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Ocean‐Induced Melt Triggers Glacier Retreat in Northwest Greenland
Author(s) -
Wood M.,
Rignot E.,
Fenty I.,
Menemenlis D.,
Millan R.,
Morlighem M.,
Mouginot J.,
Seroussi H.
Publication year - 2018
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2018gl078024
Subject(s) - geology , glacier , bathymetry , tidewater , oceanography , fjord , future sea level , tidewater glacier cycle , front (military) , advection , sill , ice calving , climatology , greenland ice sheet , glacier morphology , sea ice , ice shelf , ice stream , cryosphere , geomorphology , pregnancy , thermodynamics , physics , geochemistry , lactation , biology , genetics
In recent decades, tidewater glaciers in Northwest Greenland contributed significantly to sea level rise but exhibited a complex spatial pattern of retreat. Here we use novel observations of bathymetry and water temperature from NASA's Ocean Melting Greenland mission to quantify the role of warm, salty Atlantic Water in controlling the evolution of 37 glaciers. Modeled ocean‐induced undercutting of calving margins compared with ice advection and ice front retreat observed by satellites from 1985 to 2015 indicate that 35 glaciers retreated when cumulative anomalies in ocean‐induced undercutting rose above the range of seasonal variability of calving‐front positions, while two glaciers standing on shallow sills and colder water did not retreat. Deviations in the observed timing of retreat are explained by residual uncertainties in bathymetry, inefficient mixing of waters in shallow fjords, and the presence of small floating sections. Overall, warmer ocean temperature triggered the retreat, but calving processes dominate ablation (71%).