Results 31 to 40 of about 16,487 (268)
Geosciences, 2018 Glacial forefields areas are dynamic landscapes, and due to the glacier frontal position changes, they are sensitive to climatic fluctuations. The results of the analysis of aerial photos, satellite imagery, archival maps, and terrestrial laser scanning ...
Joanna Sziło, Robert Józef Bialik
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Simulated last deglaciation of the Barents Sea Ice Sheet primarily driven by oceanic conditions
Quaternary Science Reviews, 2020 An interconnected complex of ice sheets, collectively referred to as the Eurasian ice sheets, covered north-westernmost Europe, Russia and the Barents Sea during the Last Glacial Maximum (around 21 ky BP), connecting to the Scandinavian Ice Sheet to ...
M. Petrini +10 more
semanticscholar +1 more source
Rate of Melt Ascent Beneath Iceland From the Magmatic Response to Deglaciation [PDF]
Geochemistry Geophysics Geosystems, 2019 Observations of the time lag between the last deglaciation and a surge in volcanic activity in Iceland constrain the average melt ascent velocity to be ≥50 m/year. Although existing theoretical work has explained why the surge in eruption rates increased
I. Eksinchol +2 more
semanticscholar +1 more source
Two additions to the moss flora of the South Shetland Islands in the maritime Antarctic
Acta Societatis Botanicorum Poloniae, 2018 Tortella fragilis (Drumm.) Limpr. (Pottiaceae) and Bryum nivale Müll. Hal. (Bryaceae) are recorded for the first time from the South Shetland Islands in the northern maritime Antarctic. They were discovered in the Admiralty Bay area on King George Island,
Mariusz Wierzgoń +2 more
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Eskers and bedrock gorges (tunnel valleys) in the Pakasaivo area, western Finnish Lapland [PDF]
Bulletin of the Geological Society of Finland, 2003 Studies of the deglaciation of the last Scandinavian Ice Sheet, including the behavior of the ice sheet and meltwater activity, were conducted in the vicinity of the Pakasaivo canyon lake, located in western Finnish Lapland.
P. Johansson
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The North American hydrologic cycle through the last deglaciation
Quaternary Science Reviews, 2019 While the climate evolution of North America during the last deglaciation has received considerable attention, few detailed model–data comparisons of the deglacial hydroclimate have been conducted at the continental scale. Here we use a transient climate
J. Lora, D. Ibarra
semanticscholar +1 more source
Arctic, Antarctic, and Alpine Research, 2023 Widespread glacial retreat is now occurring in many arctic mountain ranges, yet little is known about primary succession following deglaciation in these settings.
Shawnee A. Kasanke +3 more
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Deep-water circulation changes lead North Atlantic climate during deglaciation
Nature Communications, 2019 Constraining the response time of the climate system to changes in North Atlantic Deep Water (NADW) formation is fundamental to improving climate and Atlantic Meridional Overturning Circulation predictability.
F. Muschitiello +11 more
semanticscholar +1 more source
Retreat of the Cordillera Darwin icefield during Termination I
Cuadernos de Investigación Geográfica, 2017 During the last glaciation, the Cordillera Darwin icefield expanded northward toward the Straits of Magellan, eastward across Isla Grande de Tierra del Fuego and through Canal Beagle, and south and west across the numerous islands of southernmost Chile ...
B. L. Hall +4 more
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Geomorphology of the Aran Valley (Upper Garonne Basin, Central Pyrenees)
Journal of Maps, 2022 Geomorphological mapping in mountain regions is key for a better understanding of past and present environmental dynamics. Here, we present a 1:25000 scale geomorphological map covering 553 km2 of the Aran Valley, Upper Garonne Basin (Central Pyrenees ...
M. Fernandes +3 more
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