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Spatiotemporal Variability in the Glacier Snowline Altitude across High Mountain Asia and Potential Driving Factors

The glacier snowline altitude (SLA) at the end of the melt season is an indicator of the glacier equilibrium line altitude and can be used to estimate glacier mass balance and reconstruct past climate. This study analyzes the spatiotemporal variability in glacier SLA across High Mountain Asia, inclu...

Ausführliche Beschreibung

Gespeichert in:
Hauptverfasser: Zhongming Guo, Lei Geng, Baoshou Shen, Yuwei Wu, Anan Chen, Ninglian Wang
Format: Artigo
Sprache:Inglês
Veröffentlicht: MDPI AG 2021-01-01
Schriftenreihe:Remote Sensing
Schlagworte:
glaciers
SLA
temporal variation
High Mountain Asia
temperature
precipitation
Online-Zugang:https://www.mdpi.com/2072-4292/13/3/425
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