11.3: Water Use and Distribution

In the United States, 355 billion gallons (1344 billion liters) of ground and surface water are used each day, of which 76 billion gallons (288 billion liters) are fresh groundwater. The state of California accounts for 16% of national groundwater [8].

Figure \(\PageIndex{1}\): Agricultural water use in the United States by state.

Utah is the second driest state in the United States behind its neighbor Nevada, having a mean statewide precipitation of 12.2 inches (31 cm) per year. Utah also has the second-highest per capita rate of total domestic water use [8] of 167 gallons (632.16 liters) per day per person. With the combination of relatively high demand and limited quantity, Utah is at risk for water budget deficits.

Figure \(\PageIndex{2}\): Trends in water use by source.

Surface Water Distribution

Fresh water is a precious resource and should not be taken for granted, especially in dry climates. Surface water makes up only 1.2% of the fresh water available on the planet, and 69% of that surface water is trapped in ground ice and permafrost. Stream water accounts for only 0.006% of all fresh water and lakes contain only 0.26% of the world’s fresh water [9].

Global circulation patterns are the most important factor in distributing surface water through precipitation. Due to the Coriolis effect and the uneven heating of the Earth, air rises near the equator and near 60° north and south latitude. Air sinks at the poles and 30° north and south latitude. Land masses near rising air are more prone to humid and wet climates. Land masses near sinking air, which inhibits precipitation, are prone to dry conditions [10; 11]. Prevailing winds, ocean circulation patterns such as the Gulf Stream’s effects on eastern North America, rain shadows (dry leeward sides of mountains), and even the proximity of bodies of water can affect local climate patterns. For example, when cold winds blow across the relatively warm Great Salt Lake, the air warms, which causes it to pick up moisture. This local increase in the moisture content of the air may eventually fall as snow or rain on nearby mountains, a phenomenon known as “lake-effect precipitation” [12].

In the United States, the 100th Meridian roughly marks the boundary between the humid and arid parts of the country. Growing crops west of the 100th Meridian requires irrigation [13]. In the west, surface water is stored in reservoirs and mountain snowpacks [14], then strategically released through a system of canals during times of high use.

Figure \(\PageIndex{3}\): Distribution of precipitation in the United States. The 100th Meridian is approximately where the average precipitation transitions from relatively wet to dry. (Source: U.S. Geological Survey)

Some of the driest parts of the western United States are in the Basin and Range Province. The Basin and Range has multiple mountain ranges that are oriented north to south. Most of the basin valleys in the Basin and Range are dry, receiving less than 12 inches (30 cm) of precipitation per year. However, some of the mountain ranges can receive more than 60 inches (1.52 m) of water as snow or snow-water-equivalent. The snow-water equivalent is the amount of water that would result if the snow were melted, as the snowpack is generally much thicker than the equivalent amount of water that it would produce [12].

Groundwater Distribution

Groundwater makes up 30.1% of the fresh water on the planet, making it the most abundant reservoir of fresh water accessible to most humans. The majority of fresh water, 68.7%, is stored in glaciers and ice caps as ice [9]. As the glaciers and ice caps melt due to global warming, this fresh water is lost as it flows into the oceans.

Table \(\PageIndex{1}\): Groundwater distribution on Earth.

Water source	Water volume (cubic miles)	Freshwater (%)	Total water (%)
Oceans, seas, & bays	321,000,000	—	96.5%
Ice caps, glaciers, & permanent snow	5,773,000	68.7%	1.74%
Groundwater (total)	5,614,000	—	1.69%
Groundwater (fresh)	2,526,000	30.1%	0.76%
Groundwater (saline)	3,088,000	—	0.93%
Soil moisture	3,959	0.05%	0.001%
Ground ice & permafrost	71,970	0.86%	0.022%
Lakes (total)	42,320	—	0.013%
Lakes (fresh)	21,830	0.26%	0.007%
Lakes (saline)	20,490	—	0.006%
Atmosphere	3,095	0.04%	0.001%
Swamp water	2,752	0.03%	0.0008%
Rivers	509	0.006%	0.0002%
Biological water	269	0.003%	0.0001%
Source: Igor Shiklomanov’s chapter “World freshwater resources” in Peter H. Gleick (editor), 1993, Water in Crisis: A Guide to the World’s Fresh Water Resources (Oxford University Press, New York).

References

8. Maupin MA, Kenny JF, Hutson SS, et al (2014) Estimated use of water in the United States in 2010. US Geological Survey

9. Gleick PH (1993) Water in Crisis: A Guide to the World’s Fresh Water Resources, 1 edition. Oxford University Press

10. Hadley G (1735) Concerning the cause of the general trade-winds: By Geo. Hadley, Esq; FRS. Philosophical Transactions 39:58–62

11. Lorenz EN (1955) Available potential energy and the maintenance of the general circulation. Tell’Us 7:157–167

12. Halvorson SF, James Steenburgh W (1999) Climatology of lake-effect snowstorms of the Great Salt Lake. University of Utah

13. Powell JW (1879) Report on the lands of the arid region of the United States with a more detailed account of the land of Utah with maps. Monograph

14. U.S. Geological Survey (2012) Snowmelt - The Water Cycle, from USGS Water-Science School