Editorial Type:
Article
Article Type:
Research Article

The Influence of Blowing Snow and Precipitation on Snow Depth Change across the Ross Ice Shelf and Ross Sea Regions of Antarctica

Shelley L. Knuth Antarctic Meteorological Research Center, University of Wisconsin—Madison, Madison, Wisconsin

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Gregory J. Tripoli University of Wisconsin—Madison, Madison, Wisconsin

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Jonathan E. Thom Antarctic Meteorological Research Center, University of Wisconsin—Madison, Madison, Wisconsin

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George A. Weidner Antarctic Meteorological Research Center, University of Wisconsin—Madison, Madison, Wisconsin

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Print Publication:
01 Jun 2010
Collections:
International Precipitation Working Group (IPWG)
DOI:
https://doi.org/10.1175/2010JAMC2245.1
Page(s):
1306–1321
Restricted access

Abstract

Measuring snowfall in the polar regions is an issue met with many complications. Across the Antarctic, ground-based precipitation measurements are only available from a sparse network of manned stations or field studies. Measurements from satellites promise to fill in gaps in time and space but are still in the early stages of development and require surface measurements for proper validation. Currently, measurements of accumulation from automated reporting stations are the only available means of tracking snow depth change over a broad area of the continent. The challenge remains in determining the cause of depth change by partitioning the impacts of blowing snow and precipitation. While a methodology for separating these two factors has yet to be developed, by comparing accumulation measurements with meteorological measurements, an assessment of whether these terms were a factor in snow depth change during an event can be made. This paper describes a field study undertaken between January 2005 and October 2006 designed to identify the influences of precipitation and horizontal snow transport on surface accumulation. Seven acoustic depth gauges were deployed at automatic weather stations (AWS) across the Ross Ice Shelf and Ross Sea regions of Antarctica to measure net accumulation changes. From these measurements, episodic events were identified and were compared with data from the AWS to determine the primary cause of depth change—precipitation or horizontal snow transport. Information regarding the local impacts of these two terms, as well as climatological information regarding snow depth change across this region, is also provided.

Corresponding author address: Shelley L. Knuth, Antarctic Meteorological Research Center, University of Wisconsin—Madison, 1225 W. Dayton St., Madison, WI 53706. Email: shelley.knuth@colorado.edu

This article included in the International Precipitation Working Group (IPWG) special collection.

Abstract

Measuring snowfall in the polar regions is an issue met with many complications. Across the Antarctic, ground-based precipitation measurements are only available from a sparse network of manned stations or field studies. Measurements from satellites promise to fill in gaps in time and space but are still in the early stages of development and require surface measurements for proper validation. Currently, measurements of accumulation from automated reporting stations are the only available means of tracking snow depth change over a broad area of the continent. The challenge remains in determining the cause of depth change by partitioning the impacts of blowing snow and precipitation. While a methodology for separating these two factors has yet to be developed, by comparing accumulation measurements with meteorological measurements, an assessment of whether these terms were a factor in snow depth change during an event can be made. This paper describes a field study undertaken between January 2005 and October 2006 designed to identify the influences of precipitation and horizontal snow transport on surface accumulation. Seven acoustic depth gauges were deployed at automatic weather stations (AWS) across the Ross Ice Shelf and Ross Sea regions of Antarctica to measure net accumulation changes. From these measurements, episodic events were identified and were compared with data from the AWS to determine the primary cause of depth change—precipitation or horizontal snow transport. Information regarding the local impacts of these two terms, as well as climatological information regarding snow depth change across this region, is also provided.

Corresponding author address: Shelley L. Knuth, Antarctic Meteorological Research Center, University of Wisconsin—Madison, 1225 W. Dayton St., Madison, WI 53706. Email: shelley.knuth@colorado.edu

This article included in the International Precipitation Working Group (IPWG) special collection.

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Journal of Applied Meteorology and Climatology

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