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Arctic glacier snowline altitudes rise 150 m over the last 4 decades

<p>The number of Arctic glaciers with direct, long-term measurements of mass balance is limited. Here we used satellite-based observations of the glacier snowline altitude (SLA), the location of the transition between snow cover and ice late in the summer, to approximate the position of the equilibr...

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Bibliographic Details
Main Authors: L. J. Larocca, J. M. Lea, M. P. Erb, N. P. McKay, M. Phillips, K. A. Lamantia, D. S. Kaufman
Format: Artigo
Language:Inglês
Published: Copernicus Publications 2024-08-01
Series:The Cryosphere
Online Access:https://tc.copernicus.org/articles/18/3591/2024/tc-18-3591-2024.pdf
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