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Winter precip far below normal

December 21, 2013
A late summer deluge soaked the Pacific Northwest, but precipitation has been considerably less than recent decades’ average ever since as the region heads into what is its all-important wintertime snow/water supply accumulation period, according to latest issue of the PNW Climate Impacts and Outlook produced by the Climate Impacts Resource Consortium.

And most sources say that predictions of near-term future precipitation are made more difficult because El Nino/Southern Oscillation signs are in a neutral phase.

“The majority of atmospheric and oceanic indicators used to monitor ENSO are well within the neutral range,” according to the December 17 ENSO update released by Australia’s Bureau of Meteorology. International climate models surveyed by the Bureau of Meteorology indicate the tropical Pacific is expected to remain neutral at least through to the first quarter of 2014.

ENSO is the major source of inter-annual climate variability in the Pacific Northwest, according to the University of Washington’s Climate Impacts Group. ENSO variations are more commonly known as El Niño (the warm phase of ENSO) or La Niña (the cool phase of ENSO).

An El Niño is characterized by stronger than average sea surface temperatures in the central and eastern equatorial Pacific Ocean, reduced strength of the easterly trade winds in the Tropical Pacific, and an eastward shift in the region of intense tropical rainfall.

A La Niña is characterized by the opposite – cooler than average sea surface temperatures, stronger than normal easterly trade winds, and a westward shift in the region of intense tropical rainfall. Average years, i.e., years where there is no statistically significant deviation from average conditions at the equator, are called ENSO-neutral

El Niño winters tend to be warmer and drier than average with below normal snowpack and streamflow, according to CIG.

La Niña winters seem to tilt the odds toward cooler and wetter than average winters with above normal snowpack and streamflow.

Similar to precipitation, there are equal chances of above, below, or normal temperatures across the Pacific Northwest, as estimated in the most recent NOAA’s Climate Prediction Center’s three-month forecast. That December-February forecast is for a slightly higher than equal chance for above average precipitation during the period across much of Montana.

The CPC winter “outlook” for the United States can be found at:
http://www.noaanews.noaa.gov/stories2013/20131121_winteroutlook.html.

September 2013 was the wettest on record in the Pacific Northwest (Oregon, Washington, and Idaho), with a regional average of 3.68 inches (2.47 inches above the 20th century average). In late September, remnants of Typhoon Pabuk soaked western Oregon and Washington, according to the CIRC newsletter.

A ridge built into the region, making for an abnormally dry start to the water year, which runs from October 1 to September 30, especially in southern Oregon, the Snake River Valley, and eastern Washington’s Palouse. October to November 2013 was the 12th driest such period on record, according to the CIRC.

The regionally averaged total of 3.18 inches was 2.70 inches below the 20th century average, and the driest since 2002.

According to the NOAA National Weather Service’s Northwest River Forecast Center, precipitation in the area upstream of the lower Snake’s Ice Harbor Dam was only 49 percent of its average for this month through December 16.

Precipitation in that Snake River part of the Columbia basin was 38 percent of average in October and 48 percent of average in November.

Upper Columbia precipitation – above central Washington’s Grand Coulee Dam – was also low at 70 percent of average during the first 16 days of December, following 24 percent of average in October and 86 percent of average in November.

The area upstream of the lower Columbia’s The Dalles Dam, which includes the Snake and mid and upper Columbia, was 57 percent of average December 1 to 16; 30 percent of average in October and 63 percent of average in November.

The NWRFC’s first official water supply forecast for next spring and summer is scheduled for release in early January.

The Pacific Northwest Climate Impacts Research Consortium delivers science, information, and tools to decision makers responsible for the management of resources and services in a changing climate. It is housed in the Oregon Climate Change Research Institute at Oregon State University. The team consists of experts from Oregon State University, the University of Oregon, the University of Idaho, Boise State University, and the University of Washington. CIRC is funded by the National Oceanic and Atmospheric Administration..

You can find the latest issue of the PNW Climate Impacts and Outlook on the new CIRC website: http://pnwcirc.org/wp-content/uploads/2013/12/circfall_final.pdf.
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