Ice-dammed lake drainage in west Greenland: drainage pattern and implications on ice flow and bedrock motion

Kristian Kjellerup Kjeldsen; Shfaqat Abbas Khan; Anders Anker Bjørk; Karina Nielsen; Jeremie Mouginot

doi:10.1002/2017GL074081

Ice-dammed lake drainage in west Greenland: drainage pattern and implications on ice flow and bedrock motion

Kristian Kjellerup Kjeldsen, Shfaqat Abbas Khan, Anders Anker Bjørk, Karina Nielsen, Jeremie Mouginot

5 Citationer (Scopus)

Abstract

Ice-dammed lakes drain frequently in Greenland, but the impacts of these events differ between sites. Here we study the quasi-cyclic behavior of the ~40 km² Lake Tininnilik in west Greenland and its impact on ice flow and crustal deformation. Data reveal rapid drainage of 1.83 ± 0.17 km³ of water in less than 7 days in 2010, leading to a speedup of the damming glacier, and an instantaneous modeled elastic bedrock uplift of 18.6 ± 0.1 mm confirmed by an independent lakeside GPS record. Since ice-dammed lakes are common on Greenland, our results highlight the importance of including other sources of surface loading in addition to ice mass change, when assessing glacial isostatic adjustment or elastic rebound using geodetic data. Moreover, the results illustrates a linkage between subglacial discharge and ice surface velocity, important for assessing ice flux, and thus mass balance, in a future warming climate.

Originalsprog	Engelsk
Tidsskrift	Geophysical Research Letters
Vol/bind	44
Udgave nummer	14
Sider (fra-til)	7320-7327
Antal sider	8
ISSN	0094-8276
DOI	https://doi.org/10.1002/2017GL074081
Status	Udgivet - 28 jul. 2017

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Citationsformater

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title = "Ice-dammed lake drainage in west Greenland: drainage pattern and implications on ice flow and bedrock motion",

abstract = "Ice-dammed lakes drain frequently in Greenland, but the impacts of these events differ between sites. Here we study the quasi-cyclic behavior of the ~40 km2 Lake Tininnilik in west Greenland and its impact on ice flow and crustal deformation. Data reveal rapid drainage of 1.83 ± 0.17 km3 of water in less than 7 days in 2010, leading to a speedup of the damming glacier, and an instantaneous modeled elastic bedrock uplift of 18.6 ± 0.1 mm confirmed by an independent lakeside GPS record. Since ice-dammed lakes are common on Greenland, our results highlight the importance of including other sources of surface loading in addition to ice mass change, when assessing glacial isostatic adjustment or elastic rebound using geodetic data. Moreover, the results illustrates a linkage between subglacial discharge and ice surface velocity, important for assessing ice flux, and thus mass balance, in a future warming climate.",

author = "Kjeldsen, {Kristian Kjellerup} and Khan, {Shfaqat Abbas} and Bj{\o}rk, {Anders Anker} and Karina Nielsen and Jeremie Mouginot",

year = "2017",

month = jul,

day = "28",

doi = "10.1002/2017GL074081",

language = "English",

volume = "44",

pages = "7320--7327",

journal = "Geophysical Research Letters",

issn = "0094-8276",

publisher = "Wiley-Blackwell",

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TY - JOUR

T1 - Ice-dammed lake drainage in west Greenland

T2 - drainage pattern and implications on ice flow and bedrock motion

AU - Kjeldsen, Kristian Kjellerup

AU - Khan, Shfaqat Abbas

AU - Bjørk, Anders Anker

AU - Nielsen, Karina

AU - Mouginot, Jeremie

PY - 2017/7/28

Y1 - 2017/7/28

N2 - Ice-dammed lakes drain frequently in Greenland, but the impacts of these events differ between sites. Here we study the quasi-cyclic behavior of the ~40 km2 Lake Tininnilik in west Greenland and its impact on ice flow and crustal deformation. Data reveal rapid drainage of 1.83 ± 0.17 km3 of water in less than 7 days in 2010, leading to a speedup of the damming glacier, and an instantaneous modeled elastic bedrock uplift of 18.6 ± 0.1 mm confirmed by an independent lakeside GPS record. Since ice-dammed lakes are common on Greenland, our results highlight the importance of including other sources of surface loading in addition to ice mass change, when assessing glacial isostatic adjustment or elastic rebound using geodetic data. Moreover, the results illustrates a linkage between subglacial discharge and ice surface velocity, important for assessing ice flux, and thus mass balance, in a future warming climate.

AB - Ice-dammed lakes drain frequently in Greenland, but the impacts of these events differ between sites. Here we study the quasi-cyclic behavior of the ~40 km2 Lake Tininnilik in west Greenland and its impact on ice flow and crustal deformation. Data reveal rapid drainage of 1.83 ± 0.17 km3 of water in less than 7 days in 2010, leading to a speedup of the damming glacier, and an instantaneous modeled elastic bedrock uplift of 18.6 ± 0.1 mm confirmed by an independent lakeside GPS record. Since ice-dammed lakes are common on Greenland, our results highlight the importance of including other sources of surface loading in addition to ice mass change, when assessing glacial isostatic adjustment or elastic rebound using geodetic data. Moreover, the results illustrates a linkage between subglacial discharge and ice surface velocity, important for assessing ice flux, and thus mass balance, in a future warming climate.

U2 - 10.1002/2017GL074081

DO - 10.1002/2017GL074081

M3 - Letter

SN - 0094-8276

VL - 44

SP - 7320

EP - 7327

JO - Geophysical Research Letters

JF - Geophysical Research Letters

IS - 14

ER -

Ice-dammed lake drainage in west Greenland: drainage pattern and implications on ice flow and bedrock motion

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