2023
DOI: 10.3390/w15152762
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The Influence of Glacier Mass Balance on River Runoff in the Typical Alpine Basin

Bin Yang,
Weibing Du,
Junli Li
et al.

Abstract: Quantifying the effects of alpine GMB (Glacier Mass Balance) on river runoff is an important content of climate change. Uncertainty exists in GMB monitoring when applying remote-sensing technology. There are several reasons for these uncertainties, such as terrain deviation co-registration among different topographic data, the mismatch between GSE (Glacier Surface Elevation) from satellite monitoring and the GMB that comprises the physical glacier properties, the driving factors of GMB, and the response patter… Show more

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Cited by 3 publications
(1 citation statement)
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“…Glaciers are abundant in the high-cold mountains area (HCMA), which are the main source of freshwater resources in the arid and semi-arid downstream areas [2,3]. Glaciers in many of the world's HCMAs have been observed to be melting significantly, and river runoff has increased such as the Kumalak River and Tuoshikan River, typical watersheds in the Tianshan Mountains of China, where runoff has increased by 1.5 × 10 8 m 3 and 3.3 × 10 8 m 3 , respectively, over the past 50 years, leading to greater flooding [4][5][6]. Arid and semi-arid mountainous areas in northwest China are highly vulnerable to glacial snowmelt flooding under extreme climate change [7].…”
Section: Introductionmentioning
confidence: 99%
“…Glaciers are abundant in the high-cold mountains area (HCMA), which are the main source of freshwater resources in the arid and semi-arid downstream areas [2,3]. Glaciers in many of the world's HCMAs have been observed to be melting significantly, and river runoff has increased such as the Kumalak River and Tuoshikan River, typical watersheds in the Tianshan Mountains of China, where runoff has increased by 1.5 × 10 8 m 3 and 3.3 × 10 8 m 3 , respectively, over the past 50 years, leading to greater flooding [4][5][6]. Arid and semi-arid mountainous areas in northwest China are highly vulnerable to glacial snowmelt flooding under extreme climate change [7].…”
Section: Introductionmentioning
confidence: 99%