Results 121 to 130 of about 1,196 (236)

Palaeoglaciations in the Polar and Subpolar Ural Mountains

open access: yesBoreas, EarlyView.
The Ural Mountains form a major physiographic boundary between the East European Plain and West Siberia, both repeatedly glaciated during the Pleistocene by the Barents–Kara ice sheet. Although the present‐day topography reflects significant glacial modification, the extent, chronology and interaction of mountain glaciers with the Barents–Kara ice ...
Bartosz Kurjanski   +6 more
wiley   +1 more source

Glaciology

open access: yes, 1954
Glaciological research, mainly since World War II, is reviewed by the first author; and specific aspects outlined by the second: velocity relations, and structures in glaciers, phase relations in glacier ice, oxygen isotope studies in snow, firn and ...
Sharp, R.P., Baird, P.D.
core  

The Early Upper Palaeolithic open‐air site of Friedrichsdorf‐Seulberg, Germany, in the context of the northern central European Aurignacian

open access: yesBoreas, EarlyView.
Our knowledge of the Early Upper Palaeolithic occupation in northern central Europe is very limited, and recent research at the open‐air site of Friedrichsdorf‐Seulberg in Hesse, Germany, provides important new information on the Aurignacian. The site is rather small (26.5 m2) and spatial analysis identified a central hearth with two associated ...
Tilman Böckenförde   +5 more
wiley   +1 more source

Japanese National Institute of Polar Research

open access: yes, 2009
NIPR was established in Tokyo as one of the Inter-University Research Institutes of Monbusho, the Ministry of Education, Science, Sports and Culture, to conduct polar research in Japan. The NIPR Arctic Environment Research Center is Japan's corresponding

core  

Japanese glaciological activities in the Arctic region (report)

open access: yesJapanese glaciological activities in the Arctic region (report)
P(論文) The objectives of the Japanese Arctic Glaciological Expedition were to study the regional characteristics of glacier processes and the climatic and environmental changes for the last few hundred years in the Arctic cryosphere. During 1987-1996,glaciological observation and shallow ice core drilling were carried out at various places such as the ...
openaire  

Seasonal Ice Dynamics Control the Timing of Crevasse Drainage at a Fast‐Flowing Outlet Glacier

open access: yesAGU Advances, Volume 7, Issue 3, June 2026.
Abstract Crevasse field drainage transfers at least half of the seasonal runoff from the surface to the bed of the Greenland Ice Sheet, but the patterns of drainage are complex and spatio‐temporally heterogenous. To better understand controls on crevasse drainage processes, we use an automated deep learning method to map the seasonal filling and ...
T. R. Chudley   +7 more
wiley   +1 more source

Harold Victor Serson (1926-1992)

open access: yes, 1992
... Harold first went to the Arctic in 1944 as a Hudson\u27s Bay Company seaman aboard the Nascopie. Thus began a lifelong association with the Arctic. In 1945 he joined the Department of Transport as a radiosonde technician.
Jeffries, Martin O.
core  

Convection in fluid and porous media [PDF]

open access: yes, 2003
The subject of convection in fluid and porous media is investigated. Particular attention is paid to penetrative convection. The first two chapters are devoted to penetrative convection when fluid overlies and saturates a porous medium.
Carr, Magda
core  

Circumpolar Science : Scandinavian Approaches to the Arctic and the North Atlantic, ca. 1920 to 1960

open access: yes, 2014
ArgumentThe Scandinavian countries share a solid reputation as longstanding contributors to top level Arctic research. This received view, however, veils some deep-seated contrasts in the ways that Sweden, Norway, and Denmark have conducted research in ...
Sörlin, Sverker,
core   +1 more source

Ice‐Sheet–Ocean Interactions and the Reversibility of a Regime Shift Beneath Filchner‐Ronne Ice Shelf

open access: yesJournal of Geophysical Research: Oceans, Volume 131, Issue 6, June 2026.
Abstract Future atmospheric warming could cause an abrupt increase in ocean temperature beneath the Filchner–Ronne Ice Shelf, Antarctica, from −2.2°C to more than 0°C in a few decades. In simulations, such a transition leads to a twenty‐fold increase in sub‐shelf melt rates, driving a retreat of the ice sheet.
Ronja Reese   +2 more
wiley   +1 more source

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