Results 191 to 200 of about 32,255 (226)

Magma Chamber Response to Ice Unloading: Applications to Volcanism in the West Antarctic Rift System. [PDF]

Geochem Geophys Geosyst
Coonin AN, Huber C, Troch J, Townsend M, Scholz K, Singer BS.   +5 more
europepmc   +1 more source

Sea level since the Last Glacial Maximum from the Atlantic coast of Africa. [PDF]

Nat Commun
Vacchi M, Shaw TA, Anthony EJ, Spada G, Melini D, Li T, Cahill N, Horton BP.   +7 more
europepmc   +1 more source

A rigorous and versatile statistical test for correlations between stationary time series. [PDF]

PLoS Biol
Yuan AE, Shou W.
europepmc   +1 more source

Reconstructing East Antarctic Temperature and Snowfall Variability from δ15N of N2

Bouchet M, Landais A, Klüssendorf AM, Brückner L, Legrain E, Capron E, Parrenin F, Menviel L, Grisart A, Prié F, Extier T, Jacob R, Fischer H, Traeger H, Tinner P, Schmitt J, Grimmer M.   +16 more
europepmc   +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
Le Hir, Guillaume, Donnadieu, Yannick, Krinner, Gerhard, Ramstein, Gilles   +3 more
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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
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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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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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Deglacial hypsometry of Antarctica

Earth and Planetary Science Letters, 1984
Abstract A new and more detailed analysis of the hypsometry of the Antarctic continent, based upon 1° digital data on ice thickness and surface and subglacial elevations, shows that Antarctica, even when deglaciated according to a simple Airy-isostatic model, is an unusual continent.
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