Streamflow, water-temperature, and specific-conductance data for selected streams draining into Lake Fryxell, lower Taylor Valley, Victoria Land, Antarctica, 1990-92

Abstract

During the 1990-91 and 1991-92 field seasons in Antarctica, streamflow, water-temperature, and specific-conductance data were collected on 11 streams draining into Lake Fryxell. Lake Fryxell, which is permanently ice covered, is situated in a closed basin. Continuous streamflow data were collected at eight sites, and periodic streamflow measurements were made at three sites. Continuous water-temperature and specificconductance data were collected at seven sites, and periodic water-temperature and specificconductance data were collected at all sites.