Research Article

Variability in snow accumulation patterns within forest stands on the interior plateau of British Columbia, Canada

  1. R. D. Winkler1,*,
  2. R. D. Moore2

Article first published online: 18 OCT 2006

DOI: 10.1002/hyp.6382

Issue

Hydrological Processes

Hydrological Processes

Special Issue: Canadian Geophysical Union — Hydrology Section

Volume 20, Issue 17, pages 3683–3695, 15 November 2006

Additional Information

How to Cite

Winkler, R. D. and Moore, R. D. (2006), Variability in snow accumulation patterns within forest stands on the interior plateau of British Columbia, Canada. Hydrol. Process., 20: 3683–3695. doi: 10.1002/hyp.6382

Author Information

  1. 1

    B.C. Ministry of Forests and Range, 515 Columbia St., Kamloops, B.C., Canada V2C 2T7

  2. 2

    Departments of Geography and Forest Resources Management, The University of British Columbia, 1984 West Mall, Vancouver, B.C., Canada V6T 1Z2

*B.C. Ministry of Forests and Range, 515 Columbia St., Kamloops, B.C., Canada V2C 2T7.

Publication History

  1. Issue published online: 18 OCT 2006
  2. Article first published online: 18 OCT 2006
  3. Manuscript Accepted: 29 NOV 2005
  4. Manuscript Received: 1 AUG 2005

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Keywords:

  • snow accumulation;
  • forest cover;
  • spatial analysis

Abstract

Previous research has highlighted the relationship between snow accumulation and forest stand characteristics, as well as the effects of topography, but not the variability within stands. This study examined spatial patterns in snow accumulation within forest stands, their consistency from year to year, and the extent to which they can be predicted from commonly used stand measurements.

Snow water equivalent (SWE) was measured on or near April 1, 1995 to 1997, and a forest inventory was completed at 64 points (15-m grid spacing) in each of nine stand types including mature and juvenile forests and clearcuts. Semivariograms revealed little evidence of spatial correlation among sample points, indicating that each sample could be considered statistically independent for analysis. Within the study stands, no strong spatial trends were evident through quadratic trend surface analysis. The within-stand coefficient of variation (CV) generally decreased with increasing mean accumulation. Spearman's rank correlation analysis and principal components analysis (PCA) indicated a weak to moderate similarity in snow accumulation patterns from year to year.

Site-scale canopy measures do not appear to provide a reliable basis for parameterizing the variability of within-stand snow deposition. Through the fitting of general linear models (GLM), year alone accounted for 33% of the variability in snow water equivalent within stands, on average. Of the stand inventory variables measured, crown closure explained the largest proportion of the variability in SWE within each stand, but together with year never more than 43%. The strongest correlations between snow water equivalent and crown closure were found in those stands exhibiting the greatest consistency in interannual spatial patterns of snow accumulation. Copyright © 2006 John Wiley & Sons, Ltd.

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