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土地利用与土地覆盖动态变化及其对水文响应的影响:以埃塞俄比亚北部高地的吉尔盖尔·特克泽集水区为例

Dynamics of land use and land cover and its effects on hydrologic responses: case study of the Gilgel Tekeze catchment in the highlands of Northern Ethiopia.

作者信息

Haregeweyn Nigussie, Tesfaye Samuel, Tsunekawa Atsushi, Tsubo Mitsuru, Meshesha Derege Tsegaye, Adgo Enyew, Elias Asres

机构信息

Arid Land Research Center, Tottori University, 1390 Hamasaka, Tottori, 680-0001, Japan,

出版信息

Environ Monit Assess. 2015 Jan;187(1):4090. doi: 10.1007/s10661-014-4090-1. Epub 2014 Nov 19.

DOI:10.1007/s10661-014-4090-1
PMID:25407989
Abstract

Unprecedented land use and land cover (LULC) changes in the Gilgel Tekeze catchment of the upper Nile River basin in Ethiopia may have far-reaching consequences for the long-term sustainability of the natural resources base. This study analyzed the dynamics and hydrologic effects of LULC changes between 1976 and 2003 as shown in satellite imagery. The effects of these LULC changes on the hydrologic response were investigated using the WetSpa model to estimate spatially distributed average annual evapotranspiration, surface runoff, and groundwater recharge. Digital image analysis revealed major increments of cultivated land and settlements of 15.4 and 9.9%, respectively, at the expense of shrubland and grazing lands. Population growth and the associated demand for land were found to be the major driving forces. The WetSpa simulation showed an increase in annual surface runoff of 101 mm and a decrease in groundwater recharge of 39 mm over the period 1976-2003. These results signify an increasing threat of moisture unavailability in the study area and suggest that appropriate land management measures under the framework of the integrated catchment management (ICM) approach are urgently needed.

摘要

埃塞俄比亚尼罗河上游流域吉尔盖尔·特克泽集水区前所未有的土地利用和土地覆盖(LULC)变化,可能会对自然资源基础的长期可持续性产生深远影响。本研究分析了1976年至2003年间卫星图像所示的LULC变化动态及其水文效应。利用WetSpa模型研究了这些LULC变化对水文响应的影响,以估算空间分布的年均蒸散量、地表径流和地下水补给量。数字图像分析显示,耕地和居民点分别大幅增加了15.4%和9.9%,代价是灌木林和牧场面积减少。研究发现人口增长及相关的土地需求是主要驱动力。WetSpa模拟显示,1976年至2003年期间,年地表径流量增加了101毫米,地下水补给量减少了39毫米。这些结果表明研究区域内水分供应不足的威胁日益增加,并表明迫切需要在综合流域管理(ICM)方法框架下采取适当的土地管理措施。

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