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ACTIVE LAYER MONITORING METADATA FORM

Return (by mail, e-mail or fax) to Sharon Smith

Geological Survey of Canada, 601 Booth St. Ottawa, Ontario K1A 0E8

Email: ssmith@nrcan.gc.ca

Fax: 613 992 0190

This form is currently in use for the Circumpolar Active Layer Monitoring (CALM) component of the Global Terrestrial Network for Permafrost

Site name: Marmot Basin 1, Jasper National Park

Site history (Year Started): 1979

Responsible individual(s) and address of organization for data collection including email and fax addresses: S. A. Harris

Latitude and longitude: 52°47'52.8"N            118°07'2.0"W

Elevation above sea level(m): 2286m

Slope and aspect of site(s): 0°

Landform or geomorphological description of area occupied by site(s): Ridge top trending NNE-SSW

Predominant texture of soil (sand, gravel, peat, etc.): Fractured bedrock

Vegetation classification (dominant, vegetation type, percentage of vegetation, bare ground, etc.): Alpine tundra -1% vegetation cover

Method used to determine active layer thickness: Interpolation of ground temperature profile

Information on permanent temperature and/or moisture installations(probes, recorders, depth of sensors, depth of permafrost boreholes, etc.); if possible provide annual values (or ranges) of these data: Air temperature has been measured along with relative humidity (for some years). Originally the data was collected manually, but data loggers have been used since 1992

Name and location (lat./long.) of closest climate station; provide separately mean monthly air temperatures and snow depth as available for years of active layer data: Snowfall is measured at the middle Chalet, Marmot Basin

Relevant publications (complete citation, use additional space):

"Permafrost Distribution Along the Rocky Mountains in Alberta" (with the late R.J.E. Brown).1982. The Roger J. E. Brown Memorial Volume, Proceedings of the 4th Canadian Permafrost Conference, Calgary, Alberta, H.M. French, Ed. National Research Council, Ottawa, pp.59-67.

"Permafrost Distribution, Zonation, and Stability Along the Eastern Ranges of the Cordillera of North America", Arctic, vol. 39, 1986, 29-38.

"Distribution and Zonation of Permafrost Along the Eastern Ranges of the Cordillera of North America", Biuletyn Peryglacjalny, vol. 31, 1986, 107-118.

"Continentality Index: Its Uses and Limitations When Applied to Permafrost in the Canadian Cordillera", Journal of Physical Geography, vol. 10, 1989, 268-282.

"Long-Term Air and Ground Temperature Records From the Canadian Cordillera", Proc. 5th Canadian Permafrost Conference. National Research Council of Canada. Universite Laval, Collection Nordicana #54, 1990, pp. 151-157.

"Heat Transfer Processes at the Lower Limit of Alpine Permafrost, Marmot Basin, Jasper National Park, Canada". Biuletyn Peryglacjalny, vol. 38, 1999, 73-93.

"Twenty years of data on climate-permafrost-active layer variations at the lower limit of alpine permafrost, Marmot Basin, Jasper National Park, Canada." Geografiska Annaler, vol. 83A, 2001, pp.1-13.

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Last Updated: 2006-12-14