Wyoming Estimated Net Annual Aquifer Recharge

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Frequently-anticipated questions:


What does this data set describe?

    Title: Wyoming Estimated Net Annual Aquifer Recharge
    Abstract:
    This dataset represents an estimated representation of net annual recharge of surficial aquifers in Wyoming from natural sources. Irrigation or other man-made recharge structures are not represented. Estimated recharge is calculated using a simplistic formula based on soil type and average annual rainfall. The dataset is in raster format with 500 meter cell size.

    For more details about this dataset, please refer to this report:

    Hamerlinck, J.D. and Arneson, C.S., editors, 1998, Wyoming Ground-Water Vulnerability Assessment Handbook: Volume 1. Background, Model Development, and Aquifer Sensitivity Analysis: Spatial Data and Visualization Center Publication SDVC 98-01-1, University of Wyoming, Laramie, WY.

  1. How should this data set be cited?

    Larry C. Munn and Christopher S. Arneson, 1998, Wyoming Estimated Net Annual Aquifer Recharge: University of Wyoming Spatial Data and Visualization Center, Laramie, Wyoming.

    Online Links:

  2. What geographic area does the data set cover?

    West_Bounding_Coordinate: -111.26477012
    East_Bounding_Coordinate: -103.83670034
    North_Bounding_Coordinate: 44.99903411
    South_Bounding_Coordinate: 40.94837176

  3. What does it look like?

    <URL:http://www.sdvc.uwyo.edu/images/recharge.gif> (gif)
    500K Recharge

  4. Does the data set describe conditions during a particular time period?

    Calendar_Date: 1998
    Currentness_Reference: publication date

  5. What is the general form of this data set?

  6. How does the data set represent geographic features?

    1. How are geographic features stored in the data set?

      This is a Raster data set. It contains the following raster data types:

      • Dimensions 898 x 1172, type Grid Cell

    2. What coordinate system is used to represent geographic features?

      The map projection used is Lambert Conformal Conic.

      Projection parameters:
      Standard_Parallel: 33
      Standard_Parallel: 45
      Longitude_of_Central_Meridian: -107.5
      Latitude_of_Projection_Origin: 41
      False_Easting: 0.00000
      False_Northing: 0.00000

      Planar coordinates are encoded using coordinate pair
      Abscissae (x-coordinates) are specified to the nearest 1.0
      Ordinates (y-coordinates) are specified to the nearest 1.0
      Planar coordinates are specified in METERS

      The horizontal datum used is North American Datum of 1983.
      The ellipsoid used is GRS1980.
      The semi-major axis of the ellipsoid used is 6378137.
      The flattening of the ellipsoid used is 1/298.257.

  7. How does the data set describe geographic features?

    Entity_and_Attribute_Overview:
    This raster dataset is in floating point format, so it is not currently Associated with an attribute table. The values of the cells range from 0 to 49.487, the amount of water infiltrating to the water table per unit of area per unit of time (inches per year).

    Entity_and_Attribute_Detail_Citation: n/a


Who produced the data set?

  1. Who are the originators of the data set? (may include formal authors, digital compilers, and editors)

  2. Who also contributed to the data set?

  3. To whom should users address questions about the data?

    Chris Arneson
    Spatial Data and Visualization Center
    Box 4008 University Station
    Laramie, Wyoming 82071
    USA

    307-766-2735 (voice)
    arneson@uwyo.edu

    Hours_of_Service: 8:00 - 5:00 MST


Why was the data set created?

This layer was developed specifically to aid in the creation of a Wyoming ground-water vulnerability to surface contamination study conducted at the Wyoming Water Resources Center. The DRASTIC-based model requires surficial aquifer recharge as one of its parameters. This layer was specifically developed to aid in small-scale regional analysis within Wyoming and is not suitable for site specific analysis.


How was the data set created?

  1. From what previous works were the data drawn?

    soil data (source 1 of 2)
    L.C. Munn and C.S. Arneson, 1998, Soils of Wyoming: A Digital ARC/INFO Map at 1:500,000-Scale <URL:http://www.sdvc.uwyo.edu/clearinghouse/metadata/soil500k.html> .

    Type_of_Source_Media: digital map
    Source_Scale_Denominator: 500000
    Source_Contribution: recharge is percent of rainfall based on soils

    PRISM model (source 2 of 2)
    Chris Daly of PRISM Services, George Taylor of the Oregon Climate Se, 1997, Wyoming Average Annual Precipitation, 1961-1991, 2 km resolution <URL:http://www.sdvc.uwyo.edu/clearinghouse/metadata/prism.html>.

    Type_of_Source_Media: digital map
    Source_Contribution: recharge is percent of rainfall based on soils

  2. How were the data generated, processed, and modified?

    Date: 1997 (process 1 of 1)
    Net aquifer recharge refers to the volume of water that infiltrates into the soil and continues to percolate through the soil and unsaturated geologic material into the ground water. Recharge is expressed as an amount of water infiltrating to the water table per unit of area per unit of time (inches per year). Recharge represents a primary transport mechanism of potential contaminants from the ground surface into the aquifer. At modest recharge rates, the more water available to recharge, the more susceptible the ground water is to potential contamination. Note that there is a higher recharge rate where recharge begins to dilute contaminants, resulting in an inverse relationship between recharge and potential ground water contamination. Nevertheless, this dilution is not considered likely under natural conditions of the semi-arid Wyoming landscape (Knight 1994). Actual recharge values are poorly documented within much of Wyoming. Recharge values for this project were based on published percolation percentages for documented soil/vegetation combinations. Using this approach, several common themes are found within the body of scientific literature on this topic:

    1. recharge fraction (R/P) or percent of precipitation that reaches the uppermost aquifer, for a given environment increases as the depth to the water table decreases.

