Note: This publication is currently undergoing major revisions. The current publication will be replaced with a new publication based on stakeholder requirements and scientific advances. We expect to begin sharing details on this soon. If you have input on content, format, or publication frequency at any time, please contact us at cbrfc.webmasters@noaa.gov.Virgin Water Supply Outlook, April 1, 2009

Virgin Water Supply Outlook, April 1, 2009


Prepared by G. Smith
NOAA, National Weather Service
Colorado Basin River Forecast Center
Salt Lake City, Utah
www.cbrfc.noaa.gov

Contents

Virgin Summary

Model Soil Moisture/Observed Streamflow - Dry weather in the late summer and fall created below average soil moisture conditions in the Virgin River Basin heading into the winter season. Below average streamflow has been observed throughout the winter months. Despite significant snow melt below the 8000 ft elevation level, March streamflow volumes were below to much below average.

Snowpack/Precipitation - Precipitation in the upper Virgin River Basin was near 40 percent of average for March. Seasonal precipitation is near 110 percent of average. While lower elevations below 8000 feet experienced snow melt, higher elevations experienced both losses and gains to the snowpack during March. Snowpack at the higher elevations as of April 1st ranged from 95 to 105 percent of average. The latest snowpack conditions can be found here: snowpack conditions.

General Discussion/Forecasts - Seasonal volume forecasts have been lowered from those issued in March. April through July runoff volumes are expected to range from 55 to 80 percent of average, which equates to 100 to 120 percent of the 1971-2000 median values.



*Median of forecasts within each basin.


Virgin Basin Conditions

Apr-Jul runoff volumes in the Virgin River Basin are expected to range from near 55 to 80 percent of the average (100 to 120 percent of median).



* Percent usable capacity, not percent average contents.
Click for multi-month Graph.



Differences between the full period forecasts and the residual forecasts may not exactly equal the actual observed volumes due to rounding conventions (see Definitions section).

Precipitation Maps








Hydrologist: G. Smith