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The geological record shows that abrupt changes in the Earth system can occur on
timescales short enough to challenge the capacity of human societies to adapt to …
timescales short enough to challenge the capacity of human societies to adapt to …
[HTML][HTML] Reconciling records of ice streaming and ice margin retreat to produce a palaeogeographic reconstruction of the deglaciation of the Laurentide Ice Sheet
This paper reconstructs the deglaciation of the Laurentide Ice Sheet (LIS; including the
Innuitian Ice Sheet) from the Last Glacial Maximum (LGM), with a particular focus on the …
Innuitian Ice Sheet) from the Last Glacial Maximum (LGM), with a particular focus on the …
Direct astronomical influence on abrupt climate variability
Abstract Changes in the magnitude of millennial-scale climate variability (MCV) during the
Late Pleistocene occur as a function of changing background climate state over tens of …
Late Pleistocene occur as a function of changing background climate state over tens of …
Persistent orbital influence on millennial climate variability through the Pleistocene
Abundant evidence from marine, ice-core and terrestrial records demonstrates that Earth's
climate has experienced co-evolution of orbital-and millennial-scale variability through the …
climate has experienced co-evolution of orbital-and millennial-scale variability through the …
Anatomy of Heinrich Layer 1 and its role in the last deglaciation
DA Hodell, JA Nicholl, TRR Bontognali… - …, 2017 - Wiley Online Library
X‐ray fluorescence (XRF) core scanning and X‐ray computed tomography data were
measured every 1 mm to study the structure of Heinrich Event 1 during the last deglaciation …
measured every 1 mm to study the structure of Heinrich Event 1 during the last deglaciation …
Abrupt North Atlantic circulation changes in response to gradual CO2 forcing in a glacial climate state
Glacial climate is marked by abrupt, millennial-scale climate changes known as Dansgaard–
Oeschger cycles. The most pronounced stadial coolings, Heinrich events, are associated …
Oeschger cycles. The most pronounced stadial coolings, Heinrich events, are associated …
A new view on abrupt climate changes and the bipolar seesaw based on paleotemperatures from Iberian Margin sediments
The last glacial cycle provides the opportunity to investigate large changes in the Atlantic
Meridional Overturning Circulation (AMOC) beyond the small fluctuations evidenced from …
Meridional Overturning Circulation (AMOC) beyond the small fluctuations evidenced from …
Ocean tide influences on the Antarctic and Greenland ice sheets
Ocean tides are the main source of high‐frequency variability in the vertical and horizontal
motion of ice sheets near their marine margins. Floating ice shelves, which occupy about …
motion of ice sheets near their marine margins. Floating ice shelves, which occupy about …
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 …
[HTML][HTML] Stochastic bifurcation of the North Atlantic circulation under a midrange future climate scenario with the NASA-GISS ModelE
Stochastic Bifurcation of the North Atlantic Circulation under a Midrange Future Climate
Scenario with the NASA-GISS ModelE in: Journal of Climate Volume 36 Issue 18 (2023) Jump …
Scenario with the NASA-GISS ModelE in: Journal of Climate Volume 36 Issue 18 (2023) Jump …