生态恢复对毛乌素沙地陆地水储量影响
编号:3547 访问权限:仅限参会人 更新:2024-04-13 22:12:40 浏览:395次 口头报告

报告开始:2024年05月19日 14:10(Asia/Shanghai)

报告时间:5min

所在会场:[S14] 主题14、水文地球科学 [S14-7] 主题14、水文地球科学 专题14.19、专题14.20、专题14.23(19日下午,402)

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摘要
Large-scale ecological restoration (ER) programmes have been implemented in China to combat climate change and ecosystem degradation. However, there has been controversy regarding how ER affects terrestrial water storage (TWS). Researchers use the solutions provided by the Gravity Recovery and Climate Experiment (GRACE) to analyze TWS changes and the impact of ER on TWS. However, other human-induced disturbances are usually ignored, such as human-induced mass changes interfering with GRACE observations, and the impact of agricultural water consumption on TWS. Here, we focus on the Mu Us Sandyland, a model for environmental governance in China and globally, accurately quantifying the impact of ER and other anthropogenic disturbances on TWS in this area. We estimate that ER has consumed TWS at a maximum average rate of 7.46 ± 2.07 mm yr1 in the study area. ER results in a significant decrease in TWS in 68.68% of the regional area (P < 0.05). Areas with high TWS consumption are concentrated in the southeastern part of the Mu Us Sandyland, which is an ER hotspot. Moreover, ignoring the impact of coal mining and agricultural activities on TWS will lead to an overestimation of the negative impact of ER on TWS by 45.53%. Our study proposes a method to accurately quantify the impact of ER and highlights the importance of other human activities having non-negligible effects on TWS.
 
关键词
陆地水储量;气候变化;人类活动
报告人
申小凡
博士研究生 中科院地理所

稿件作者
申小凡 中科院地理所
贾小旭 中科院地理所
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重要日期
  • 会议日期

    05月17日

    2024

    05月20日

    2024

  • 03月31日 2024

    初稿截稿日期

  • 03月31日 2024

    报告提交截止日期

  • 05月20日 2024

    注册截止日期

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青年地学论坛理事会
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厦门大学近海海洋环境科学国家重点实验室
中国科学院城市环境研究所
自然资源部第三海洋研究所
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