蒙古国地表水体长期变化及其影响

Long-term changes in water bodies and their relevant impacts in Mongolia

  • 摘要: 地表水体是地球生态系统的重要组成部分, 干旱区地表水体对气候变化反映尤其敏感, 其变化能够直接或间接影响区域生态安全及社会经济发展。为深入探讨蒙古国水体变化的时空规律, 本文基于Google Earth Engine平台和Landsat遥感影像数据, 提取建立了1990—2023年地表水体数据集, 在验证新建数据集可靠性的基础上, 分析了30多年来水体变化趋势及成因。结果表明, 从时间序列上看, 水体变化呈先减少后增加的趋势; 不同大小水体类型间存在明显差异, 其中, 小型水体(1~10 km²)以及过去研究相对不足的微小水体(≤1 km²)在数量和面积上波动幅度最大, 中大型水体变化较为平稳; 从空间分布来看, 与中国接壤的干旱沙漠及戈壁区(如东南戈壁流域和杭爱山脉谷地流域)水体变化更加剧烈, 对气候的年际变化敏感; 气候因素特别是降水、年均降水与蒸散之差、标准化降水指数(SPI)和标准化降水蒸散指数(SPEI), 能够准确反映干旱和湿润交替对水体数量和面积变化的影响。此外, 年耕地面积和牲畜数量与水体特别是微小水体有相似的变化趋势, 表明水体数量减少潜在影响游牧型畜牧业的用水保障, 并通过影响灌溉和改变土壤墒情间接影响农作物种植结构与规模。

     

    Abstract: Surface water bodies play a vital role in maintaining the ecological balance and supporting socioeconomic development, particularly in arid and semi-arid regions such as Mongolia. These regions are particularly sensitive to climate change, and variations in surface water can have far-reaching implications for environmental security and human livelihood. To better understand the spatiotemporal dynamics and driving mechanisms of water body changes in Mongolia, this study constructed a comprehensive and continuous dataset of surface water bodies from 1990 to 2023 using Landsat satellite imagery. Dataset reliability was thoroughly validated, and subsequent analysis were conducted to reveal long-term trends and patterns in water body changes across different size categories. Temporally, the results indicated a pronounced decline in surface water bodies prior to 2009, followed by a gradual recovery trend thereafter. Notably, small water bodies (1–10 km2) and micro water bodies (<1 km²) experienced the most dramatic changes, with frequent appearances and disappearances. These micro water bodies have historically received limited research attention, despite their ecological significance. In contrast, medium and large water bodies exhibited relatively stable transformations. Spatial analysis revealed that regions located in desert and Gobi environments (such as the Southeast Gobi and Hangay Uul Valley basins), demonstrated heightened sensitivity to climate variations. These areas experienced the most substantial changes in water body distribution. Climatic variables such as precipitation and evapotranspiration, represented by the standardized precipitation index (SPI) and standardized precipitation evapotranspiration index (SPEI), were found to be strongly correlated with the number and area of water body. These indices effectively captured the impact of Mongolia’s wet–dry–wet climatic cycles on surface water availability. Moreover, land use and socioeconomic indicators such as annual arable land area and livestock number showed fluctuation patterns similar to those of water bodies, particularly micro water bodies. This suggests a potential link between surface water loss, decreased pasture quality, and rain-fed agricultural capacity. These findings highlight the ecological importance of small and micro water bodies, which deserve greater attention in future research and water resource management strategies aimed at promoting sustainable development in Mongolia’s fragile environment.

     

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