同奈河流域上游水量平衡变化

H. Pham, L. P. Vo, V. T. Le, P. Olivier
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引用次数: 2

摘要

近几十年来,社会经济发展导致的土地利用和土地覆盖(LULC)变化,加上气候变化,严重破坏和损害了东奈河上游流域的环境可持续性。评估气候变化和LULC变化对UPDN流域水文条件和水平衡的长期影响对流域可持续管理至关重要。利用Landsat影像和SWAT (Soil and Water Assessment Tool)模型,在1994年、2004年和2014年3个不同的时间间隔评估了气候和LULC变化导致的水资源平衡变化。Landsat影像分类结果表明,林地是该流域主要的土地利用变化类型。1994年森林覆盖面积为706,803公顷(占总陆地面积的72.68%)。2004年,森林面积下降到520,359公顷(53.51%)。2014年,森林面积进一步减少到485908公顷(49.97%)。LULC的变化引起了年流量和峰值流量的变化。分析结果表明,历史气候变化对产水量的影响大于LULC变化。在LULC 2014情景下,灌溉用水量最高,且主要发生在旱季。研究结果可为决策者规划和制定可持续流域管理和气候变化适应政策提供有用信息。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Water balance changes in the upper part of Dong Nai River basin
In recent decades, changes in land use and land cover (LULC) arising from socio-economic development, coupled with climate change, have severely undermined and compromised the environmental sustainability of the upper part of Dong Nai (UPDN) river basin. Assessing the long-term impacts of climate change and changes in LULC on hydrological conditions and water balance in the UPDN river basin is essential for sustainable watershed management. In the present study, Landsat images and SWAT (Soil and Water Assessment Tool) model were used to assess water balance changes due to changes of climate and LULC at three different intervals: 1994, 2004, and 2014. The results of Landsat images classification indicated that forest land was the main LULC type in the basin. In 1994 the forest cover was 706,803 ha (72.68% of the total landmass). In 2004 the forest area dropped to 520,359 ha (53.51%). In 2014 the forest area dropped further to 485,908 ha (49.97%). The change in LULC has caused changes in the annual and peak water flows. The analysis of the results revealed that the effect of historical climate variations on water yield was greater than the LULC change. With the scenario of LULC 2014, the consumption of irrigation water was the highest and mainly in the dry season. The findings can provide useful information for decision-makers in planning and formulating policies for sustainable watershed management and climate change adaptation.
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