California, Arizona and New Mexico as well as parts of Colorado, Utah and Nevada are experiencing prolonged drought, focusing attention again on the winter snowfall.
"Right now, snowpack and streamflow forecasts look pretty close to normal for much of the West," NWCC hydrologist Cara McCarthy said. "A couple of major regional exceptions are the Southwest and California, which are unusually dry, once again."
In Western states where snowmelt accounts for the majority of seasonal water supply, information about snowpack serves as an indicator of future water availability. Streamflow in the West consists largely of accumulated mountain snow that melts and flows into streams as temperatures warm in spring and summer. NWCC scientists analyze the snowpack, air temperature, soil moisture and other measurements taken from remote sites to develop the water supply forecasts.
Overall, the basins of the Missouri, Colorado and Columbia rivers are expected to receive near-normal streamflows.
In the Pacific Northwest, although rainfall during the fall months has been above average, the current snowpack is far below normal because of higher than normal temperatures.
"This is just the first forecast of the season; everything can change," McCarthy said. "A weak El Niño is forecast for this year, which might play a part in coming months."
Although variable, El Niño conditions tend to deliver more than normal winter precipitation to the Southwest and less to the Pacific Northwest.
The NWCC, part of the USDA's Natural Resources Conservation Service, monitors conditions year-round and will continue to issue monthly forecasts until June. The water supply forecast is part of several USDA efforts to improve public awareness and mitigate the impacts of climate change, including drought and other extreme weather events.
Since 1939, the USDA has conducted snow surveys and issued regular water supply forecasts. Other resources on drought include the U.S. Drought Monitor. You can also view forecast information by state. 
—From USDA news release