    2. recharge fraction increases as precipitation increases.

    3. recharge fraction increases as the sand and rock content of the soil increases.

    4. recharge fraction will be higher in an above average precipitation year and lower when precipitation is below average.

    5. seasonal pattern and occurrence of major events such as spring snowmelt alter the general effect of mean annual precipitation.

    In Soil Taxonomy (Soil Survey Staff, 1998), five moisture regimes are recognized in the soils of Wyoming. These are aquic, udic, ustic, xeric and aridic. The aquic regime has a high water table or a perched water table from an isolated surficial aquifer during at least part of the growing season. The udic regime is a leaching regime meaning precipitation exceeds evapotranspiration for a significant portion of the growing season. Soils with a udic regime commonly have a perched water table early in the spring following snowmelt. In the aridic regime evapotranspiration exceeds precipitation and soils are characterized by accumulations of secondary salts of varying solubility (CaCO3 , gypsum and more soluble salts). Recharge to the aquifer usually only occurs where the soils are very sandy (e.g. stabilized sand dunes) in soils along the banks of perennial streams with shallow water tables. The ustic and xeric moisture regimes are intermediate between aridic and udic regimes. The vegetation is primarily grassland, shrub land, or dry, open woodland. The ustic regime in Wyoming occurs typically where the precipitation varies between 30 cm and 45 cm/yr. The xeric regime is similar to the ustic regime except that precipitation is concentrated in the non-growing season. Soils in this regime can be as dry as aridic soils during the growing season but may be leached of salts by water accumulations in excess of the soils' winter water storage capacity.

    Using these generalizations, recharge percentages were estimated based on soil type and applied to the 1:500,000-Scale Soils Map of Wyoming (Munn and Arneson, 1998). Using these percentage values and average annual precipitation calculated by the PRISM model, a value of precipitation in inches can be calculated. Calculations were done in ARC/INFO's GRID module at a 500 meter cell resolution.

    Percentage Values used:

       WY01    36
       WY02    36
       WY03    40
       WY04    60
       WY05    40
       WY06    35
       WY07    30
       WY08    60
       WY09     1
       WY10    10
       WY11     1
       WY12     2
       WY13     2
       WY14     1
       WY15     2
       WY16     4
       WY17     1
       WY18     4
       WY19     1
       WY20    18
       WY21     1
       WY22    18
       WY23    12
       WY24     1
       WY25     4
       WY26     1
       WY27     5
       WY28    30
       WY29    50
       WY30    60
       WY31    38
       WY32    60
       WY33     2
       WY34     1
       WY35     1
       WY36     2
       WY37     1
       WY38     2
       WY39     1
       WY40     2
       WY41     6
       WY42     6
       WY43     1
       WY44     1
       WY45     6
    
    Citations:

    Knight, D.H. 1994. Mountains and Plains: the ecology of Wyoming landscapes. Yale University Press, New Haven.

    Soil Survey Staff, 1998. Keys to Soil Taxonomy. Eighth edition. USDA-NRCS. US Government Printing Office, Wash. D.C. 326 pp.

    Munn, L.C. and C.S. Arneson, 1998. Soils of Wyoming: A digital statewide map at 1:500,000-scale. Agricultural Experiment Station Report B-1069. University of Wyoming, College of Agriculture, Laramie, Wyoming.

  3. What similar or related data should the user be aware of?


How reliable are the data; what problems remain in the data set?

  1. How well have the observations been checked?

    see Process Steps

  2. How accurate are the geographic locations?

    see Process Steps

  3. How accurate are the heights or depths?

  4. Where are the gaps in the data? What is missing?

    All cells within the State of Wyoming are attributed.

  5. How consistent are the relationships among the observations, including topology?

    does not apply for raster data


How can someone get a copy of the data set?

Are there legal restrictions on access or use of the data?

Access_Constraints: none
Use_Constraints:
This data should not be used for analysis at a scale larger than 1:500,000. Because updates to this dataset or the attached metadata will occur without notice, this dataset may not be redistributed or repackaged in any form without the express written consent of the University of Wyoming Spatial Data and Visualization Center. Instead it is recommended that additional users download the most current version of the data from <http://www.sdvc.uwyo.edu/clearinghouse>.

  1. Who distributes the data set? (Distributor 1 of 1)

    SDVC Technical Coordinator
    Spatial Data and Visualization Center
    Box 4008 University Station
    Laramie, Wyoming 82071
    USA

    307-766-2532 (voice)
    n/a

  2. What's the catalog number I need to order this data set?

  3. What legal disclaimers am I supposed to read?

    The distributor shall not be held liable for improper or incorrect use of this data, based on the description of appropriate/inappropriate used described in this metadata document. The distributor makes no claims for the data's suitability for other purposes. It is strongly recommended that this data is directly acquired from the distributor described above and not indirectly through other sources which may have changed the data in some way.

  4. How can I download or order the data?


Who wrote the metadata?

Dates:
Last modified: Aug-1998

Metadata author:
Margo Berendsen
Box 4008 University Station
Laramie, Wyoming 82071
USA

307-766-2751 (voice)
meh@uwyo.edu

Metadata standard:
FGDC Content Standards for Digital Geospatial Metadata (FGDC-STD-001-1998)


This page is <http://www.wygisc.uwyo.edu/clearinghouse/metadata/rech500k.faq.html>
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