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Glacier meltwater modulation of lake warming trends in China

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  • Corresponding author: lysist@ynnu.edu.cn 
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    1. We studied 2,260 lakes in China to assess how glacier meltwater modulates lake warming.

      Glacier meltwater suppressed over 86% of surface warming in glaciated lakes.

      Lakes in glaciated regions warmed less, especially during spring and summer melt seasons.

      Longwave radiation and air temperature drive glacier melt, controlling warming in glacial lakes.

  • Global warming has led to a rapid rise in lake surface water temperature (LSWT) over the past few decades. However, in some regions, enhanced glacier meltwater due to climate change may mitigate these trends. In this study, we investigated 2,260 lakes across China to understand the impact of glacier meltwater on LSWT from 1985 to 2022. We found that glaciated regions have a significantly lower average warming rate (0.06±0.004°C decade-1) compared to lakes in non-glaciated regions (0.17±0.004°C decade-1) (p<0.05). This difference is more pronounced during the glacier melting season (spring and summer). Importance assessment suggested that increased longwave radiation and air temperature accelerate glacier melting, controlling warming rate in glaciated lakes (66.9%). Moreover, we find that glacier meltwater significantly impacts LSWT trends (-0.1°C decade-1) suppressing over 86% of the warming rates in lakes located in glaciated regions. These findings provide important references to accurately evaluate the warming trend of LSWT in China, as well as more broadly, providing valuable insights for climate change impact studies and water resource management.
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  • Cite this article:

    Chen L., Luo Y., Yang K., et al. (2025). Glacier meltwater modulation of lake warming trends in China. The Innovation Geoscience 3:100147. https://doi.org/10.59717/j.xinn-geo.2025.100147
    Chen L., Luo Y., Yang K., et al. (2025). Glacier meltwater modulation of lake warming trends in China. The Innovation Geoscience 3:100147. https://doi.org/10.59717/j.xinn-geo.2025.100147

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