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Wyoming Framework Water Plan - Living Rivers Home Page

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4.0 RESOURCES<br />

4.1 INTRODUCTION<br />

This chapter presents the physical characteristics (quantity and quality) of <strong>Wyoming</strong>’s surface<br />

water and groundwater. Regarding water quantity, the intent of the chapter is to characterize <strong>Wyoming</strong>’s<br />

total hydrologically available water supply irrespective of existing uses, institutional constraints, and<br />

visions for how water resources might be put to future beneficial use. In other words, this chapter<br />

provides estimates for the volume of water <strong>Wyoming</strong> must draw upon to sustain itself and future<br />

generations.<br />

The results described herein pertain to physical availability, which is to be distinguished from<br />

legal or permitted availability. Physical availability is important in assessing the viability of any future<br />

project, and lack of physical availability of water is an obvious fatal flaw for any water development.<br />

4.2 GENERAL<br />

<strong>Wyoming</strong> is a headwaters state, and<br />

precipitation is the source of most water in the<br />

state. Figure 4-1 presents mean precipitation<br />

rates. Approximately 68 million acre-feet per<br />

year 1 of precipitation joins 1.5 million acrefeet<br />

of surface inflows to create the total water<br />

resource. The basic hydrologic cycle is<br />

depicted in the margin graphic for a typical<br />

<strong>Wyoming</strong> river basin. Most of the<br />

precipitation will evaporate from the surface<br />

or be taken up and transpired by local<br />

vegetation. Figure 4-2 presents mean rates of<br />

potential evapotranspiration. Precipitation<br />

and snowmelt in excess of immediate<br />

demands will either run off (feeding rivers,<br />

streams, and lakes) or infiltrate to become<br />

groundwater. Approximately 15 million acrefeet<br />

per year of water become either surface or<br />

Hydrologic Cycle<br />

groundwater and thus available for use. This<br />

estimate is made up of the water that flows into the state plus the precipitation that runs off as streamflow<br />

or infiltrates as groundwater. Groundwater recharge will eventually return to the surface. Surface water<br />

will eventually evaporate to the atmosphere, completing the cycle. These two elements of the total water<br />

resource, surface water and groundwater, are the subject of the present report.<br />

1 13.07 inches per year mean annual statewide precipitation rate (<strong>Wyoming</strong> Climate Atlas, 2004).<br />

4-1

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