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Climate variability, snow, and physiographic controls on storm hydro graphs in small forested basins, western Cascades, OregonAuthor(s): Reed M. Perkins; Julia A. Jones
Source: Hydrologocal Processes, Vol. 22, p. 4949-4964
Publication Series: Scientific Journal (JRNL)
PDF: Download Publication (3.4 MB)
DescriptionLarge floods are often attributed to the melting of snow during a rain event. This study tested how climate variability, snowpack presence, and basin physiography were related to storm hydrograph shape in three small (<1 km2) basins with old-growth forest in western Oregon. Relationships between hydrograph characteristics and precipitation were tested for approximately 800 storms over a nearly 30-year period. Analyses controlled for (1) snowpack presence/absence, (2) antecedent soil moisture, and (3) hillslope length and gradient. For small storms (<150 mm precipitation), controlling for precipitation, the presence of a snowpack on near-saturated soil increased the threshold of precipitation before hydrograph rise, extended the start lag, centroid lag, and duration of storm hydrographs, and increased the peak discharge. The presence of a snowpack on near-saturated soil sped up and steepened storm hydrographs in a basin with short steep slopes, but delayed storm hydrographs in basins with longer or more gentle slopes. Hydrographs of the largest events, which were extreme regional rain and rain-on-snow floods, were not sensitive to landform characteristics or snowpack presence/absence. Although the presence of a snowpack did not increase peak discharge in small, forested basins during large storms it had contrasting effects on storm timing in small basins, potentially synchronizing small basin contributions to the larger basin hydrograph during large rain-on-snow events. By altering the relative timing of hydrographs, snowpack melting could produce extreme floods from precipitation events whose size is not extreme. Further work is needed to examine effects of canopy openings, snow pack, and climate warming on extreme rain-on-snow floods at the large basin scale.
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CitationPerkins, Reed M.; Jones, Julia A. 2008. Climate variability, snow, and physiographic controls on storm hydro graphs in small forested basins, western Cascades, Oregon. Hydrologocal Processes, Vol. 22, p. 4949-4964
Keywordsclimate, flooding, rain-on-snow, hydrograph, Oregon
- Extreme flood sensitivity to snow and forest harvest, western Cascades, Oregon, United States
- Precipitation-snowmelt timing and snowmelt augmentation of large peak flow events, western Cascades, Oregon
- An evaluation of the hydrologic relevance of lateral flow in snow at hillslope and catchment scales
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