Planktic foraminiferal distribution and stable isotope ratios of sediment core MSM05/5_712-1 from the Arctic Ocean

The Arctic is responding more rapidly to global warming than most other areas on our planet. Northward flowing Atlantic Water is the major means of heat advection towards the Arctic and strongly affects the sea ice distribution. Records of its natural variability are critical for the understanding o...

Full description

Bibliographic Details
Main Authors: Spielhagen, Robert F, Werner, Kirstin, Sørensen, Steffen Aagaard, Zamelczyk, Katarzyna, Kandiano, Evgenia S, Budéus, Gereon, Husum, Katrine, Marchitto, Thomas M, Hald, Morten
Format: Dataset
Language:English
Published: PANGAEA 2011
Subjects:
GKG
IPY
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.755114
https://doi.org/10.1594/PANGAEA.755114
Description
Summary:The Arctic is responding more rapidly to global warming than most other areas on our planet. Northward flowing Atlantic Water is the major means of heat advection towards the Arctic and strongly affects the sea ice distribution. Records of its natural variability are critical for the understanding of feedback mechanisms and the future of the Arctic climate system, but continuous historical records reach back only ~150 years. Here, we present a multidecadal scale record of ocean temperature variations during the last 2000 years, derived from marine sediments off Western Svalbard (79°N). We find that early-21st-century temperatures of Atlantic Water entering the Arctic Ocean are unprecedented over the past 2000 years and are presumably linked to the Arctic Amplification of global warming.