THE SENSITIVITY OF SNOWMELT PROCESSES TO CLIMATE CONDITIONS AND FOREST COVER DURING RAIN-ON-SNOW - A CASE-STUDY OF THE 1996 PACIFIC-NORTHWEST FLOOD

A warm, very wet Pacific storm caused significant flooding in the Paci fic Northwest during February 1996. Rapid melting of the mountain snow cover contributed to this flooding. An energy balance snowmelt model is used to simulate snowmelt processes during this event in the Centra l Cascade Mountains of Oregon. Data from paired open and forested expe rimental sites at locations at and just below the Pacific Crest were u sed to drive the model, The event was preceded by cold, stormy conditi ons that developed a significant snow cover down to elevations as low as 500 m in the Oregon Cascades. At the start of the storm, the depth of the snow cover at the high site (1142 m) was 1.97 m with a snow wat er equivalent (SWE) of 425 mm, while at the mid-site (968 m) the snow cover was 1.14 m with a SWE of 264 mm. During the 5-6 day period of th e storm the open high site received 349 mm of rain, lost 291 mm of SWE and generated 640 mm of runoff, leaving only 0.22 m of snow on the gr ound. The mid-site received 410 mm of rain, lost 264 mm of SWE to melt and generated 674 mm of runoff, completely depleting the snow cover. Simulations at adjacent forested sites showed significantly less snowm elt during the event. The snow cover under the mature forest at the hi gh site lost only 44 mm of SWE during the event, generating 396 mm of runoff and leaving 0.69 m of snow. The model accurately simulated both snow cover depth and SWE during the development of the snow cover pri or to the storm, and the depletion of the snow cover during the event. This analysis shows that because of the high temperature, humidity an d relatively high winds in the open sites during the storm, 60-90% of the energy for snowmelt came from sensible and latent heat exchanges. Because the antecedent conditions extended the snow cover to very low elevations in the basin, snowmelt generated by condensation during the event made a significant contribution to the flood. Lower wind speeds beneath the forest canopy during the storm reduced the magnitude of t he turbulent exchanges at the snow surface, so the contribution of sno wmelt to the runoff from forested areas was significantly less, This e xperiment shows the sensitivity of snowmelt processes to both climate and land cover, and illustrates how the forest canopy is coupled to th e hydrological cycle in mountainous areas. (C) 1998 John Wiley & Sons, Ltd.