Results 271 to 280 of about 27,141 (366)

A collection of figures for education and presentations. Theme: Glaciology and Paleoglaciology

, 2016
Hernán De Angelis
openalex   +2 more sources

Climate Feedbacks Derived From Spatial Gradients in Recent Climatology

Journal of Geophysical Research: Atmospheres, Volume 130, Issue 12, 28 June 2025.
Abstract Climate feedbacks, including Planck, surface albedo, water vapor‐lapse rate (WVLR) and cloud feedbacks, determine how much surface temperatures will eventually warm to balance anthropogenic radiative forcing. Climate feedbacks remain difficult to constrain directly from temporal variation in observed surface warming and radiation budgets due ...
P. Goodwin, R. G. Williams, P. Ceppi, B. B. Cael   +3 more
wiley   +1 more source

Regional ice flow piracy following the collapse of Midgaard Glacier in Southeast Greenland. [PDF]

Nat Commun
Huiban F, Millan R, Kjeldsen KK, Andresen CS, Dømgaard M, Dehecq A, Brunt S, Khan SA, Mouginot J, Bjørk AA.   +9 more
europepmc   +1 more source

Annotated bibliography of the Russian languages literature on glaciology for 2015

, 2017
V. M. Kotlyakov, Л. П. Чернова
openalex   +2 more sources

Glaciers in Western Canada‐Conterminous US and Switzerland Experience Unprecedented Mass Loss Over the Last Four Years (2021–2024)

Geophysical Research Letters, Volume 52, Issue 12, 28 June 2025.
Abstract Over the period 2021–2024, glaciers in Western Canada and the conterminous US (WCAN‐US), and Switzerland respectively lost mass at rates of 22.2 ± 9.0 and 1.5 ± 0.3 Gt yr−1 representing a twofold increase in mass loss compared to the period 2010–2020.
Brian Menounos, Matthias Huss, Shawn Marshall, Mark Ednie, Caitlyn Florentine, Lea Hartl   +5 more
wiley   +1 more source

Interpreting Ice Anisotropy of Greenland's Fastest Outlet Glacier Using Basal Icequakes

Geophysical Research Letters, Volume 52, Issue 12, 28 June 2025.
Abstract Ice anisotropy can have significant impact on ice rheology and flow dynamics. However, a lack of in situ measurements limits the validation and incorporation of anisotropy, so most ice flow models assume isotropic ice. Especially observations of anisotropy in fast‐flowing ice streams are scarce.
A. Nap, T. Hudson, F. Walter, A. Wehrlé, A. Kneib‐Walter, H. Rousseau, M. P. Lüthi   +6 more
wiley   +1 more source

Group 2i Isochrysidales thrive in marine and lacustrine systems with ice cover. [PDF]

Sci Rep
Wang KJ, Huang Y, Kartzinel T, Majaneva M, Richter N, Liao S, Andresen CS, Vermassen F.   +7 more
europepmc   +1 more source

Irreversible glacier change and trough water for centuries after overshooting 1.5 °C. [PDF]

Nat Clim Chang
Schuster L, Maussion F, Rounce DR, Ultee L, Schmitt P, Lacroix F, Frölicher TL, Schleussner CF.   +7 more
europepmc   +1 more source

Processes and Palaeo‐Environmental Changes in the Arctic from Past to Present (PalaeoArc) – introduction

Boreas, Volume 54, Issue 3, Page 284-287, July 2025.
Astrid Lyså, Ívar Ö. Benediktsson, Nicolaj K. Larsen, Juliane Müller, Matt O'Regan   +4 more
wiley   +1 more source