3 December, 2000
Logging the Shallow Holes
The primary goal of the project is to obtain precise temperature data from the surface to the base of the ice sheet. With this information Gary Clow will be able to reconstruct the climate history for about the last five thousand years. Most of the data comes from the main borehole, which reaches down 1000 meters (3280ft) to the bedrock. Most of this hole is filled with fluid. However, above the ice is about 70 meters of firn. In this layer the pore spaces are interconnected so it won't hold fluid. Reliable temperatures cannot be taken in this air-filled portion of the borehole.
To obtain temperature data for the top portion of the ice sheet, four shallower holes were drilled last year. These 12 cm (5 in) holes are between 160 and 200 meters (525-656 ft) deep. They were lined with pipe and filled with fluid up to the surface. The four holes are located along a line stretching 10 km north and 32 km south of the main drill site. Logging these holes will provide climate data for the last 50 to 100 years. The data will also provide information about climate variability between the four sites during that time period.
The weather at Siple Dome has been great for the last five days. Sun and light winds have been the rule. This has allowed the two science teams using the Twin Otter to fly to all their sites. Demetri Capetanopoulos and Shannon Jackson were able to download data from their three GPS sites in the coastal mountains north of here. This data will provide information about the activity of plate tectonics in the region. It also will gauge the rate of uplift as the continent rebounds from the thicker ice cover that was present during the last ice age.
Their work being completed, these people are leaving for McMurdo Station today. That will reduce the population of camp by six down to a total of ten people. It will be nice to have some more space in the beaker hut, but I will miss having those folks around.
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