Identifying the causes of sea-level change
Global mean sea-level change has increased from a few centimetres per century over recent
millennia to a few tens of centimetres per century in recent decades. This tenfold increase in …
millennia to a few tens of centimetres per century in recent decades. This tenfold increase in …
A model of Greenland ice sheet deglaciation constrained by observations of relative sea level and ice extent
BS Lecavalier, GA Milne, MJR Simpson, L Wake… - Quaternary Science …, 2014 - Elsevier
An ice sheet model was constrained to reconstruct the evolution of the Greenland Ice Sheet
(GrIS) from the Last Glacial Maximum (LGM) to present to improve our understanding of its …
(GrIS) from the Last Glacial Maximum (LGM) to present to improve our understanding of its …
Twenty years of XRF core scanning marine sediments: what do geochemical proxies tell us?
RG Rothwell, I Croudace - Micro-XRF Studies of Sediment Cores …, 2015 - Springer
XRF core scanners, with their rapid and non-destructive analytical capability, have now
been used for two decades in the analysis of marine sediments. Initially they were used to …
been used for two decades in the analysis of marine sediments. Initially they were used to …
History of the Greenland Ice Sheet: paleoclimatic insights
RB Alley, JT Andrews, J Brigham-Grette… - Quaternary Science …, 2010 - Elsevier
Paleoclimatic records show that the Greenland Ice Sheet consistently has lost mass in
response to warming, and grown in response to cooling. Such changes have occurred even …
response to warming, and grown in response to cooling. Such changes have occurred even …
Holocene relative sea-level changes from near-, intermediate-, and far-field locations
Holocene relative sea-level (RSL) records exhibit spatial and temporal variability that arises
mainly from the interaction of eustatic (land ice volume and thermal expansion) and isostatic …
mainly from the interaction of eustatic (land ice volume and thermal expansion) and isostatic …
The Greenland Ice Sheet during the past 300,000 years: A review
The Greenland ice sheet's response to climate change is a major issue in the climate
debate. This report reviews existing evidence on how the ice sheet margins reacted to …
debate. This report reviews existing evidence on how the ice sheet margins reacted to …
Calibrating a glaciological model of the Greenland ice sheet from the Last Glacial Maximum to present-day using field observations of relative sea level and ice extent
We constrain a three-dimensional thermomechanical model of Greenland ice sheet (GrIS)
evolution from the Last Glacial Maximum (LGM, 21ka BP) to the present-day using, primarily …
evolution from the Last Glacial Maximum (LGM, 21ka BP) to the present-day using, primarily …
[HTML][HTML] Tracing Holocene temperatures and human impact in a Greenlandic Lake: Novel insights from hyperspectral imaging and lipid biomarkers
Global warming particularly impacts terrestrial and aquatic ecosystems in the Arctic. To
constrain the sensitivity of Arctic lakes and make meaningful predictions about future change …
constrain the sensitivity of Arctic lakes and make meaningful predictions about future change …
Improving the reliability of bulk sediment radiocarbon dating
Radiocarbon dated chronologies are the most extensively applied dating technique when
investigating the last∼ 45,000 years. In lake and marine sediments, a single macrofossil or …
investigating the last∼ 45,000 years. In lake and marine sediments, a single macrofossil or …
[PDF][PDF] Paleoenvironmental records, geophysical modelling and reconstruction of sea level trends and variability on centennial and longer time scales
K Lambeck, CD Woodroffe, F Antonioli… - … sea level rise and …, 2010 - academia.edu
The level of the sea does not remain constant. It changes at varying rates, geographically
and over time. Changes of sea level have affected human civilisations in the past (as …
and over time. Changes of sea level have affected human civilisations in the past (as …