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Published on: October 26, 2019
Lake pulses driven by glacier melting and climate variability
Songtao Ai1,2,3,4, Shoukat Ali Shah5,6, Yi Cai5
1Chinese Antarctic Center of Surveying and Mapping, Wuhan University, Wuhan, 430079, China. ast@whu.edu.cn.
Glacier melt dynamics in the Blue Moon Lake Valley show significant water level fluctuations, influenced by temperature and precipitation. This research offers insights into water availability and climate adaptation strategies for glacier-fed regions.
Area of Science:
- Glaciology and Hydrology
- Climate Change Science
- Environmental Modeling
Background:
- The Tibetan Plateau's glaciers are crucial for freshwater and climate regulation, acting as sensitive indicators of climate change.
- Understanding glacier-fed hydrological systems is vital for water resource management and climate adaptation planning.
- The Blue Moon Lake Valley (BMLV), fed by Baishui River Glacier No. 1, experiences subtle yet significant water level fluctuations (lake pulse phenomenon).
Purpose of the Study:
- To investigate the dynamic fluctuations in the water level of the Blue Moon Lake Valley.
- To analyze the interactions among glacier melt dynamics, climatic variables, and hydrological responses.
- To quantify the lake pulse phenomenon and its drivers.
Main Methods:
- Employed fast Fourier transform (FFT), multivariate regression (MVR), and random forest (RF) models.
- Analyzed water level data, glacier melt rates, and key climatic variables (temperature, solar radiation, precipitation, etc.).
- Calculated rate of change (ROC) in water level and glacier melt, cumulative sum (CS), and transit times.
Main Results:
- Water level ROC fluctuates between -0.006 and 0.01 m/min, with a median of -7.24E-06 m/min, influenced by glacier melt and precipitation.
- Maximum CS of 0.09 m indicates a net water level increase driven by precipitation, reduced evaporation, and increased glacier melt.
- Temperature is a critical factor influencing glacier melt and water level; melt peaks occur every ~2.87 hours, while water level peaks occur every ~6.5 hours, with a meltwater transit time of ~4.16 hours.
Conclusions:
- The study systematically elucidates the hydrological dynamics of the BMLV, highlighting the significant impact of glacier melt and climate variables.
- Findings underscore the importance of considering subtle hydrological fluctuations for accurate water resource assessment.
- This research provides crucial data for water resource management, ecosystem health, and climate change adaptation in glacier-dependent regions.
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