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Areal differentiation of snow cover in east central Ontario

Areal differentiation of snow cover in east central Ontario Vegetationally based patterns of snow depth, density, and water equivalent are identified by using snow course, grid, and unaligned random sample measurements. The limitations of extrapolations from point measurements to general characteristics of regional snow cover are discussed for an area in which midwinter melt is a feature of snow cover evolution. The snow cover of the vegetation zones was most distinct in terms of water equivalent and least distinct in terms of density. Measurements of depth proved to have a high predictive value for water equivalents. The validity of generalizations from point measurements, even in terms of quite coarse measures of snow cover characteristics, is limited in areas such as this to a short period following the time of measurement. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Water Resources Research Wiley

Areal differentiation of snow cover in east central Ontario

Water Resources Research , Volume 12 (6) – Dec 1, 1976

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References (7)

Publisher
Wiley
Copyright
Copyright © 1976 by the American Geophysical Union.
ISSN
0043-1397
eISSN
1944-7973
DOI
10.1029/WR012i006p01226
Publisher site
See Article on Publisher Site

Abstract

Vegetationally based patterns of snow depth, density, and water equivalent are identified by using snow course, grid, and unaligned random sample measurements. The limitations of extrapolations from point measurements to general characteristics of regional snow cover are discussed for an area in which midwinter melt is a feature of snow cover evolution. The snow cover of the vegetation zones was most distinct in terms of water equivalent and least distinct in terms of density. Measurements of depth proved to have a high predictive value for water equivalents. The validity of generalizations from point measurements, even in terms of quite coarse measures of snow cover characteristics, is limited in areas such as this to a short period following the time of measurement.

Journal

Water Resources ResearchWiley

Published: Dec 1, 1976

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