Monthly glacier mass changes from CryoSat-2 radar altimetry

We generate arecord of ice loss across glaciers globally for the first time from CryoSat-2 swath interferometric radar altimetry. CryoSat-2’s orbital sub-cycle of 30 days allows us to resolve changes at high temporal resolution for Alaska, Arctic Canada North and South, Greenland periphery glaciers,...

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Bibliographic Details
Main Authors: Livia Jakob, Noel Gourmelen
Format: Other/Unknown Material
Language:unknown
Published: Zenodo 2023
Subjects:
glaciers
mass change
mass balance
Franz Josef Land
glacier
glacier*
Greenland
Iceland
Novaya Zemlya
Severnaya Zemlya
Svalbard
Alaska
Online Access:https://doi.org/10.5281/zenodo.7565993
Description
Summary:We generate arecord of ice loss across glaciers globally for the first time from CryoSat-2 swath interferometric radar altimetry. CryoSat-2’s orbital sub-cycle of 30 days allows us to resolve changes at high temporal resolution for Alaska, Arctic Canada North and South, Greenland periphery glaciers, Iceland, Svalbard, Franz Josef Land, Novaya Zemlya, Severnaya Zemlya, High Mountain Asia, Southern Andes andAntarctic periphery glaciers between 2010 and 2020.

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