AND LAND COVER CHANGES USING L-THIA MODEL IN THE QINHUAI RIVER WATERSHED OF JIANGSU PROVINCE, CHINA
【24h】

THE LONG-TERM HYDROLOGICAL IMPACT ASSESSMENT OF LAND USE AND LAND COVER CHANGES USING L-THIA MODEL IN THE QINHUAI RIVER WATERSHED OF JIANGSU PROVINCE, CHINA

机译:利用江苏省秦淮河流域的L-THIA模型改变土地利用和土地利用的长期水文影响评价

获取原文

摘要

This study examined the effects of land use and land cover changes due to urbanization on the annual direct runoff of the Qinhuai River Watershed in Jiangsu Province, China. Landsat Thematic Mapper (TM) images from 1988, 1994, 2006, Enhanced Thematic Mapper Plus (ETM+) images from 2001 and 2003, and China-Brazil Earth Resources Satellite (CBERS) image from 2009 were used to obtain historical land use and land cover maps. These maps revealed that the watershed experienced conversion of approximately 16% non-urban area to urban area between 1988 and 2009. The Long-Term Hydrological Impact Assessment (L-THIA) model was used to calculate direct runoff generation. The model was calibrated and validated using observed daily stream flow data collected at the outlets of the watershed, and then repeatedly run with different urbanization scenarios to investigate the hydrological response to land use changes. The simulation results of L-THIA model for the various urbanization scenarios indicate that when the impervious surface area changed from 3.4% of 1988 scenario to 20.5% of 2009 scenario, the average annual direct runoff depth would increase from 355 mm to 496 mm. The results also indicate that the annual direct runoff depth is highly correlated with the percentage of impervious surface area. When impervious surface area is less than 9.0%, the annual direct runoff depth will increase linearly with impervious surface area (R~2=0.97); however, when impervious surface area is greater than 9.0%, the annual direct runoff depth will also increase linearly with impervious surface area (R~2 = 1.00) but at much lower rate.
机译:本研究土地利用和土地覆盖变化的影响,由于对秦淮河流域的江苏省,中国每年直接径流城市化。陆地卫星专题制图仪(TM)1988年,1994年,2006年,增强型专题制图仪(ETM +),从2001年和2003年,和中国巴西地球资源卫星(CBERS)从2009年的图像图像被用来获得历史上土地利用和土地覆盖的图像地图。这些地图显示,约16%的非城市地区向城市地区1988年和2009年长期水文影响评估(L-THIA)模型之间的分水岭经验的转化率来计算直接径流的产生。该模型进行校准,并使用在流域的出口收集每日观察流流量数据验证,然后反复用不同的城市化的方案运行,以调查对土地利用变化的水文响应。 L-THIA模型的用于各种城市化方案的模拟结果表明,当不透表面积从1988情形的3.4%变化到2009情形的20.5%,平均每年的直接径流深度将增加从355毫米496毫米。研究结果还表明,每年直接径流深是高度不透水地面面积的比例呈正相关。当不透水表面面积小于9.0%时,每年的直接径流深度将不透表面积增加而线性增加(R〜2 = 0.97);然而,当不透表面积是大于9.0%时,每年的直接径流深度也将线性地不透水表面积(R〜2 = 1.00),但在低得多的速率增加。

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