Preprints
https://doi.org/10.5194/egusphere-2024-826
https://doi.org/10.5194/egusphere-2024-826
25 Mar 2024
 | 25 Mar 2024

Impacts of glacier changes on precipitation in the Tibetan Plateau

Qian Lin, Jie Chen, and Deliang Chen

Abstract. The Tibetan Plateau (TP) harbors the largest expanse of glaciers at middle and high latitudes globally. Against the backdrop of ongoing global warming, TP glaciers have experienced widespread retreat and significant mass balance alterations in recent decades, raising questions about their impact on regional climate. In this study, we address this knowledge gap by investigating the magnitude and spatial extent of precipitation responses to glacier changes across the TP using four distinct Weather Research and Forecasting (WRF) simulations reflecting different glacier and climate conditions. Our findings reveal that, on average, mean precipitation (except for winter) tends to diminish by approximately 0.6 % to 2.0 % during a cold year and increases by about 0.2 % to 2.5 % during a warm year over most grid cells influenced by glacier alterations. Additionally, glacier changes lead to a reduction (or augmentation) of summer mean precipitation by an average of 0.6 % to 5.2 % (1.2 % to 10.7 %) over different regions of the TP during the cold (warm) years, accompanied by a notable increase of 0.8 % to 19.7 % in summer extreme precipitation, irrespective of climate conditions. In general, glacier changes exert a more pronounced impact on summer extreme precipitation events than mean precipitation, with an average increase of 1.7 % and 4.6 % over the whole TP during the cold and warm years, respectively. Moreover, glacier changes in warmer climate conditions tend to increase summer precipitation amounts in high-altitude areas when the water supply is adequate.

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Qian Lin, Jie Chen, and Deliang Chen

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-826', Anonymous Referee #1, 03 Apr 2024
    • AC1: 'Reply on RC1', Qian Lin, 06 Jun 2024
  • RC2: 'Comment on egusphere-2024-826', Anonymous Referee #2, 27 Apr 2024
    • AC2: 'Reply on RC2', Qian Lin, 06 Jun 2024

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-826', Anonymous Referee #1, 03 Apr 2024
    • AC1: 'Reply on RC1', Qian Lin, 06 Jun 2024
  • RC2: 'Comment on egusphere-2024-826', Anonymous Referee #2, 27 Apr 2024
    • AC2: 'Reply on RC2', Qian Lin, 06 Jun 2024
Qian Lin, Jie Chen, and Deliang Chen
Qian Lin, Jie Chen, and Deliang Chen

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Short summary
Glaciers of the Tibetan Plateau (TP) have experienced widespread retreat in recent decades, but impacts of glacier changes that have occurred on regional climate, including precipitation, is still unknown. Thus, this study addressed this knowledge gap, and found that glacier changes exert a more pronounced impact on summer extreme precipitation events than mean precipitation over the TP. This provides a certain theoretical reference for the further improvement of long-term glacier projection.