自2018年至今,卢善龙课题组持续关注和研究青藏高原河流与湖泊水系统变化,并通过对气候变化引发的长江源可可西里卓乃湖-盐湖流域湖泊溃决—湖泊流域沙化—河湖水力联系重构等连锁水文生态问题的研究(Lu et al., 2019,2020),认为长江源卓乃湖-盐湖流域河流湖泊水系统水量显著增加、湖泊溃决、河湖水力联系重建等河流湖泊水系统变化是在青藏高原水系统整体失衡失稳过程中形成的,它是气候变化和人类活动共同作用推动形成的地表河湖水系统演化新模式 (Lu et al., 2021)。
Lu, S., Jin, J., Zhou, J., Li, X., Ju, J., Li, M., Chen, F., Zhu, L., Zhao, H., Yan, Q., Xie, C., Yao, X., Fagherazzi, S. 2021. Drainage basin reorganization and endorheic-exorheic transition triggered by climate change and human intervention. Global and Planetary Change, 201: 103494.
Lu, S., Chen, F., Zhou, J., Hughes, A.C., Ma, X., Gao, W. 2020. Cascading implications of a single climate change event for fragile ecosystems on the Qinghai-Tibetan Plateau. Ecosphere, 11(9): e03243.
Lu, S., Chen, F., Zhou, J., Hughes, A.C. 2019. Accounting for the long lasting unexpected impacts of climate change on the Tibetan antelope survival. Science, eLetters, https://science.sciencemag.org/content/accounting-long-lasting-unexpected-impacts-climate-change-tibetan-antelope-survival.
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