Mean sand flux in cores ER11, ER07 and ER13, Sermilik Fjord, Greenland

During the early 2000s the Greenland Ice Sheet experienced the largest ice-mass loss of the instrumental record, largely as a result of the acceleration, thinning and retreat of large outlet glaciers in West and southeast Greenland. The quasi-simultaneous change in the glaciers suggests a common cli...

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Bibliographic Details
Main Author: Andresen, Camilla S
Format: Dataset
Language:English
Published: PANGAEA 2012
Subjects:
Climate Change: Learning from the past climate
Grain size
Mastersizer 2000
Malvern Instrument Inc.
Helheim_Glacier_sandflux
High resolution
low background gamma spectroscopy (HPGe detector
Canberra Inc.)
Past4Future
Sand
flux
mean
per year
Sermilik Fjord
SE Greenland
Year of deposition
East Greenland
glacier
Greenland
Ice Sheet
North Atlantic
North Atlantic oscillation
Sermilik
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.786791
https://doi.org/10.1594/PANGAEA.786791

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