Atlantic water intrusion triggers rapid retreat and regime change at previously stable Greenland glacier
Ice discharge from Greenland's marine-terminating glaciers contributes to half of all mass
loss from the ice sheet, with numerous mechanisms proposed to explain their retreat. Here …
loss from the ice sheet, with numerous mechanisms proposed to explain their retreat. Here …
An interdisciplinary perspective on Greenland's changing coastal margins
Greenland's coastal margins are influenced by the confluence of Arctic and Atlantic waters,
sea ice, icebergs, and meltwater from the ice sheet. Hundreds of spectacular glacial fjords …
sea ice, icebergs, and meltwater from the ice sheet. Hundreds of spectacular glacial fjords …
Consistent seasonal hydrography from moorings at Northwest Greenland glacier fronts
Greenland's marine‐terminating glaciers connect the ice sheet to the ocean and provide a
critical boundary where heat, freshwater, and nutrient exchanges take place. Buoyant …
critical boundary where heat, freshwater, and nutrient exchanges take place. Buoyant …
Advances in monitoring glaciological processes in Kalallit Nunaat (Greenland) over the past decades
Greenland's glaciers have been retreating, thinning and accelerating since the mid-1990s,
with the mass loss from the Greenland Ice Sheet (GrIS) now being the largest contributor to …
with the mass loss from the Greenland Ice Sheet (GrIS) now being the largest contributor to …
Summer hydrography conditions at proglacial fjord entrances along East Greenland
S Rysgaard, J Mortensen, M Haxen… - Journal of …, 2024 - Wiley Online Library
Climate change is causing widespread melting of land and sea ice in the Arctic, leading to
an increase in freshwater input to the ocean. This may have an impact on ocean circulation …
an increase in freshwater input to the ocean. This may have an impact on ocean circulation …
Heterogeneous impacts of ocean thermal forcing on ice discharge from Greenland's peripheral tidewater glaciers over 2000–2021
Abstract The Greenland Ice Sheet is losing mass at increasing rates. Substantial amounts of
this mass loss occur by ice discharge which is influenced by ocean thermal forcing. The ice …
this mass loss occur by ice discharge which is influenced by ocean thermal forcing. The ice …
Relative roles of plume and coastal forcing on exchange flow variability of a glacial fjord
Glacial fjord circulation determines the import of oceanic heat to the Greenland Ice Sheet
and the export of ice sheet meltwater to the ocean. However, limited observations and the …
and the export of ice sheet meltwater to the ocean. However, limited observations and the …
Inferring Mass Loss by Measuring Contemporaneous Deformation around the Helheim Glacier, Southeastern Greenland, Using Sentinel-1 InSAR
Z Erfani Jazi, M Motagh, V Klemann - Remote Sensing, 2022 - mdpi.com
The elastic response of solid earth to glacier and ice sheet melting, the most important
consequences of climate change, is a contemporaneous uplift. Here, we use interferometric …
consequences of climate change, is a contemporaneous uplift. Here, we use interferometric …
Changing oceanographic conditions in East Greenland
CVB Gjelstrup - 2024 - orbit.dtu.dk
East Greenland is a region of significant climatic and ecological importance. The region
provides three main ecosystem functions: climate regulation, carbon sequestration and …
provides three main ecosystem functions: climate regulation, carbon sequestration and …
Alongshore winds force warm Atlantic water toward Helheim glacier in southeast Greenland
Enhanced transport of warm subsurface Atlantic Water (AW) into Greenland fjords has
driven glacier mass loss, but the mechanisms transporting AW to the fjords remain poorly …
driven glacier mass loss, but the mechanisms transporting AW to the fjords remain poorly …