Stability of the Atlantic Meridional Overturning Circulation: A review and synthesis
The notion that the Atlantic Meridional Overturning Circulation (AMOC) can have more than
one stable equilibrium emerged in the 1980s as a powerful hypothesis to explain rapid …
one stable equilibrium emerged in the 1980s as a powerful hypothesis to explain rapid …
Pattern and timing of retreat of the last British-Irish Ice Sheet
During the last glacial the ice sheet that subsumed most of Britain, Ireland and the North Sea
attained its maximum extent by 27 ka BP and with an ice volume sufficient to raise global …
attained its maximum extent by 27 ka BP and with an ice volume sufficient to raise global …
Growth and retreat of the last British–Irish Ice Sheet, 31 000 to 15 000 years ago: the BRITICE‐CHRONO reconstruction
The BRITICE‐CHRONO consortium of researchers undertook a dating programme to
constrain the timing of advance, maximum extent and retreat of the British–Irish Ice Sheet …
constrain the timing of advance, maximum extent and retreat of the British–Irish Ice Sheet …
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 …
Coherent deglacial changes in western Atlantic Ocean circulation
Abrupt climate changes in the past have been attributed to variations in Atlantic Meridional
Overturning Circulation (AMOC) strength. However, the exact timing and magnitude of past …
Overturning Circulation (AMOC) strength. However, the exact timing and magnitude of past …
Millennial-scale fluctuations of the European Ice Sheet at the end of the last glacial, and their potential impact on global climate
Abstract Reconstructing Northern Hemisphere ice-sheet oscillations and meltwater routing
to the ocean is important to better understand the mechanisms behind abrupt climate …
to the ocean is important to better understand the mechanisms behind abrupt climate …
A new concept for the paleoceanographic evolution of Heinrich event 1 in the North Atlantic
New records of planktonic foraminiferal δ 18 O and lithic and foraminiferal counts from Eirik
Drift are combined with published data from the Nordic Seas and the “Ice Rafted Debris …
Drift are combined with published data from the Nordic Seas and the “Ice Rafted Debris …
Growth, dynamics and deglaciation of the last British–Irish ice sheet: the deep-sea ice-rafted detritus record
JD Scourse, AI Haapaniemi… - Quaternary Science …, 2009 - Elsevier
The evolution and dynamics of the last British–Irish Ice Sheet (BIIS) have hitherto largely
been reconstructed from onshore and shallow marine glacial geological and …
been reconstructed from onshore and shallow marine glacial geological and …
Radiocarbon as a dating tool and tracer in paleoceanography
LC Skinner, E Bard - Reviews of Geophysics, 2022 - Wiley Online Library
Radiocarbon is an extremely useful carbon cycle tracer and radiometric dating tool. Here,
we review the main principles and challenges involved in the use of radiocarbon in …
we review the main principles and challenges involved in the use of radiocarbon in …
Evolution of the Global Overturning Circulation since the Last Glacial Maximum based on marine authigenic neodymium isotopes
Abstract The Global Overturning Circulation is linked to climate change on glacial-
interglacial and multi-millennial timescales. The understanding of past climate-circulation …
interglacial and multi-millennial timescales. The understanding of past climate-circulation …