Large-eddy simulations of the ice-shelf–ocean boundary layer near the ice front of Nansen Ice Shelf, Antarctica [PDF]
Ice melting beneath Antarctic ice shelves is caused by heat transfer through the ice-shelf–ocean boundary layer (IOBL). However, our understanding of the fluid dynamics and thermohaline physics of the IOBL flow is poor.
J. S. Na +6 more
doaj +1 more source
The Geo-educational and Conservational Challenges Posed by Unconsolidated Deposits: Some Thoughts and Possible Solutions as Applied to Diamicton Deposits from the British Isles [PDF]
Unconsolidated diamicton deposits of Quaternary age cover much of the lowland areas of the British Isles. These are often poorly exposed and as a result their influence on development and importance as palaeontological archives are often under ...
Murphy Phillip
doaj +1 more source
Arctic deep-water anoxia and its potential role for ocean carbon sink during glacial periods
Freshening and oxygen depletion of the polar deep waters of the Amerasian Basin during the last glacial periods probably resulted in significant carbon burial, according to geochemical analyses of inorganic authigenic carbonates in Arctic Ocean sediments.
Kwangchul Jang +3 more
doaj +1 more source
Seasonality of isotopic and chemical composition of snowpack in the vicinity of Jang Bogo Station, East Antarctica [PDF]
Seasonal variations of the isotopic and chemical compositions of snowpits can provide useful tools for dating the age of the snowpit and examining the sources of aerosol.
Soon Do Hur +3 more
doaj +1 more source
Sensitivity of the Tropical Dust Cycle to Glacial Abrupt Climate Changes
During abrupt climate changes of the last glacial period paleorecords show large amplitude changes in the dust cycle. We use Earth System model simulations to evaluate processes operating across these events.
Peter O. Hopcroft +3 more
doaj +1 more source
Ice Shelf Water Structure Beneath the Larsen C Ice Shelf in Antarctica
Understanding ice shelf water (ISW) structure is crucial for studying the basal melting of ice shelves. In this study, we performed large‐eddy simulation experiments to assess ISW structure and basal melt patterns under different current velocity ...
Ji Sung Na +4 more
doaj +1 more source
The Late Palaeozoic Ice Age unconformity in southern Namibia viewed as a patchwork mosaic
The expansion of ice masses across southern Africa during the Late Palaeozoic Ice Age has been known for 150 years, including the distribution of upland areas in controlling the configuration of glaciation.
Daniel P. Le Heron +8 more
doaj +1 more source
Global mean sea level rise, driven by ice mass loss in Antarctic and Greenland Ice Sheets (AIS and GrIS), is a significant consequence of global warming.
Donghyuck David Lee +6 more
doaj +1 more source
Widespread erosion on high plateaus during recent glaciations in Scandinavia [PDF]
Glaciers create some of Earth’s steepest topography; yet, many areas that were repeatedly overridden by ice sheets in the last few million years include extensive plateaus.
Andersen, Jane L. +10 more
core +2 more sources
Sea surface temperature changes in the southern California borderlands during the last glacial-interglacial cycle [PDF]
A variety of evidence suggests that average sea surface temperatures (SSTs) during the last glacial maximum in the California Borderlands region were significantly colder than during the Holocene.
Bandy +52 more
core +2 more sources

