Results 101 to 110 of about 16,487 (268)
, 2018 Key external forcing factors have been proposed to explain the collapse of ice sheets, including atmospheric and ocean temperatures, subglacial topography, relative sea level and tidal amplitudes.
J. Scourse +4 more
semanticscholar +1 more source
Permafrost and Periglacial Processes, Volume 37, Issue 1, Page 78-106, January/March 2026.ABSTRACT The aim of this work is to study a variety of glacial, periglacial and paraglacial features found in a small cirque, Fremri‐Grasárdalur, in Tröllaskagi (Northern Iceland). We implement a multidisciplinary approach combining high‐resolution geomorphological mapping, horizontal/vertical boulder displacement (from 1994 to 2019) and surface ...
Javier Santos‐González +13 more
wiley +1 more source
Frontiers in Earth ScienceVestnesa Ridge is built-up of thick contourites mainly deposited during the last ∼5 million years. Methane leaks from deep gas reservoirs creating pockmarks on its crest, and which have been the focus of numerous studies.
Tine L. Rasmussen, Tove Nielsen
doaj +1 more source
Environmental Controls on the Cycling of Fe and Mn in Patagonian Fjord Systems
Journal of Geophysical Research: Biogeosciences, Volume 131, Issue 1, January 2026.Abstract Fjord sediments are important reservoirs and conduits of potentially bioavailable iron (Fe) and manganese (Mn). Both elements are critical to life, serving as key reactants in metabolic pathways, and play an important role in the reactivity and burial of organic carbon.
L. Piret +3 more
wiley +1 more source
Polar Research, 2019 Kongsfjorden, a fjord in north-western Svalbard, is characterized by large environmental gradients driven by meltwater processes along the margins of tidewater glaciers and the inflow of relatively warm Atlantic Water, the main heat source for the ...
Katrine Husum +16 more
doaj +1 more source
Stratigraphic interpretation of loess in the marginal zone of the Dnieper I ice sheet and the evolution of its landscape after deglaciation (Dnieper Upland, Ukraine) [PDF]
, 2018 Maryna Komar +5 more
openalex +1 more source
Paleoceanography and Paleoclimatology, Volume 41, Issue 1, January 2026.Abstract Constraining how faunal communities vary over time and space in response to environmental change has long been a major goal of paleoecologists. Among fossilized organisms, few yield a better and greater detailed record than foraminifera to understand past marine conditions.
R. Fentimen, A. Sturbois, M. Mojtahid
wiley +1 more source
Polar Research, 2016 A lake sediment sequence from southern Store Koldewey, north-east Greenland, has been investigated using a multidisciplinary approach, including geophysical, geochemical, biogeochemical, biological and sedimentological methods.
Martin Klug, Ole Bennike, Bernd Wagner
doaj +1 more source
Centennial‐scale variability of the British Ice Sheet: Implications for climate forcing and Atlantic meridional overturning circulation during the last deglaciation [PDF]
, 2007 Paul Cornils Knutz +2 more
openalex +1 more source
New Insolation Forcing for Paleoclimate Studies
Paleoceanography and Paleoclimatology, Volume 41, Issue 1, January 2026.Abstract Insolation forcing at the top of the atmosphere is widely used in paleoceanographic and paleoclimatological studies. In paleoclimate simulations, it must reflect Earth’s orbital history. General Circulation Models (GCMs) typically use a modern orbital configuration to allow direct comparison to modern and near‐future scenarios, often with time
I. J. Kocken, R. E. Zeebe
wiley +1 more source