Results 91 to 100 of about 1,196 (236)

Bases for Field Research in Arctic and Subarctic Canada

open access: yes, 1988
There are more than 50 field stations in northern Canada. These are operated by governments, universities and private agencies. Although many have a particular disciplinary bias, such as marine science, meteorology, native studies, archaeology, limnology,
Adams, W. Peter
core  

Late Holocene moisture variability in Arctic Alaska from chitin δ18O

open access: yesBoreas, EarlyView.
Amplified warming in the Arctic has resulted in reduced sea‐ice extent, which can impact regional climate dynamics. Elucidating past moisture variability in response to changing temperatures and sea‐ice conditions can offer insight into how anthropogenic climate change may impact Arctic areas such as the Alaskan North Slope in the future. We contribute
Briana A. Edgerton, Melissa L. Chipman
wiley   +1 more source

Identifying the pre‐Odra river system with hydroacoustic and seismic reflection imagery offshore Rügen Island, southern Baltic Sea

open access: yesBoreas, EarlyView.
Understanding the course and dynamics of ancient river systems, such as the pre‐Odra, provides valuable insights into the post‐glacial evolution of landscapes and riverine processes. The northwest‐trending pre‐Odra was an important drainage system of the European mainland into the Baltic Basin during and after the Scandinavian Ice Sheet retreat ...
Maryse C. Schmidt   +4 more
wiley   +1 more source

Geomorphological and historical records of the surge-type behaviour of Hansbreen (Svalbard)

open access: yesAnnals of Glaciology
This paper presents geomorphological and historical records of the surge-type behaviour of Hansbreen, one of the most studied tidewater glaciers in Svalbard.
Aleksandra Osika, Jacek Jania
doaj   +1 more source

Palaeowinds and depositional conditions from Holocene loess in Sweden and Finland

open access: yesBoreas, EarlyView.
The nature of deglacial and Holocene wind regimes in Fennoscandia is debated, as is the degree to which wind‐blown loess deposits exist in the region. Loess deposits in Fennoscandia are often relatively thin, discontinuous and less well‐sorted than typical loess, and questions remain over the degree of their post‐depositional reworking and the impact ...
Calum J. Edward   +6 more
wiley   +1 more source

Devon Island Programs, 1968

open access: yes, 1969
Four field parties, studying glaciology, botany and ornithology, used the Arctic Institute\u27s facilities on Devon Island during the summer of 1968. The botanical and ornithological studies were carried out from the Base Camp near Cape Sparbo, while the
Hussell, D.J.T.   +2 more
core  

A review of topographic controls on moraine distribution [PDF]

open access: yes, 2014
Ice-marginal moraines are often used to reconstruct the dimensions of former ice masses, which are then used as proxies for palaeoclimate. This approach relies on the assumption that the distribution of moraines in the modern landscape is an accurate ...
Barr, Iestyn David   +4 more
core   +1 more source

Notes from the field: An interdisciplinary perspective on the experiences, challenges and solutions for conducting fieldwork in glacial and periglacial environments

open access: yesNordia Geographical Publications
Interdisciplinary research approaches are critical to understanding the profound shifts in glacial and periglacial environments due to climate change.
Virginija Popovaite   +6 more
doaj   +1 more source

Reanalysis of the US Geological Survey Benchmark Glaciers: long-term insight into climate forcing of glacier mass balance

open access: yesJournal of Glaciology, 2019
Mountain glaciers integrate climate processes to provide an unmatched signal of regional climate forcing. However, extracting the climate signal via intercomparison of regional glacier mass-balance records can be problematic when methods for ...
Shad O'Neel   +8 more
doaj   +1 more source

Thorncliffe Formation: A proglacial to subglacial lacustrine basin sequence, Greater Toronto Region, Canada

open access: yesBoreas, EarlyView.
Map of Lower sediment (LS) thickness is a surrogate for the distribution of Thorncliffe Formation (TF) and ~75% of TF thickness from the slope of Niagara Escarpment east to Brighton. Inset images show the LS sequence at the Don Valleys brickyards (DVBY) and undeformed TF sand and gravel (~15 m) below Newmarket Till (NT) at sites L and Co.
David R. Sharpe   +3 more
wiley   +1 more source

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