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Automatic Weather Station established at Cape Hallett in the 2003/04 season
Gus McAllister/Rachel Brown Antarctica New Zealand:K002:03/04 |
Soil Biodiversity and Response to Climate Change: a Regional Comparison of Cape Hallett and Taylor Valley
An automated meteorological station (AWS) was established at Cape Hallett in December 2003 to collect data for the following parameters: barometric pressure, air and soil temperatures, relative humidity, photosynthetically active radiation (PAR), incoming and outgoing shortwave solar radiation, snow depth, and wind speed and direction. This AWS will complement existing stations in the McMurdo Dry Valleys as well as throughout the region and continent.
Samples were collected from a one meter snow pit and a six meter firn core in the accumulation zone of the Towles Glacier and analyzed for major ions (Cl-, SO42-, NO3-, Na+, K+, Mg2+, Ca2+) and oxygen and deuterium stable isotopes. Snow chemistry data will be used to reconstruct the short-term history of climate variation for temperature, snow accumulation rates as a proxy for precipitation, and Cl- and NO3- to estimate the intensity of marine legacies on salt and N deposition.
Contact: Thomas Nylen, Department of Geology, Portland State University, USA LTER Cape Hallett snowpit analysis LTER Cape Hallett AWS LTER (Long Term Ecological Research)
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