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Climatology of Precipitation and Precipitation Extremes in the United States

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Title: Climatology of Precipitation and Precipitation Extremes in the United States


1
Climatology of Precipitation and Precipitation
Extremes in the United States
  • Greg Johnson
  • Applied Climatologist
  • USDA-NRCS
  • National Water and Climate Center
  • Portland, Oregon

2
Characteristics of the Mean Precipitation Climate
  • The principal controlling factors are the
    availability of atmospheric moisture and lifting
    mechanisms
  • Moisture controlled by flow from or proximity to
    large water bodies
  • Propensity for lifting influenced by topography,
    convergence zones (seabreeze, etc.), preferred
    storm tracks (jet dynamics)

3
Orographic Precipitation Enhancement Factors
  • Wind Direction (relative to topography)
  • Wind Speed
  • Atmos. Moisture (precipitable water)
  • Elevation Rise
  • Slope Angle

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Issues of Scale(Spatial and Temporal)
  • Over long averaging times (say, the 30 year
    normal maps), only the most important and
    consistent meteorological factors are evident
  • Progressively shorter time spans reveal
    ever-increasing nuances of the atmospheric system

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July normal Precipitation (top) versus
July 1993 Precipitation (bottom)
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Statistical Properties of Precipitation
  • Persistence, or lack thereof
  • Average amount of precipitation
  • Variability in precipitation amount, and
    theoretical maximum
  • Frequency of precipitation
  • Duration of precipitation

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Standardized PrecipitationIndex (SPI)
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A Spatial Climate Modeling System
  • PRISM (Parameter-elevation Regressions on
    Independent Slopes Model)
  • Statistical/Dynamical/Topographic approach
  • Uses point data, a DEM and a coordinated set of
    rules, decisions and calculations, designed to
    mimic an expert climatologist
  • For good reference see PRISM Guide Book under
    Technical Papers at the OSU PRISM web site

23
PRISM
  • Originally developed for precipitation only, now
    expanded to temperature, dewpoint, solar
    radiation and many derived variables such as
    HDDs/CDDs, GDDs, frost dates, snowfall, snow
    water equivalent, etc.
  • Most commonly applied in monthly or annual time
    increments, but also applied to events

24
PRISM Model from OSUsSpatial Climate Analysis
Service
  • Funded primarily by the NRCS-NWCC since 1993 for
    development of spatial climate products for the
    U.S.
  • Originally developed for precipitation only, now
    expanded to temperature, dewpoint, solar
    radiation and many derived variables such as
    HDDs/CDDs, GDDs, frost dates, snowfall, snow
    water equivalent, etc.
  • 4 km horizontal resolution raster data, and ARC
    polygon coverages both available
  • Most commonly applied in monthly or annual time
    increments, but also applied to events

25
PRISM
  • Any given grid cell value is determined by a
    linear regression of station values against
    elevation
  • Stations assigned weights
  • Combined weight of a station is a function of
    many factors

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SNOTEL
  • Large Automated Climate Network
  • Began in 1978
  • Over 650 remote site
  • Generally in high elevation areas
  • Located in the 12 Western States and Alaska
  • Utilizes meteor burst communication technology to
    telemeter data

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Typical SNOTEL Site
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SNOTEL Coverage
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PRISM-derived Products
  • Mean Mon. and Ann. Precipitation
  • Mean Mon. and Ann. Temps (mx/mn)
  • Frost dates and freeze-free season
  • Extreme winter min. temps probs.
  • Growing, heating, cooling degree days
  • Snow-water equivalent

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Avg. Ann. Precip. from UMAC web site
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Cartographic-quality Map of Mean Annual
Precipitation for Idaho Produced at the USDA-NRCS
NCGC
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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
  • 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 DEMs)
  • NRCS www.ftw.nrcs.usda.gov/prism/prism.html
  • (U.S., Regional and State mean annual
    precipitation cartographic products)

47
http//www.ftw.nrcs.usda.gov/prism/prism.html
  • Cartographic state mean annual precipitation
    maps
  • Full repository of official NRCS PRISM layers

48
PRISM Product Dissemination
  • Compact Discs
  • All precipitation layers for all of the U.S.
    3 CDs (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
  • 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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Precipitation Trend Analysis
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Precipitation Trends (in./decade)
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Extreme Precipitation Climatology
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Spatial Considerations
  • 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
  • Max24 2.62
  • Washington DC MAP 39.00
  • Max24 7.19

56
Reynolds Creek Watershed Idaho
  • Valley bottom MAP 11.14
  • 50 yr 1-hour value 1.18
  • Mountain top location MAP 43.58
  • 50 yr 1-hour value 1.26
  • Distance between stations 10 miles
  • Elevation difference 3500 feet

57
Example of Variations over Small Regions
Reynolds Creek, Idaho(values in mm
precipitation)
  • 10 Year Return
  • 3500 feet Atlas 2
    7000 feet Atlas 2
  • 30 min. 14 9 13 9
  • 1 hour 21 20 29 20
  • 24 hours 41 43 103 48
  • 50 Year Return
  • 30 min. 21 13 19 13
  • 1 hour 30 28 32 29
  • 24 hours 54 53 129 64

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Precipitation Frequency Definition
  • 100 - Year Event An event which has a 1
    percent chance of occurrence IN ANY YEAR NOT ONE
    event every 100 years.

61
Extreme Precipitation Climatology References
  • Technical Paper 40, Rainfall Frequency Atlas of
    the United States for Durations from 30 minutes
    to 24 Hours and Return Periods from 1 to 100
    Years (1961, 15.50).
  • NOAA Atlas 2, Precipitation Frequency Atlas of
    the Western United States, (1973).

62
Extreme Precipitation Climatology References
  • Technical Memorandum NWS Hydro 35, Five to
    60-minutes Precipitation Frequency for Eastern
    and Central United States (1977, 9.00)
  • Technical Paper 49, Two-to-Ten-Day Precipitation
    for Return Periods of 2 to 100 Years in the
    Contiguous United States (1964, 7.25)

63
Hydrometeorological Design Studies Center (HDSC)
of the NWShttp//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
65
50 Year, 6-hour NOAA Atlas 2 Values
(inches) Northwest Colorado
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100 Year, 24-hour NOAA Atlas 2 Values
(inches) Northwest Colorado
67
Ft. Collins CO Rainfall (in.), 530 -11 pm, July
28, 1997
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Probable Maximum Precipitation (PMP)
  • 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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