Articles | Volume 18, issue 8
https://doi.org/10.5194/tc-18-3591-2024
https://doi.org/10.5194/tc-18-3591-2024
Research article
 | 
15 Aug 2024
Research article |  | 15 Aug 2024

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

Laura J. Larocca, James M. Lea, Michael P. Erb, Nicholas P. McKay, Megan Phillips, Kara A. Lamantia, and Darrell S. Kaufman

Data sets

Snowline altitudes and shapefiles for 269 glaciers, Pan-Arctic, 1984-2022 Laura Larocca https://doi.org/10.18739/A2ZS2KF5T

Randolph Glacier Inventory - A Dataset of Global Glacier Outlines, Version 6 RGI Consortium https://doi.org/10.7265/4m1f-gd79

ERA5-Land hourly data from 1950 to present J. Muñoz-Sabater https://doi.org/10.24381/cds.e2161bac

ERA5-Land monthly averaged data from 1950 to present J. Muñoz-Sabater https://doi.org/10.24381/cds.68d2bb30

ASTER Global Digital Elevation Model V003 NASA/METI/AIST/Japan Spacesystems and U.S./Japan ASTER Science Team https://doi.org/10.5067/ASTER/ASTGTM.003

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Short summary
Here we present summer snowline altitude (SLA) time series for 269 Arctic glaciers. Between 1984 and 2022, SLAs rose ∼ 150 m, equating to a ∼ 127 m shift per 1 °C of summer warming. SLA is most strongly correlated with annual temperature variables, highlighting their dual effect on ablation and accumulation processes. We show that SLAs are rising fastest on low-elevation glaciers and that > 50 % of the studied glaciers could have SLAs that exceed the maximum ice elevation by 2100.