<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:creator>A.L. Kontis</dc:creator>
  <dc:date>2001</dc:date>
  <dc:description>The Variable-Recharge Package is a&#13;
computerized method designed for use with the&#13;
U.S. Geological Survey three-dimensional finitedifference&#13;
ground-water flow model&#13;
(MODFLOW-88) to simulate areal recharge to an&#13;
aquifer. It is suitable for simulations of aquifers in&#13;
which the relation between ground-water levels&#13;
and land surface can affect the amount and&#13;
distribution of recharge. The method is based on&#13;
the premise that recharge to an aquifer cannot&#13;
occur where the water level is at or above land&#13;
surface. Consequently, recharge will vary&#13;
spatially in simulations in which the Variable-&#13;
Recharge Package is applied, if the water levels&#13;
are sufficiently high. The input data required by&#13;
the program for each model cell that can&#13;
potentially receive recharge includes the average&#13;
land-surface elevation and a quantity termed&#13;
?water available for recharge,? which is equal to&#13;
precipitation minus evapotranspiration.&#13;
The Variable-Recharge Package also can&#13;
be used to simulate recharge to a valley-fill&#13;
aquifer in which the valley fill and the adjoining&#13;
uplands are explicitly simulated. Valley-fill&#13;
aquifers, which are the most common type of&#13;
aquifer in the glaciated northeastern United&#13;
States, receive much of their recharge from&#13;
upland sources as channeled and(or) unchanneled&#13;
surface runoff and as lateral ground-water flow.&#13;
Surface runoff in the uplands is generated in the&#13;
model when the applied water available for&#13;
recharge is rejected because simulated water&#13;
levels are at or above land surface. The surface&#13;
runoff can be distributed to other parts of the&#13;
model by (1) applying the amount of the surface&#13;
runoff that flows to upland streams (channeled&#13;
runoff) to explicitly simulated streams that flow&#13;
onto the valley floor, and(or) (2) applying the&#13;
amount that flows downslope toward the valley-&#13;
fill aquifer (unchanneled runoff) to specified&#13;
model cells, typically those near the valley wall.&#13;
An example model of an idealized valley-&#13;
fill aquifer is presented to demonstrate application&#13;
of the method and the type of information that can&#13;
be derived from its use. Documentation of the&#13;
Variable-Recharge Package is provided in the&#13;
appendixes and includes listings of model code&#13;
and of program variables. Comment statements in&#13;
the program listings provide a narrative of the&#13;
code. Input-data instructions and printed model&#13;
output for the package are included.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr00173</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Computer program for simulation of variable recharge with the U. S. Geological Survey modular finite-difference ground-water flow model (MODFLOW)</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>