Results 51 to 60 of about 5,463 (215)
PROMICE-2022 ice mask: a high-resolution outline of the Greenland Ice Sheet from August 2022 [PDF]
Earth System Science DataThe Greenland Ice Sheet (GrIS) is losing mass at an accelerating rate in response to climate change. Its geometry responds to these changes over annual to decadal timescales, therefore making accurate and up-to-date mapping of its extent essential for ...
G. Luetzenburg +13 more
doaj +1 more source
Boreas, EarlyView.Raised marine MIS 5c sediments evidence extensive preceding (5d) glaciation in western Norway. This is the first out of five (or six) major Weichselian glacier advances that seem to correspond to North Atlantic sea surface cooling periods. Till beds capping the marine sediments show stages of pre‐LGM advance and subsequent retreat.
Eiliv Larsen +9 more
wiley +1 more source
Geology of Greenland Survey Bulletin, 1999 Chemical analyses by X-ray fluorescence spectrometry (XRF) and atomic absorption spectrometry (AAS) have been monitored since 1990 by five internal standards. Diagrams of the variability over nine years show that analytical data for major elements, Cr, Cu and V have been stable over the entire period, while data for Ni, Rb and Sr have been stable since
openaire +1 more source
New geophysical and geological mapping of the eastern Baffin Bay region, offshore West Greenland [PDF]
, 2016 The Geological Survey of Denmark and Greenland has carried out a detailed mapping project in the eastern Baffin Bay region covering c. 200 000 km2 (Fig. 1).
Knutz, Paul C +2 more
core +1 more source
Geological Survey of Denmark and Greenland Bulletin, 2019 The Greenland ice sheet has been losing mass in response to increased surface melting (Khan et al. 2015; van den Broeke et al. 2017) as well as discharge of ice from marine terminating outlet glaciers (van den Broeke et al. 2009; Box et al. 2018). Marine
Jonas K Andersen +17 more
doaj +1 more source
GEUS Bulletin, 2023 Two drill cores spanning the Upper Jurassic – Lower Cretaceous succession in Wollaston Forland, North-East Greenland, offer an insight into mud accumulation in an evolving distal fault block.
Jussi Hovikoski +5 more
doaj +1 more source
The Greenland–Scotland Ridge in a Changing Ocean: Time to Act?
Marine Ecology, EarlyView.ABSTRACT The Greenland–Scotland Ridge is a submarine mountain that rises up to 500 m below the sea surface and extends from the east coast of Greenland to the continental shelf of Iceland and across the Faroe Islands to Scotland. The ridge not only separates deeper ocean basins on either side, that is, the North Atlantic and Arctic oceans, but also ...
Christophe Pampoulie +2 more
wiley +1 more source
Regional airborne radiometric survey in West Greenland
, 1976 For description of data set see: GGU West Greenland survey details.Size: 46 ...
Geological Survey of Greenland and Risø National Laboratory
core +1 more source
The potential for large-scale, subsurface geological CO2 storage in Denmark [PDF]
, 2009 Carbon capture and storage (CCS) is increasingly considered to be a tool that can significantly reduce the emission of CO2. It is viewed as a technology that can contribute to a substantial, global reduction of emitted CO2 within the timeframe that seems
Anthonsen, Karen Lyng +3 more
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Water Resources ResearchSeveral climatic and state variables may drive the occurrence of coastal zone flooding, including, for example, storm surges, sea level rise, heavy rainfall, and high river and groundwater levels.
I. K. Seidenfaden +4 more
doaj +1 more source