京津冀2000-2021年地表水面积时空变化与影响因素分析
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1.天津师范大学 京津冀生态文明发展研究院;2.河北省海洋岸线生态修复与智慧海洋监测工程研究中心

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中图分类号:

X87

基金项目:

河北省海洋岸线生态修复与智慧海洋监测工程研究中心开放基金(53H23039)


Spatial-temporal variation and influencing factors of surface water area in Beijing-Tianjin-Hebei Region from 2000 to 2021
Author:
Affiliation:

Beijing-tianjin-hebei Ecological Civilization Development Institute, Tianjin Normal University

Fund Project:

Hebei Province Marine Shoreline Ecological Restoration and Smart Ocean Monitoring Engineering Research Center Open Fund (53H23039)

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    摘要:

    [目的]京津冀地区面临水资源短缺、水生态环境退化严重等问题,因此推动京津冀地区水资源系统的高质量发展,对于区域发展和国家战略的实施具有着重要的实际意义。[方法]利用JRC全球地表水产品数据集提取2000-2021年京津冀各市不同类型的地表水,分析京津冀各市近22a地表水面积时空变化趋势,利用形态学空间格局分析模型(MSPA)分析典型区域白洋淀、七里海湿地的地表水空间形态演变,结合气候和人类活动数据,采用相关性分析法,阐明不同城市地表水时空变化的驱动机制。[结果](1)从时间上看,近22a京津冀永久性水体面积整体呈下降趋势,而季节性水体面积整体呈增长趋势。从空间上看,地表水面积动态度减少的重心区域主要集中在都市圈北京、天津、廊坊等城市,而南北方向上南水北调中线沿线城市邯郸市、邢台市、石家庄市等城市地表水面积动态度呈现增加趋势。(2)近22a来白洋淀核心湿地地表水面积有一个下降和上升过程,在2000-2005年间逐渐减少,在2005年后开始逐渐增加,而边缘湿地逐年增加。七里海的核心湿地、边缘湿地和桥接湿地面积在2000-2010年逐年减少,2010年后开始恢复。(3)京津冀南部城市最大水体面积与降水量呈正相关,而东部沿海城市呈负相关。反映出人类活动与自然补给之间的不平衡性。北京市、承德市、唐山市的用水量与最大地表水面积之间存在显著正相关,显示跨流域调水和生态补水的影响较大。而秦皇岛市、天津市则表现为显著负相关和极显著负相关,显示地下水超采对地表水资源有着负面影响。[结论]研究揭示近22a京津冀地表水面积变化,为实现水资源的可持续发展提供参考。

    Abstract:

    [Objective] The Beijing-Tianjin-Hebei region confronts critical challenges, including water resource scarcity and ecological degradation. Advancing the sophisticated development of the water resources system is pivotal for regional progress and aligns with national strategic objectives. [Methods] This study utilized the JRC global surface water dataset to identify surface water variations in Beijing, Tianjin, and Hebei from 2000 to 2021. We examined the spatial-temporal trends of surface water and the morphological evolution within Baiyangdian and Qilihai wetlands using the Morphological Spatial Pattern Analysis (MSPA). Correlation analyses, incorporating climate and anthropogenic factors, elucidated the drivers behind these spatial-temporal changes. [Results] Temporally, the region’s permanent water bodies diminished, whereas seasonal water bodies expanded over the past 22 years. Spatially, urban centers like Beijing, Tianjin, and Langfang saw a decline in surface water, in contrast to cities along the South-to-North Water Transfer project, which experienced growth. Baiyangdian's core wetland area fluctuated, decreasing initially then rising post-2005, while its periphery steadily increased. Qilihai wetlands saw a decline until 2010, followed by recovery. A positive correlation exists between maximum water area and precipitation in the south, and a negative one in eastern coastal cities, highlighting the natural replenishment and human activity imbalance. Significant correlations between water usage and surface water area in Beijing, Chengde, and Tangshan indicate the positive impact of water transfers and ecological replenishment, whereas negative correlations in Qinhuangdao and Tianjin suggest adverse effects of groundwater over-extraction. [Conclusion] This analysis uncovers the two-decade dynamics of surface water in the Beijing-Tianjin-Hebei region, offering insights for sustainable water resource management.

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  • 收稿日期:2023-10-26
  • 最后修改日期:2024-03-25
  • 录用日期:2024-03-29
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