Results 11 to 20 of about 208,369 (219)

Regional variability of diatoms in ice cores from the Antarctic Peninsula and Ellsworth Land, Antarctica [PDF]

open access: yesThe Cryosphere, 2022
The presence of marine microfossils (diatoms) in glacier ice and ice cores has been documented from numerous sites in Antarctica, Greenland, as well as from sites in the Andes and the Altai mountains, and attributed to entrainment and transport by winds.
D. R. Tetzner   +3 more
doaj   +1 more source

Regional validation of the use of diatoms in ice cores from the Antarctic Peninsula as a Southern Hemisphere westerly wind proxy [PDF]

open access: yesClimate of the Past, 2022
The Southern Hemisphere westerly winds are among the most important drivers of recently observed environmental changes in West Antarctica. However, the lack of long-term wind records in this region hinders our ability to assess the long-term context of ...
D. R. Tetzner   +4 more
doaj   +1 more source

The contribution of melt ponds to enhanced Arctic sea-ice melt during the Last Interglacial [PDF]

open access: yesThe Cryosphere, 2021
The Hadley Centre Global Environment Model version 3 (HadGEM3) is the first coupled climate model to simulate an ice-free Arctic during the Last Interglacial (LIG), 127 000 years ago.
R. Diamond   +5 more
doaj   +1 more source

Physical properties of shallow ice cores from Antarctic and sub-Antarctic islands [PDF]

open access: yesThe Cryosphere, 2021
The sub-Antarctic is one of the most data-sparse regions on earth. A number of glaciated Antarctic and sub-Antarctic islands have the potential to provide unique ice core records of past climate, atmospheric circulation, and sea ice. However, very little
E. R. Thomas   +9 more
doaj   +1 more source

Ice Core Chronologies from the Antarctic Peninsula: The Palmer, Jurassic, and Rendezvous Age-Scales

open access: yesGeosciences, 2022
In this study, we present the age scales for three Antarctic Peninsula (AP) ice cores: Palmer, Rendezvous, and Jurassic. The three cores are all intermediate-depth cores, in the 133–141 m depth range.
B. Daniel Emanuelsson   +4 more
doaj   +1 more source

Decadal Scale Variability of Larsen Ice Shelf Melt Captured by Antarctic Peninsula Ice Core

open access: yesGeosciences, 2022
In this study, we used the stable water isotope record (δ18O) from an ice core drilled in Palmer Land, southern Antarctic Peninsula (AP). Utilizing δ18O we identified two climate regimes during the satellite era.
B. Daniel Emanuelsson   +3 more
doaj   +1 more source

An Unprecedented Sea Ice Retreat in the Weddell Sea Driving an Overall Decrease of the Antarctic Sea‐Ice Extent Over the 20th Century

open access: yesGeophysical Research Letters, 2023
Sea‐ice extent is predicted to decrease in a warming climate. However, despite global warming over the past century, total Antarctic sea ice remained relatively stable from 1979 until 2015, before strongly melting.
Quentin Dalaiden   +5 more
doaj   +1 more source

The internal structure of the Brunt Ice Shelf from ice-penetrating radar analysis and implications for ice shelf fracture [PDF]

open access: yesThe Cryosphere, 2018
The rate and direction of rift propagation through ice shelves depend on both the stress field and the heterogeneity (or otherwise) of the physical properties of the ice.
E. C. King   +4 more
doaj   +1 more source

An Age Scale for the First Shallow (Sub-)Antarctic Ice Core from Young Island, Northwest Ross Sea

open access: yesGeosciences, 2021
The climate of the sub-Antarctic is important in understanding the environmental conditions of Antarctica and the Southern Ocean. However, regional climate proxy records from this region are scarce.
Dorothea Elisabeth Moser   +10 more
doaj   +1 more source

First evidence of industrial fly-ash in an Antarctic ice core

open access: yesScientific Reports, 2023
Spheroidal carbonaceous particles (SCPs) are a component of fly-ash, the particulate by-product of industrial high temperature combustion of fuel-oil and coal-series fuels.
E. R. Thomas   +4 more
doaj   +1 more source

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