eCite Digital Repository

Inter-hemispheric temperature variability over the past millennium


Neukom, R and Gergis, J and Karoly, DJ and Wanner, H and Curran, MAJ and Elbert, J and Gonzalez-Rouco, F and Linsley, BK and Moy, AD and Mundo, I and Raible, CC and Steig, EJ and van Ommen, TD and Vance, TR and Villalba, R and Zinke, J and Frank, D, Inter-hemispheric temperature variability over the past millennium, Nature Climate Change, 4, (5) pp. 362-367. ISSN 1758-678X (2014) [Refereed Article]

Copyright Statement

Copyright 2014 Macmillan Publishers

DOI: doi:10.1038/nclimate2174


The Earth’s climate system is driven by a complex interplay of internal chaotic dynamics and natural and anthropogenic external forcing. Recent instrumental data have shown a remarkable degree of asynchronicity between Northern Hemisphere and Southern Hemisphere temperature fluctuations, thereby questioning the relative importance of internal versus external drivers of past as well as future climate variability1, 2, 3. However, large-scale temperature reconstructions for the past millennium have focused on the Northern Hemisphere4, 5, limiting empirical assessments of inter-hemispheric variability on multi-decadal to centennial timescales. Here, we introduce a new millennial ensemble reconstruction of annually resolved temperature variations for the Southern Hemisphere based on an unprecedented network of terrestrial and oceanic palaeoclimate proxy records. In conjunction with an independent Northern Hemisphere temperature reconstruction ensemble5, this record reveals an extended cold period (1594–1677) in both hemispheres but no globally coherent warm phase during the pre-industrial (1000–1850) era. The current (post-1974) warm phase is the only period of the past millennium where both hemispheres are likely to have experienced contemporaneous warm extremes. Our analysis of inter-hemispheric temperature variability in an ensemble of climate model simulations for the past millennium suggests that models tend to overemphasize Northern Hemisphere–Southern Hemisphere synchronicity by underestimating the role of internal ocean–atmosphere dynamics, particularly in the ocean-dominated Southern Hemisphere. Our results imply that climate system predictability on decadal to century timescales may be lower than expected based on assessments of external climate forcing and Northern Hemisphere temperature variations5, 6 alone.

Item Details

Item Type:Refereed Article
Keywords:temperature variability, temperature fluctuations, palaeoclimate
Research Division:Earth Sciences
Research Group:Physical geography and environmental geoscience
Research Field:Palaeoclimatology
Objective Division:Environmental Policy, Climate Change and Natural Hazards
Objective Group:Understanding climate change
Objective Field:Climate variability (excl. social impacts)
UTAS Author:Curran, MAJ (Dr Mark Curran)
UTAS Author:Moy, AD (Dr Andrew Moy)
UTAS Author:van Ommen, TD (Dr Tas van Ommen)
UTAS Author:Vance, TR (Dr Tessa Vance)
ID Code:90529
Year Published:2014
Web of Science® Times Cited:183
Deposited By:CRC-Antarctic Climate & Ecosystems
Deposited On:2014-04-08
Last Modified:2017-10-30

Repository Staff Only: item control page