Results 101 to 110 of about 1,030 (156)

Plants' Contributions to People Shift With Glacier Extinction

Plant-Environment Interactions
Alpine environments are among the most vulnerable ecosystems to climate change, with glacier retreat rapidly altering plant communities, biodiversity, and ecosystem functions.
N. Khelidj, S. Balestra, M. S. Caccianiga, B. E. L. Cerabolini, D. Tampucci, G. Losapio   +5 more
doaj   +1 more source

THE LAST DEGLACIATION OF ALASKA [PDF]

Geological Society of America Abstracts with Programs, 2020
Jason P. Briner, Joseph P. Tulenko, Nicolás E. Young, Alia J. Lesnek, James F. Baichtal   +4 more
openaire   +1 more source

Deglacial decoupling

Nature Geoscience, 2013
openaire   +3 more sources

Stop-and-go deglaciation [PDF]

Nature Geoscience, 2012
openaire   +1 more source

Deglaciation of the Norwegian fjords

, 2018
Melting glaciers and ice sheets are perhaps the most visible signs of a warming cli- mate. Glaciers are retreating on every continent, ice sheets are shedding icebergs into a warming ocean at an accelerating rate, and the atmosphere melts more ice as tempera- tures rise.
openaire   +1 more source

Deglaciation of North America

, 2003
A S Dyke, A Moore, L Robertson
openaire   +1 more source

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Toward the snowball earth deglaciation…

Climate Dynamics, 2010
The current state of knowledge suggests that the Neoproterozoic snowball Earth is far from deglaciation even at 0.2 bars of CO2. Since understanding the termination of the fully ice-covered state is essential to sustain, or not, the snowball Earth theory, we used an Atmospheric General Climate Model (AGCM) to explore some key factors which could induce
Guillaume Le Hir, Yannick Donnadieu, Gerhard Krinner   +2 more
exaly   +4 more sources

Early Deglaciation of the Labrador Shelf

Science, 1978
Two marine sediment cores from a basin on the southeastern Labrador Shelf penetrate a mud sequence extending back to 21,000 carbon-14 years before the present (B.P.). The benthic foraminifera are dominated by subartic nearshore species indicative of ice-free summer waters.
G, Vilks, P J, Mudie
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The deglacial hemicycle

Geologische Rundschau, 1964
Absolute age relationships between (a) size reduction of continental ice sheets, (b) glacio-eustatic sea level rise, (c) temperature changes of the ocean surface, and (d) temperature changes on land show that the proper sequence is as follows: first, withdrawal of the ice sheets; second, warming of the land surface; and, third, warming of the ocean ...
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Deglaciation history of Latvia

2004
This chapter discusses the deglaciation history of Latvia. The earliest deglaciation schemes of Latvia were based entirely on morphological features. The spatial distribution of glacial landforms, with crests transverse to glacier movement combined with radiocarbon dates and biostratigraphical evidence, have provided the principal data for the ...
Vitālijs Zelčs, Aivars Markots
openaire   +1 more source