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Researchers resolve flood dynamics in China’s Kumalak River Catchment in Tianshan Area


Researchers unravel flood dynamics in China's Kumalak River Catchment in Tianshan Region
Evaluation of the learn about space. Credit score: npj Local weather and Atmospheric Science (2025). DOI: 10.1038/s41612-025-00918-z

A contemporary learn about revealed in npj Local weather and Atmospheric Science has make clear the criteria influencing floods within the Kumalak River catchment, China.

The learn about, led by means of Prof. Chen Yaning from the Xinjiang Institute of Ecology and Geography of the Chinese language Academy of Sciences, gives new insights into the advanced interaction of environmental variables using floods on this alpine, glacierized area.

The Kumalak River, positioned within the Tianshan Mountains, has lengthy been recognized for its advanced flooding patterns, influenced by means of glacier meltwater, snowmelt, and rainfall. Alternatively, the mechanisms in the back of those occasions have remained poorly understood, in particular as local weather trade continues to have an effect on the area.

To analyze the relative contributions of those elements, the researchers hired the Soil and Water Review Software (SWAT)—Glacier style and a degree-day issue style. Additionally they presented two Lengthy Brief-Time period Reminiscence (LSTM) fashions, LSTM-SG and LSTM-DDF, to improve their research.

The usage of complicated ways comparable to additive decomposition and built-in gradients, the crew interpreted the effects to raised perceive the flooding dynamics.

The learn about discovered that glacier meltwater is the dominant driving force of annual most flood (AMF) occasions, contributing between 60.49% and 60.92% of the full runoff. Rainfall and snowmelt practice, contributing 26.86% to 29.50% and 10.01% to twelve.21%, respectively.

By contrast, for spring most flood (AMFSp) occasions, snowmelt performs a extra vital function, accounting for 48.49% to 56.08% of the full, with glacier meltwater and rainfall contributing 16.12% to 22.08% and 27.79% to 29.42%, respectively.

They discovered that glacier meltwater is the dominant driving force of annual most flood (AMF) occasions, whilst snowmelt considerably influences spring most flood (AMFSp) occasions. From 1960 to 2018, glacier meltwater accounted for roughly 60.49% to 60.92% of AMF occasions, adopted by means of rainfall at 26.86% to 29.50%, and snowmelt at 10.01% to twelve.21%.

For AMFSp occasions between 1961 and 2018, snowmelt emerged because the main issue, contributing 48.49% to 56.08%, with glacier meltwater and rainfall following at 16.12% to 22.08% and 27.79% to 29.42%, respectively.

“Interpretable deep studying can function a complementary device, offering precious views at the research of flood formation mechanisms,” stated Liang Wenting, first writer of the learn about.

This learn about gives essential insights that would considerably improve flood prediction fashions and make stronger the control of water sources in glacierized catchments, in particular amidst the demanding situations posed by means of local weather trade.

Additional information:
Wenting Liang et al, Shifted dominant flood drivers of an alpine glacierized catchment within the Tianshan area printed thru interpretable deep studying, npj Local weather and Atmospheric Science (2025). DOI: 10.1038/s41612-025-00918-z

Quotation:
Researchers resolve flood dynamics in China’s Kumalak River Catchment in Tianshan Area (2025, February 20)
retrieved 20 February 2025
from https://phys.org/information/2025-02-unravel-dynamics-china-kumalak-river.html

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