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452 Precipitation. Rainshadow. Rainshadow in westerly flow. Annual Precipitation. SW Olympic Slopes-Hoh Rain Forest: 150-170 inches yr -1. Sequim: roughly 15 inches per year. Puget Sound Convergence Zone. Progress in Precipitation Prediction in Terrain. NGM, 80 km, 1995. NGM, 1995.
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36-km 12-km
2007-2008 12-km UW MM5 Real-time 12-km WRF-ARW and WRF-NMM are similar December 3, 2007 0000 UTC Initial 12-h forecast 3-hr precip.
2007-2008 4-km MM5 Real-time
Smaller Scale Terrain Modulates Precipitation 10-km
12-km 4-km
Small-Scale Spatial Gradients in Climatological Precipitation on the Olympic Peninsula Alison M. Anders, Gerard H. Roe, Dale R. Durran, and Justin R. Minder Journal of Hydrometeorology Volume 8, Issue 5 (October 2007) pp. 1068–1081
Convective Precipitation • Need at least 2-4 km resolution to get most convection even half right. • If grid spacing is more coarse must have cumulus parameterization--Kain-Fritsch is used for MM5/WRF. • Convection is least skillful precipitation in virtually all models. • High resolution models can potentially give a heads on type of precipitation a day ahead (squall line, supercell, etc.)
Real-time WRF 4 km BAMEX Forecast Valid 6/10/03 12Z 4 km BAMEX forecast 36 h Reflectivity 4 km BAMEX forecast 12 h Reflectivity Composite NEXRAD Radar
Real-time 12 h WRF Reflectivity Forecast Valid 6/10/03 12Z 4 km BAMEX forecast 10 km BAMEX forecast 22 km CONUS forecast Composite NEXRAD Radar
Hurricane Isabel Reflectivity at Landfall 18 Sep 2003 1700 Z 41 h forecast from 4 km WRF Radar Composite
Most West Coast heavy precip events are associated with “atmospheric rivers”, a.k.a. the“Pineapple Express” A relatively narrow current of warm, moist air from the subtropics…often starting near or just north of Hawaii.
Associated with extraordinarily narrow filaments of moisture Precipitable Water From Mike Warner
November 6-9, 2006 Dark Green: about 20 inches
We know quite a bit about atmospheric rivers and heavy NW precipitation events, although there are still gaps in our knowledge
Synoptic Set-Up for Top Fifty Events at ForksCourtesy of Michael Warner
Extreme Precipitation Events • The current of warm, moist air associated with atmospheric rivers are found in the warm sector, parallel, near, and in front of the cold front. • Thus, atmospheric rivers are closely associated with the jet core and the region of large baroclinicity.
Orographic Enhancement • Upslope flow greatly increases precipitation rates on terrain. • Thus, wind speed and angle of attach can greatly modify the extreme nature of the precipitation.
Human Versus Objective Skill for Precipitation Forecasts: NWS Offices Around the US
Prob. Of Precip.– Cool Season(0000/1200 UTC Cycles Combined)
Brier Scores for Precipitation for all stations for the entire study period.
Brier Score for all stations, 1 August 2003 – 1 August 2004. 3-day smoothing is performed on the data.
Precipitation Brier Score for all stations, 1 August 2003 – 1 August 2004, sorted by geographic region.