Improving ice core interpretation using in situ and reanalysis data

Thomas, E.R. ORCID: https://orcid.org/0000-0002-3010-6493; Bracegirdle, T.J. ORCID: https://orcid.org/0000-0002-8868-4739. 2009 Improving ice core interpretation using in situ and reanalysis data. Journal of Geophysical Research, 114 (D2), D20116. 8, pp. 10.1029/2009JD012263

Before downloading, please read NORA policies.

Preview

Text (Copyright American Geophysical Union) 2009JD012263.pdf - Published Version Download (432kB)

Abstract/Summary

Back trajectory analysis, provided by the British Atmospheric Data Centre using meteorological parameters from the European Centre for Medium-Range Weather Forecasts (ECMWF) reanalysis ERA-40 (1980-2001) and operational analysis (2002-2006), is used to investigate transport pathways and source regions of climate proxies preserved in a new ice core (Gomez) from the southwestern Antarctic Peninsula. The ECMWF data are compared with automatic weather station data and ice core annual accumulation records to demonstrate that the ECMWF data capture a large proportion of the annual and subseasonal precipitation variability at the site. The back trajectories reveal that precipitation preserved in the ice core accumulation record, and hence climate proxies contained therein, originate from the low-pressure systems from the Bellingshausen Sea transported via circumpolar westerly winds. Hence, precipitation-dependent ice core proxies, such as isotopic composition, will be influenced by both localized sea ice extent and large-scale circulation changes, such as the Southern Annular Mode. Sea ice proxies from the ice core are expected to be dominated by sea ice extent in the Bellingshausen Sea but also influenced by sea ice in the Weddell Sea, with a small proportion of air mass trajectories originating from this region during the summer. Comparison with other ice core sites reveals a stronger influence of easterly transport at more northerly locations, thus explaining the observed differences in snow accumulation records between ice cores and the poor correlation with instrumental records at these sites.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1029/2009JD012263
Programmes:	BAS Programmes > Polar Science for Planet Earth (2009 - ) > Climate
ISSN:	0148-0227
NORA Subject Terms:	Meteorology and Climatology Glaciology
Date made live:	12 Nov 2010 15:18 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/11313

Actions (login required)

View Item

Document Downloads

More statistics for this item...