[HTML][HTML] Deglaciation of the Eurasian ice sheet complex
The Eurasian ice sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …
[HTML][HTML] The build-up, configuration, and dynamical sensitivity of the Eurasian ice-sheet complex to Late Weichselian climatic and oceanic forcing
The Eurasian ice-sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum (LGM), after the Antarctic and North American ice sheets. Despite its …
Glacial Maximum (LGM), after the Antarctic and North American ice sheets. Despite its …
Source-specific biomarkers as proxies for Arctic and Antarctic sea ice
ST Belt - Organic geochemistry, 2018 - Elsevier
Over the last decade or so, certain source-specific C 25 highly branched isoprenoid (HBI)
lipid biomarkers have emerged as useful proxies for Arctic and Antarctic sea ice. Thus, IP 25 …
lipid biomarkers have emerged as useful proxies for Arctic and Antarctic sea ice. Thus, IP 25 …
An ice–climate oscillatory framework for Dansgaard–Oeschger cycles
LC Menviel, LC Skinner, L Tarasov… - Nature Reviews Earth & …, 2020 - nature.com
Intermediate glacial states were characterized by large temperature changes in Greenland
and the North Atlantic, referred to as Dansgaard–Oeschger (D–O) variability, with some …
and the North Atlantic, referred to as Dansgaard–Oeschger (D–O) variability, with some …
Arctic Ocean sea ice cover during the penultimate glacial and the last interglacial
Coinciding with global warming, Arctic sea ice has rapidly decreased during the last four
decades and climate scenarios suggest that sea ice may completely disappear during …
decades and climate scenarios suggest that sea ice may completely disappear during …
Abrupt climate and weather changes across time scales
The past provides evidence of abrupt climate shifts and changes in the frequency of climate
and weather extremes. We explore the nonlinear response to orbital forcing and then …
and weather extremes. We explore the nonlinear response to orbital forcing and then …
Holocene variability in sea ice cover, primary production, and Pacific‐Water inflow and climate change in the Chukchi and East Siberian Seas (Arctic Ocean)
In this study, we present new detailed biomarker‐based sea ice records from two sediment
cores recovered in the Chukchi Sea and the East Siberian Sea. These new biomarker data …
cores recovered in the Chukchi Sea and the East Siberian Sea. These new biomarker data …
[HTML][HTML] Holocene glacial history of Svalbard: Status, perspectives and challenges
We synthesize the current understanding of glacier activity on Svalbard from the end of the
Late Pleistocene (12,000 yrs. before present) to the end of the Little Ice Age (c. 1920 AD) …
Late Pleistocene (12,000 yrs. before present) to the end of the Little Ice Age (c. 1920 AD) …
Identification of paleo Arctic winter sea ice limits and the marginal ice zone: optimised biomarker-based reconstructions of late Quaternary Arctic sea ice
Abstract Analysis of> 100 surface sediments from across the Barents Sea has shown that the
relative abundances of the mono-unsaturated sea ice diatom-derived biomarker IP 25 and a …
relative abundances of the mono-unsaturated sea ice diatom-derived biomarker IP 25 and a …
Sea ice and millennial-scale climate variability in the Nordic seas 90 kyr ago to present
In the light of rapidly diminishing sea ice cover in the Arctic during the present atmospheric
warming, it is imperative to study the distribution of sea ice in the past in relation to rapid …
warming, it is imperative to study the distribution of sea ice in the past in relation to rapid …