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Greenland ice sheet climate disequilibrium and committed sea-level rise
Ice loss from the Greenland ice sheet is one of the largest sources of contemporary sea-level
rise (SLR). While process-based models place timescales on Greenland's deglaciation, their …
rise (SLR). While process-based models place timescales on Greenland's deglaciation, their …
[HTML][HTML] The future sea-level contribution of the Greenland ice sheet: a multi-model ensemble study of ISMIP6
The Greenland ice sheet is one of the largest contributors to global mean sea-level rise
today and is expected to continue to lose mass as the Arctic continues to warm. The two …
today and is expected to continue to lose mass as the Arctic continues to warm. The two …
Ubiquitous acceleration in Greenland Ice Sheet calving from 1985 to 2022
Nearly every glacier in Greenland has thinned or retreated over the past few decades,,–,
leading to glacier acceleration, increased rates of sea-level rise and climate impacts around …
leading to glacier acceleration, increased rates of sea-level rise and climate impacts around …
Rate of mass loss from the Greenland Ice Sheet will exceed Holocene values this century
Abstract The Greenland Ice Sheet (GIS) is losing mass at a high rate. Given the short-term
nature of the observational record, it is difficult to assess the historical importance of this …
nature of the observational record, it is difficult to assess the historical importance of this …
[HTML][HTML] New perspectives on ice forcing in continental arc magma plumbing systems
Determining how and why eruptive outputs are modulated by the loading and unloading of
ice is key to understanding whether ongoing and accelerating deglaciation across mid-to …
ice is key to understanding whether ongoing and accelerating deglaciation across mid-to …
Decadal to centennial timescale mantle viscosity inferred from modern crustal uplift rates in Greenland
The observed crustal uplift rates in Greenland are caused by the combined response of the
solid Earth to both ongoing and past surface mass changes. Existing elastic Earth models …
solid Earth to both ongoing and past surface mass changes. Existing elastic Earth models …
Insolation vs. meltwater control of productivity and sea surface conditions off SW Greenland during the Holocene
We address here the specific timing and amplitude of sea‐surface conditions and
productivity changes off SW Greenland, northern Labrador Sea, in response to the high …
productivity changes off SW Greenland, northern Labrador Sea, in response to the high …
Maximum southwest Greenland Ice Sheet recession in the early Holocene
Establishing the timing of maximum Holocene warmth in the Arctic is critical for
understanding global climate system response to external forcing. In Greenland, challenges …
understanding global climate system response to external forcing. In Greenland, challenges …
An improved and extended parameterization of the CO2 15 µm cooling in the middle and upper atmosphere (CO2_cool_fort-1.0)
The radiative infrared cooling of CO 2 in the middle atmosphere, where it emits under non-
local thermodynamic equilibrium (non-LTE) conditions, is a crucial contribution to the energy …
local thermodynamic equilibrium (non-LTE) conditions, is a crucial contribution to the energy …
[HTML][HTML] Greenland temperature and precipitation over the last 20 000 years using data assimilation
Reconstructions of past temperature and precipitation are fundamental to modeling the
Greenland Ice Sheet and assessing its sensitivity to climate. Paleoclimate information is …
Greenland Ice Sheet and assessing its sensitivity to climate. Paleoclimate information is …