A doubling in snow accumulation in the western Antarctic Peninsula since 1850
Thomas, Elizabeth R. ORCID: https://orcid.org/0000-0002-3010-6493; Marshall, Gareth J. ORCID: https://orcid.org/0000-0001-8887-7314; McConnell, Joseph R.. 2008 A doubling in snow accumulation in the western Antarctic Peninsula since 1850. Geophysical Research Letters, 35 (1), L01706. 5, pp. 10.1029/2007GL032529
Full text not available from this repository. (Request a copy)Abstract/Summary
We present results from a new medium depth (136 metres) ice core drilled in a high accumulation site (73.59S,70.36W) on the south-western Antarctic Peninsula during 2007. The Gomez record reveals a doubling of accumulation since the 1850s, from a decadal average of 0.49 mweq y1 in 1855–1864 to 1.10 mweq y1 in 1997–2006, with acceleration in recent decades. Comparison with published accumulation records indicates that this rapid increase is the largest observed across the region. Evaluation of the relationships between Gomez accumulation and the primary modes of atmospheric circulation variability reveals a strong, temporally stable and positive relationship with the Southern Annular Mode (SAM). Furthermore, the SAM is demonstrated to be a primary factor in governing decadal variability of accumulation at the core site (r = 0.66). The association between Gomez accumulation and ENSO is complex: while sometimes statistically significant, the relationship is not temporally stable. Thus, at decadal scales we can utilise the Gomez accumulation as a suitable proxy for SAM variability but not for ENSO.
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | 10.1029/2007GL032529 |
Programmes: | BAS Programmes > Global Science in the Antarctic Context (2005-2009) > Antarctic Climate and the Earth System |
ISSN: | 0094-8276 |
Additional Keywords: | Snow accumulation; Southern Annular Mode; Antarctica |
NORA Subject Terms: | Meteorology and Climatology Glaciology |
Date made live: | 23 Jun 2008 10:48 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/3269 |
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