An Arctic and Antarctic perspective on recent climate change

Turner, John ORCID: https://orcid.org/0000-0002-6111-5122; Overland, James E.; Walsh, John E.. 2007 An Arctic and Antarctic perspective on recent climate change. International Journal of Climatology, 27 (3). 277-293. 10.1002/joc.1406

Full text not available from this repository. (Request a copy)

Abstract/Summary

We contrast recent climatic and environmental changes and their causes in the Arctic and the Antarctic. There are continuing increases in surface temperatures, losses of sea ice and tundra, and warming of permafrost over broad areas of the Arctic, while most of the major increase in Antarctic temperatures is on the Antarctic Peninsula associated with sea ice loss in the Bellingshausen-Amundsen Seas sector. While both natural atmospheric and oceanic variability, and changes in external forcing including increased greenhouse gas concentrations, must be considered in the quest for understanding such changes, the interactions and feedbacks between system components are particularly strong at high latitudes. For the 1950s to date in the Arctic and for 1957 to date in the Antarctic, positive trends in large-scale atmospheric circulation represented by the Arctic oscillation (AO) and Antarctic oscillations (AAO) and the Pacific North American (PNA) pattern contribute to the long-term temperature trends. However, continuing Arctic trends during the last decade of near neutral AO will require alternate explanations. The trend in the AAO since 1950 is larger than expected from natural variability and may be associated with the decrease in stratospheric ozone over Antarctic. The persistence shown in many Arctic and Antarctic Peninsula components of climate and their influence through possible feedback supports continuation of current trends over the next decade. One can expect large spatial and temporal differences, however, from the relative contributions of intrinsic variability, external forcing, and internal feedback/amplifications. It is particularly important to resolve regional feedback processes in future projections based on modeling scenarios.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1002/joc.1406
Programmes:	BAS Programmes > Global Science in the Antarctic Context (2005-2009) > Antarctic Climate and the Earth System
ISSN:	0899-8418
NORA Subject Terms:	Meteorology and Climatology Atmospheric Sciences
Date made live:	27 May 2008 08:49 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/3105

Actions (login required)

View Item

Document Downloads

More statistics for this item...