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Climatology of Precipitation and Precipitation Extremes in the United States Greg Johnson Applied Climatologist USDA-NRCS National Water and Climate Center Portland, Oregon RFC Hydromet 01-1 14-21 November 2000
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Characteristics of the Mean Precipitation Climate n The principal controlling factors are the availability of atmospheric moisture and lifting mechanisms n Moisture controlled by flow from or proximity to large water bodies n Propensity for lifting influenced by topography, convergence zones (seabreeze, etc.), preferred storm tracks (jet dynamics)
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Orographic Precipitation Enhancement Factors n Wind Direction (relative to topography) n Wind Speed n Atmos. Moisture (precipitable water) n Elevation Rise n Slope Angle
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Issues of Scale (Spatial and Temporal) n Over long averaging times (say, the 30 year normal maps), only the most important and consistent meteorological factors are evident n Progressively shorter time spans reveal ever-increasing nuances of the atmospheric system
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A Snapshot in Time
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24 Hour Time Integration
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July normal Precipitation (top) versus July 1993 Precipitation (bottom)
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Statistical Properties of Precipitation n Persistence, or lack thereof n Average amount of precipitation n Variability in precipitation amount, and theoretical maximum n Frequency of precipitation n Duration of precipitation
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Annual Mean of Wet-Dry Day Prob. (x1000), Southwest Idaho
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A Spatial Climate Modeling System n PRISM (Parameter-elevation Regressions on Independent Slopes Model) n Statistical/Dynamical/Topographic approach n Funded primarily by the NRCS-NWCC since 1993 for development of spatial climate products for the U.S. n Developed by Dr. Chris Daly of the Spatial Climate Analysis Service, Oregon State University
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What is PRISM?
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PRISM n Grid based model, approx. 4 km horiz. resolution n Any given grid cell value is determined by a linear regression of station values against elevation n Stations assigned weights n Combined weight of a station is a function of many factors
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Form of Grid Cell Prediction n Y = 1 X + 0, where Y is the predicted climate element and X is the DEM elevation at the target cell. 0 and 1 are regression slope and intercept, and are determined by x,y pairs of elevation and climate observations from nearby climate stations where Y is the predicted climate element and X is the DEM elevation at the target cell. 0 and 1 are regression slope and intercept, and are determined by x,y pairs of elevation and climate observations from nearby climate stations
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Station Weighting n Combined weight of a station is: W = f {W d, W z, W c, W l, W f, W p, W e }, where W d, W z, W c, W l, W f, W p, W e are the distance, elevation, cluster, vertical layer, topographic facet, coastal proximity and effective terrain height weights. where W d, W z, W c, W l, W f, W p, W e are the distance, elevation, cluster, vertical layer, topographic facet, coastal proximity and effective terrain height weights.
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Vermont Annual Precipitation
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Olympic Mtns Terrain
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Olympic Mtns Annual Precipitation Facets On + Vertical Extrapolation On Inches
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Olympic Mtns Annual Precipitation Facets On + Vertical Extrapolation Off Inches
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Olympic Mtns Annual Precipitation Facets Off + Vertical Extrapolation Off Inches
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Olympic Mtns Annual Precipitation No elevation Inches
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Olympic Mtns Annual Precipitation Facets On + Vertical Extrapolation On Inches
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Hawaii Annual Precipitation No Layer Weighting
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Hawaii Annual Precipitation Two Layers
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SNOTEL Coverage
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PRISM-derived Products n Mean Mon. and Ann. Precipitation n Mean Mon. and Ann. Temps (mx/mn) n Frost dates and freeze-free season n Extreme winter min. temps & probs. n Growing, heating, cooling degree days n Snow-water equivalent
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Oregon Annual Precipitation
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Annual Precipitation Map of Elmore County, Idaho Produced by the NRCS NCGC “Cut-out” of State Map
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PRISM - SWE Map - Oregon
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PRISM Product Dissemination n Web Sites: OSU: www.ocs.orst.edu/prism/prism_new.html (Raster and polygon coverages of practically everything produced to date (Arc, GRASS); documentation; metadata; DEM’s) NRCS: www.ftw.nrcs.usda.gov/prism/prism.html (U.S., Regional and State mean annual precipitation cartographic products)
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http://www.ftw.nrcs.usda.gov/prism/prism.html: Cartographic state mean annual precipitation maps Cartographic state mean annual precipitation maps Full repository of “official” NRCS PRISM layers
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PRISM Product Dissemination n Compact Discs: All precipitation layers for all of the U.S. 3 CD’s (East, Central, West) of the lower 48 states. Includes Arc Explorer viewing software, and all documentation. Available from the NRCS-NCGC: 800-672-5559
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PRISM Product Dissemination n Hardcopy maps: Cartographic-quality, walls-size maps of mean annual precipitation for each state Available from the NRCS Climate Data Liaison in each state
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Extreme Precipitation Climatology
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Spatial Considerations n Means and extremes are not always correlated, especially over large spatial domains, or even in small regions with significant climate variations: Portland OR MAP 37.39” Portland OR MAP 37.39” Max24 2.62” Max24 2.62” Washington DC MAP 39.00” Washington DC MAP 39.00” Max24 7.19” Max24 7.19”
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Elevational Effect: Reynolds Creek Watershed Idaho n Valley bottom: MAP: 11.14” 50 yr 1-hour value: 1.18” 50 yr 1-hour value: 1.18” n Mountain top location: MAP: 43.58” 50 yr 1-hour value: 1.26” 50 yr 1-hour value: 1.26” Distance between stations: 10 miles Elevation difference: 3500 feet Elevation difference: 3500 feet
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Example of Variations over Small Regions: Reynolds Creek, Idaho (values in mm precipitation): n 10 Year Return n 3500 feet Atlas 2 7000 feet Atlas 2 n 30 min.14 913 9 n 1 hour21202920 n 24 hours414310348 n n 50 Year Return n 30 min.21131913 n 1 hour 30283229 n 24 hours545312964
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Geographic Effect on Extreme vs. Mean Precipitation
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Precipitation Frequency Definition n 100 - Year Event: “An event which has a 1 percent chance of occurrence IN ANY YEAR; NOT ONE event every 100 years.”
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Hydrometeorological Design Studies Center (HDSC) of the NWS: http://www.nws.noaa.gov/oh/hdsc/index. html
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TP-40 100 Yr 24-hour pcpn. (in.) from SCS TR-55, 1986
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100 Year, 24-hour NOAA Atlas 2 Values (inches) Northwest Colorado
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Probable Maximum Precipitation (PMP) n “Theoretically, the greatest depth of precipitation for a given duration that is physically possible over a given size storm area at a particular geographical location at a certain time of the year.”
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Storm Characteristics
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