Abstract

The climate varies due to human activity, natural climate cycles, and natural events external to the climate system. Understanding the different roles played by these drivers of variability is fundamental to predicting near-term climate change and changing extremes, and to attributing observed change to anthropogenic or natural factors. Natural drivers such as large explosive volcanic eruptions or multidecadal cycles in ocean circulation occur infrequently and are therefore poorly represented within the observational record. Here we turn to the first high-latitude annually-resolved and absolutely dated marine record spanning the last millennium, and the Paleoclimate Modelling Intercomparison Project (PMIP) Phase 3 Last Millennium climate model ensemble spanning the same time period, to examine the influence of natural climate drivers on Arctic sea ice. We show that bivalve oxygen isotope data are recording multidecadal Arctic sea ice variability and through the climate model ensemble demonstrate that external natural drivers explain up to third of this variability. Natural external forcing causes changes in sea-ice mediated export of freshwater into areas of active deep convection, affecting the strength of the Atlantic Meridional Overturning Circulation (AMOC) and thereby northward heat transport to the Arctic. This in turn leads to sustained anomalies in sea ice extent. The models capture these positive feedbacks, giving us improved confidence in their ability to simulate future sea ice in in a rapidly evolving Arctic.

Details

Title
Natural drivers of multidecadal Arctic sea ice variability over the last millennium
Author
Halloran, Paul R 1   VIAFID ORCID Logo  ; Hall, Ian R 2   VIAFID ORCID Logo  ; Menary, Matthew 3 ; Reynolds, David J 4 ; Scourse, James D 5 ; Screen, James A 6   VIAFID ORCID Logo  ; Bozzo Alessio 7 ; Dunstone Nick 8 ; Phipps, Steven 9   VIAFID ORCID Logo  ; Schurer, Andrew P 10   VIAFID ORCID Logo  ; Sueyoshi Tetsuo 11   VIAFID ORCID Logo  ; Zhou Tianjun 12   VIAFID ORCID Logo  ; Garry Freya 1 

 University of Exeter, College of Life and Environmental Sciences, Exeter, UK (GRID:grid.8391.3) (ISNI:0000 0004 1936 8024) 
 Cardiff University, School of Earth and Ocean Science, Cardiff, UK (GRID:grid.5600.3) (ISNI:0000 0001 0807 5670) 
 Sorbonne Universités (SU)‐CNRS‐IRD‐MNHN, LOCEAN/IPSL, Paris, France (GRID:grid.462844.8) (ISNI:0000 0001 2308 1657) 
 Cardiff University, School of Earth and Ocean Science, Cardiff, UK (GRID:grid.5600.3) (ISNI:0000 0001 0807 5670); The University of Arizona, Laboratory of Tree Ring Research, Arizona, USA (GRID:grid.134563.6) (ISNI:0000 0001 2168 186X) 
 University of Exeter, Penryn Campus, College of Life and Environmental Sciences, Penryn, UK (GRID:grid.8391.3) (ISNI:0000 0004 1936 8024) 
 University of Exeter, College of Engineering, Mathematics and Physical Sciences, Exeter, UK (GRID:grid.8391.3) (ISNI:0000 0004 1936 8024) 
 Eumetsat, Darmstadt, Germany (GRID:grid.426436.1) (ISNI:0000 0004 0621 7921) 
 Met Office Hadley Centre, Exeter, UK (GRID:grid.17100.37) (ISNI:0000000405133830) 
 University of Tasmania, Institute for Marine and Antarctic Studies, Hobart, Australia (GRID:grid.1009.8) (ISNI:0000 0004 1936 826X) 
10  The University of Edinburgh, School of Geosciences, Edinburgh, UK (GRID:grid.4305.2) (ISNI:0000 0004 1936 7988) 
11  National Institute of Polar Research, Tachikawa-city, Japan (GRID:grid.410816.a) (ISNI:0000 0001 2161 5539); Japan Agency for Marine-Earth Science and Technology, 3173-25, Showa-machi Kanazawa-ku, Yokohama City, Japan (GRID:grid.410588.0) (ISNI:0000 0001 2191 0132) 
12  LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China (GRID:grid.424023.3) (ISNI:0000 0004 0644 4737) 
Publication year
2020
Publication date
2020
Publisher
Nature Publishing Group
e-ISSN
20452322
Source type
Scholarly Journal
Language of publication
English
ProQuest document ID
2343281605
Copyright
This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.