Episodic Subglacial Drainage Cascades Below the Northeast Greenland Ice Stream

Abstract Subglacial hydrology can exert an important control on ice flow by affecting friction at the ice‐bedrock interface. Here, we report on a series of subglacial drainage events along the Northeast Greenland Ice Stream (NEGIS), initiating as far inland as 500 km from the margin of Zachariae Iss...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: J. K. Andersen, N. Rathmann, C. S. Hvidberg, A. Grinsted, A. Kusk, J. P. Merryman Boncori, J. Mouginot
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
glaciology
Greenland
hydrology
DInSAR
Geophysics. Cosmic physics
QC801-809
Online Access:https://doi.org/10.1029/2023GL103240
https://doaj.org/article/6dc846118fab493db28b483b15fb3153
Description
Summary:Abstract Subglacial hydrology can exert an important control on ice flow by affecting friction at the ice‐bedrock interface. Here, we report on a series of subglacial drainage events along the Northeast Greenland Ice Stream (NEGIS), initiating as far inland as 500 km from the margin of Zachariae Isstrøm. The drainage events exhibit local transient uplift, followed by prolonged subsidence, measured by differential satellite synthetic aperture radar interferometry (DInSAR). In downstream regions, drainage events are associated with temporary acceleration in ice flow. The high spatiotemporal resolution of the DInSAR measurements allows for a detailed mapping of the drainage propagation pathway. We show that multiple drainage cascades have occurred along the same pathway over the years 2020–2022. Finally, the propagation speed of subglacial water flow is found to vary greatly along NEGIS, suggesting that fundamental differences could exist in the subglacial environment.

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