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Monitoring decadal lake dynamics across the Yangtze Basin downstream of Three Gorges Dam

机译:监测三峡大坝下游长江流域的十年湖泊动力学

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The Yangtze River Basin downstream of China's Three Gorges Dam (TGD) (thereafter referred to as "downstream" basin) hosts the largest cluster of freshwater lakes in East Asia. These lakes are crucial water stocks to local biophysical environments and socioeconomic development. Existing studies document that individual lakes in this region have recently experienced dramatic changes under the context of enduring meteorological drought, continuous population growth, and extensive water regulation since TGD's initial impoundment (i.e., June, 2003). However, spatial and temporal patterns of lake dynamics across the complete downstream Yangtze basin remain poorly characterized. Using dailyMODIS imagery and an advanced thematic mapping scheme, this study presents a comprehensive monitoring of area dynamics in the downstream lake system at a 10-day temporal resolution during 2000-2011. The studied lakes constitute ~76% (~11,400 km~2) of the total downstream lake area, including the entire +70 major lakes larger than 20 km~2. The results reveal a decadal net decline in lake inundation area across the downstream Yangtze Basin, with a cumulative decrease of 849 km~2 or 7.4% from2000 to 2011. Despite an excessive precipitation anomaly in the year 2010, the decreasing trendwas tested significant in all seasons. The most substantial decrease in the post-TGD period appears in fall (1.1% yr~(-1)),which intriguingly coincideswith the TGDwater storage season. Regional lake dynamics exhibit contrasting spatial patterns, manifested as evident decrease and increase of aggregated lake areas respectively within and beyond the Yangtze Plain. This contrast suggests a marked vulnerability of lakes in the Yangtze Plain, to not only local meteorological variability but also intensified human water regulations from both the upstream Yangtze main stem (e.g., the TGD) and tributaries (e.g., lakes/reservoirs beyond the Yangtze Plain). The produced lakemapping result and derived lake area dynamics across the downstream Yangtze Basin provides a crucial monitoring basis for continuous investigations of changing mechanisms in the Yangtze lake system.
机译:中国三峡大坝(TGD)下游的长江流域(以下简称“下游”流域)拥有东亚最大的淡水湖泊群。这些湖泊是当地生物物理环境和社会经济发展的关键水库。现有研究表明,自TGD最初蓄水以来(即2003年6月),该地区的各个湖泊最近在持久的气象干旱,人口持续增长和广泛的水调节条件下经历了巨大变化。但是,整个长江下游流域的湖泊动力学的时空格局仍然缺乏很好的特征。利用DailyMODIS影像和先进的专题制图方案,本研究以10天的时间分辨率在2000-2011年期间全面监测了下游湖泊系统中的区域动态。所研究的湖泊约占下游湖泊总面积的76%(〜11,400 km〜2),包括整个大于70 km〜2的+70个主要湖泊。结果表明,长江流域下游湖泊淹没区的年代际净减少量,从2000年到2011年累计减少了849 km〜2或7.4%。尽管在2010年出现了异常的降水异常,但下降趋势在所有地区都得到了检验。季节。 TGD后时期最大的下降出现在秋季(1.1%yr〜(-1)),这与TGD的蓄水季节恰好吻合。区域湖泊动力学表现出相反的空间格局,表现为长江平原以内和以外地区聚集湖面积的明显减少和增加。这种对比表明,长江平原的湖泊不仅容易受到当地气象变化的影响,而且长江上游主干(例如TGD)和支流(例如长江平原以外的湖泊/水库)的人类水调节强度也大大增强。 )。长江下游地区产生的湖泊测绘结果和导出的湖泊面积动态为连续研究长江湖泊系统变化机制提供了至关重要的监测基础。

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