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Victoria University Antarctic Research Expedition Science and Logistics Reports 2007-08: VUWAE 52

d. Results and discussions

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d. Results and discussions

Snow profile

The presence of summer hoar horizons and changes in density suggests that the 4m pit represents 13 years of accumulation.

Figure 3: Snow profiling at Evans Piedmont Glacier; a) Density and observations used to locate hoar horizons (A), fresh un-compacted snow (D), normal density snow (B) and ice/ hard layers (C); b) Stratigraphy of upper 2m section of the pit.

Figure 3: Snow profiling at Evans Piedmont Glacier; a) Density and observations used to locate hoar horizons (A), fresh un-compacted snow (D), normal density snow (B) and ice/ hard layers (C); b) Stratigraphy of upper 2m section of the pit.

AWS

The weather station has recorded data from the 15th Nov 2004 through to collection on the 3/12/2007. A problem with storage limits prevented continual data throughout 2005, but this was addressed by K049 during 2005/06 season. The record from Nov 2004 to Dec 2007 for air temperature, snow depth (i.e. accumulation changes), solar radiation, pressure and snow temperature is shown below (Fig. 4).

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Figure 4: Meteorological data collected at Evans Piedmont Glacier.

Figure 4: Meteorological data collected at Evans Piedmont Glacier.