Search Results - "Langen, Peter L."
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Past perspectives on the present era of abrupt Arctic climate change
Published in Nature climate change (01-08-2020)“…Abrupt climate change is a striking feature of many climate records, particularly the warming events in Greenland ice cores. These abrupt and high-amplitude…”
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The Impact of Regional Arctic Sea Ice Loss on Atmospheric Circulation and the NAO
Published in Journal of climate (15-01-2016)“…Reduction of the Arctic sea ice cover can affect the atmospheric circulation and thus impact the climate beyond the Arctic. The atmospheric response may,…”
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The implication of nonradiative energy fluxes dominating Greenland ice sheet exceptional ablation area surface melt in 2012
Published in Geophysical research letters (28-03-2016)“…During two exceptionally large July 2012 multiday Greenland ice sheet melt episodes, nonradiative energy fluxes (sensible, latent, rain, and subsurface…”
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4
Algae Drive Enhanced Darkening of Bare Ice on the Greenland Ice Sheet
Published in Geophysical research letters (28-11-2017)“…Surface ablation of the Greenland ice sheet is amplified by surface darkening caused by light‐absorbing impurities such as mineral dust, black carbon, and…”
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The last interglacial climate: comparing direct and indirect impacts of insolation changes
Published in Climate dynamics (01-05-2017)“…The last interglacial climate was influenced by substantial changes in the annual insolation cycle that led to a warmer climate state with pronounced high…”
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Separation of Contributions from Radiative Feedbacks to Polar Amplification on an Aquaplanet
Published in Journal of climate (15-04-2012)“…When climate is forced by a doubling of CO₂, a number of feedback processes are induced, such as changes of water vapor, clouds, and surface albedo. Here the…”
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Outlet glacier flow response to surface melt: based on analysis of a high-resolution satellite data set
Published in Journal of glaciology (01-08-2023)“…The dynamics of the Greenland Ice Sheet are affected by surface meltwater reaching the base of the ice, altering ice contact with the bedrock. Lack of…”
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Dynamic simulations of Vatnajökull ice cap from 1980 to 2300
Published in Journal of glaciology (01-02-2020)“…Abstract Like most ice caps and glaciers worldwide, Icelandic glaciers are retreating in a warming climate. Here, the evolution of Vatnajökull ice cap,…”
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Asynchronous behavior of outlet glaciers feeding Godthåbsfjord (Nuup Kangerlua) and the triggering of Narsap Sermia's retreat in SW Greenland
Published in Journal of glaciology (01-04-2017)“…We assess ice loss and velocity changes between 1985 and 2014 of three tidewater and five-land terminating glaciers in Godthåbsfjord (Nuup Kangerlua),…”
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The firn meltwater Retention Model Intercomparison Project (RetMIP): evaluation of nine firn models at four weather station sites on the Greenland ice sheet
Published in The cryosphere (06-11-2020)“…Perennial snow, or firn, covers 80 % of the Greenland ice sheet and has the capacity to retain surface meltwater, influencing the ice sheet mass balance and…”
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Polar amplification as a preferred response in an idealized aquaplanet GCM
Published in Climate dynamics (01-08-2007)“…An aquaplanet atmospheric general circulation model (GCM) coupled to a mixed layer ocean is analyzed in terms of its polar amplified surface temperature…”
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Towards quantifying the glacial runoff signal in the freshwater input to Tyrolerfjord-Young Sound, NE Greenland
Published in Ambio (01-02-2017)“…Terrestrial freshwater runoff strongly influences physical and biogeochemical processes at the fjord scale and can have global impacts when considered at the…”
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The dynamic range of poleward energy transport in an atmospheric general circulation model
Published in Geophysical research letters (01-01-2005)“…Understanding the reasons for which current climate models fail to reproduce the low equator‐to‐pole temperature gradient of past warm periods is among the…”
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14
Abrupt shift in the observed runoff from the southwestern Greenland ice sheet
Published in Science advances (01-12-2017)“…The recent decades of accelerating mass loss of the Greenland ice sheet have arisen from an increase in both surface meltwater runoff and ice flow discharge…”
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Sensitivity of Glacier Runoff to Winter Snow Thickness Investigated for Vatnajökull Ice Cap, Iceland, Using Numerical Models and Observations
Published in Atmosphere (01-11-2018)“…Several simulations of the surface climate and energy balance of Vatnajökull ice cap, Iceland, are used to estimate the glacier runoff for the period 1980–2015…”
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Response in atmospheric circulation and sources of Greenland precipitation to glacial boundary conditions
Published in Climate dynamics (01-06-2009)“…The response in northern hemisphere atmospheric circulation and the resulting changes in moisture sources for Greenland precipitation to glacial boundary…”
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Polar Amplification in CCSM4: Contributions from the Lapse Rate and Surface Albedo Feedbacks
Published in Journal of climate (15-06-2014)“…A vertically nonuniform warming of the troposphere yields a lapse rate feedback by altering the infrared irradiance to space relative to that of a vertically…”
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Application of PROMICE Q‐Transect in Situ Accumulation and Ablation Measurements (2000–2017) to Constrain Mass Balance at the Southern Tip of the Greenland Ice Sheet
Published in Journal of geophysical research. Earth surface (01-06-2018)“…With nine southern Greenland ice sheet ablation area locations, the Programme for Monitoring of the Greenland Ice Sheet (PROMICE) “Q‐transect” is a source of…”
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Inflated Uncertainty in Multimodel‐Based Regional Climate Projections
Published in Geophysical research letters (28-11-2017)“…Multimodel ensembles are widely analyzed to estimate the range of future regional climate change projections. For an ensemble of climate models, the result is…”
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The future of tundra carbon storage in Greenland – Sensitivity to climate and plant trait changes
Published in The Science of the total environment (10-11-2022)“…The continuous change in observed key indicators such as increasing nitrogen deposition, temperatures and precipitation will have marked but uncertain…”
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