FGUS65 KSTR 061832 ESGUT National Weather Service Colorado Basin River Forecast Center Salt Lake City, Utah MAY 5, 2008 FLOOD POTENTIAL OUTLOOK UTAH Snowpack conditions across the Great Salt Lake region are above average in most locations for this time of year. Below average temperatures in April delayed the melt at middle and upper elevations. Low elevation snow, below 8000 feet is largely gone. Stream flow models are indicating less than a 10% chance of flood flows, however the potential for reaching bankfull is currently above average. Streams will most likely run high this spring and areas with small ungaged streams may see an elevated threat of bankfull or overbank conditions once the melt begins. The onset of conditions that will raise the threat of flooding will be monitored closely and this product will be updated as needed. Snowpack in the Duchesne basin is near average. Flood related problems due solely to snowmelt are not anticipated at this time. Mean daily flow from the model for points in the Duchesne Basin do not exceed flood flows. 50 percent exceedence flows also remain below the established bankfull stages. At this time, Spring flooding due to snowmelt is not anticipated in the Lower Green basin. While snowpack remains above average at some stations the model does not indicate any points going above flood flows or bankfull. Snow pack conditions in the Sevier River Basin have declined to 60% of seasonal peak. Above average snow melt peak flows are currently unlikely. The likelihood of snow melt driven flooding is less than 10%. A combination of rain upon high elevation snow during the next month may result in local flooding. The onset of such conditions will be monitored closely. There is no threat of flooding due solely to snowmelt in the Virgin River drainage. Much below average precipitation occurred in March and April. Snow remains at elevations above 9000 feet but it is limited in areal extent. For the latest information on peak flows in Utah and the Colorado Basins, please check our web page: http://www.cbrfc.noaa.gov/product/peak/peak.cgi B.Bernard, B. Reed, E.Clark, G.Smith $$