See also Description of Data Files.
Data are presented on the CAPS Version 1.0 CD-ROM as spreadsheets in MS-EXCEL (text only) and cover winter seasons 1983-84 to 1992-93.
Mr. Timothy Pangburn
U.S. Army Cold Regions Research and Engineering Laboratory
72 Lyme Road
Hanover, New Hampshire 03755-1290
Phone: (603) 646-4296
Fax: (603) 645 -4750
E-mail: Tim@rsgisc.crrel.usace.army.mil
Mr. William Roberts
U.S. Army Cold Regions Research and Engineering Laboratory
72 Lyme Road
Hanover, New Hampshire 03755-1290
Phone: (603) 646-4236
Fax: (603) 645 -4750
E-mail: wp
Sleepers River Research Watershed, Danville, Vermont.
Northwest Latitude: 44 31' 47" N
Northwest Longitude: 72 10' 37" W
Southeast Latitude: 44 25' 20"N
Southeast Longitude: 72 02' 22" W
The frost tube network is located within a 3.25 square mile sub-watershed of the Sleepers River Research Watershed. Tubes were positioned in forested and nonforested cover types. The forest cover includes beech, birch, maple hardwoods with a 7% slope and 240 degree aspect, mixed conifer (spruce and balsam) and hardwoods with a 3% slope and 240 degree aspect, and coniferous forest with a 3% slope and 240 degree aspect. The open areas include two large non-cultivated agricultural fields (with approximate 5% slopes and aspects of 240 and 15 degrees) and a small heavily instrumented opening. Site data were generally recorded weekly. Snow depth was measured with a metal meter ruler while frost reading were measured from a plastic tube filled with methylene blue dye suspended in a PVC outer tube.
The North Danville W-3 test site is located neat the eastern edge of a 6-ha clearing (see Anderson for a detailed site description). The forest is generally about 200 from the center of the selected site area. The surrounding first 75 m of terrain is generally free of vegetation tall enough to protrude above the midwinter snow cover. Beyond 75 m there are scattered small conifers. The central portion of the site was graded prior to the installation of instruments. The site is very flat, with a slight slope to the south, and meets site criteria given in the WMO report. This results in a very uniform snow cover over the site area. However, during windy periods the snow tends to blow off this area. The prevailing winds in winter are from a westerly direction.
Bates, R.E., Pangburn, T. and Greenan, H., 1987. WMO solid precipitation measurement intercomparison at Sleepers River Research Watershed. In: Eastern snow Conference, 44th, 3-4 June 1987, Fredericton, New Brunswick, Canada, Proceedings, p.1-7.
Roberts,W. 1991. Data Report for the period October 1990 to September 1991. U.S. Army Cold Regions Research and Engineering Laboratory, unpublished. [other unpublished reports by W. Roberts cover October - September of 1985-86 through 1989-90]
Water equivalence
Pangburn, T. and W. Roberts. 1998. Seasonal frost penetration, Sleepers River Research Watershed, Vermont, USA. In: International Permafrost Association, Data and Information Working Group, comp. Circumpolar Active-Layer Permafrost System (CAPS), version 1.0. CD-ROM available from National Snow and Ice Data Center, nsidc@kryos.colorado.edu. Boulder, Colorado: NSIDC, University of Colorado at Boulder.