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Please use this identifier to cite or link to this item: http://bura.brunel.ac.uk/handle/2438/6032

Title: An examination of the precipitation delivery mechanisms for Dolleman Island, eastern Antarctic Peninsula
Authors: Russell, A
Mcgregor, GR
Marshall, GJ
Keywords: Antarctic peninsula
ECMWF re-analysis
Backwards air trajectories
Precipitation
Publication Date: 2004
Publisher: Wiley-Blackwell
Citation: Tellus. Series A: Dynamic Meteorology and Oceanography, 56(5): 501 - 513, Oct 2004
Abstract: The variability of size and source of significant precipitation events were studied at an Antarctic ice core drilling site: Dolleman Island (DI), located on the eastern coast of the Antarctic Peninsula. Significant precipitation events that occur at DI were temporally located in the European Centre for Medium-Range Weather Forecasting (ECMWF) reanalysis data set, ERA-40. The annual and summer precipitation totals from ERA-40 at DI both show significant increases over the reanalysis period. Three-dimensional backwards air parcel trajectories were then run for 5 d using the ECMWF ERA-15 wind fields. Cluster analyses were performed on two sets of these backwards trajectories: all days in the range 1979–1992 (the climatological time-scale) and a subset of days when a significant precipitation event occurred. The principal air mass sources and delivery mechanisms were found to be the Weddell Sea via lee cyclogenesis, the South Atlantic when there was a weak circumpolar trough (CPT) and the South Pacific when the CPT was deep. The occurrence of precipitation bearing air masses arriving via a strong CPT was found to have a significant correlation with the southern annular mode (SAM); however, the arrival of air masses from the same region over the climatological time-scale showed no such correlation. Despite the dominance in both groups of back trajectories of the westerly circulation around Antarctica, some other key patterns were identified. Most notably there was a higher frequency of lee cyclogenesis events in the significant precipitation trajectories compared to the climatological time-scale. There was also a tendency for precipitation trajectories to come from more northerly latitudes, mostly from 50–70°S. The El Niño Southern Oscillation (ENSO) was found to have a strong influence on the mechanism by which the precipitation was delivered; the frequency of occurrence of precipitation from the east (west) of DI increased during El Niño (La Niña) events.
Description: Copyright @ 2004 Wiley-Blackwell
URI: http://bura.brunel.ac.uk/handle/2438/6032
DOI: http://dx.doi.org/10.1111/j.1600-0870.2004.00081.x
ISSN: 0280-6495
Appears in Collections:Institute for the Environment Research Papers
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