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ABOUT THE Arizona WSC
USGS IN YOUR STATE
USGS Water Science Centers are located in each state.
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Water Resources of Arizona
Welcome to the U.S. Geological Survey (USGS) Web page for the water resources of Arizona; this is your direct link to all kinds of water-resource information. Here you'll find information on Arizona's rivers and streams. You'll also find information about groundwater, water quality, and many other topics.
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Understanding and Managing the Effects of Groundwater Pumping on Streamflow
U.S. Geological Survey Fact Sheet 2013–3001
Interest is growing about how groundwater pumping affects rivers, streams, and springs. Although groundwater pumped from aquifers is a critical resource that provides drinking water, irrigates crops, and supports industry, water pumped from aquifers can reduce the groundwater that flows into rivers and streams. In turn, reduced streamflow can harm aquatic ecosystems, reduce the availability of surface water, and change the visual character of streams and rivers.
Scientific research and practical applications of this research to real-world settings over the past seven decades have improved the understanding and management of the effects of groundwater pumping on streamflow. This Fact Sheet, which was co-authored by the Arizona Water Science Center’s Stan Leake, summarizes information about how groundwater pumping affects streams, misconceptions about the process, and methods for understanding and managing streamflow depletion by wells. A more detailed description of these and other issues related to understanding and managing the effects of groundwater pumping on streamflow is provided in U.S. Geological Survey Circular 1376.
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Hydrologic Conditions
Drought Conditions for Selected Basins
The USGS, in cooperation with the Governor's Drought Task Force, has developed a series of maps showing drought intensity for selected drainage basins in Arizona. To view historical maps, learn how the maps are developed, and download images, visit our drought page.
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Drought conditions for January 2013
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Arizona Water Science Center Highlights
AzWSC hydrologist Fred Tillman is interviewed on NPR about groundwater levels in Arizona. (For more information, see USGS SIR 2011-5071, Water Availability and Use Pilot: Methods Development for a Regional Assessment of Groundwater Availability, Southwest Alluvial Basins, Arizona)
Microgravity Measurement for Groundwater Analysis
A video discussing the Gravity Meters used at the USGS Arizona Water Science Center.
Seepage Investigation: Clear Creek and Little Colorado River
The USGS Arizona Water Science Center performed a seepage investigation on reaches of Chevelon Creek, Clear Creek, and a reach of the Little Colorado River during the fall of 2010. The investigation is in cooperation with the Bureau of Indian Affairs Navajo Region and is part of a larger program that monitors the Coconino Aquifer in Northeastern Arizona. The video describes the process of a seepage investigation. In the video, USGS hydrologists and hydrographers measure discharge and water-quality parameters on Clear Creek and the Little Colorado River to better understand and characterize the Coconino Aquifer.
USGS CoreCast—Streamgages: The Silent Superhero
Whether you drink water from your tap, use electricity or canoe down your local river, chances are you benefit from USGS streamgage information. So what is a streamgage and what does it do for you? This CoreCast episode gives you the inside scoop on your silent superhero.
USGS Streamflow Measurement at Pinto Creek near Miami, Arizona — January 28, 2010
USGS streamgagers, Mike Sanders, Arthur Rees, and Mike Schilling, are servicing the Pinto Creek near Miami, Arizona streamflow-gaging station (09498502) and making a streamflow measurement on January 28, 2010. Flow was measured to be 207 cubic feet per second (CFS) on the 28th but peaked earlier on the 22nd at an estimated 7,400 cfs. Debris from the flood flow can be seen in trees and on the over bank areas.
Video showing Simulated Zones of Capture of Surface Water by Groundwater Pumping, upper part of the San Pedro Basin
USGS Hydrologists Stan Leake, Don Pool, and Jim Leenhouts used a groundwater flow model of the upper part of the San Pedro Basin in Arizona to produce capture maps (Scientific Investigations Report 2008-5207) to help managers understand the possible timing of effects groundwater pumping in the lower basin fill has on streams, springs, and evapotranspiration by riparian plants. Maps in the report for pumping times of 10 years and 50 years show patterns that reflect the fraction of pumping that is simulated to be a reduction of water available to the riparian system. For example, on the map for a withdrawal time of 10 years, a capture-fraction zone of 0.5-0.6 shows areas where capture or depletion of surface water and evapotranspiration will be 50-60 percent of the well pumping rate at that time. The accompanying video takes the analysis one step further by showing how some of these simulated capture zones evolve over a 100-year period of pumping. In this example, capture zones in ranges of 0.5-0.6, 0.6-0.7, 0.7-0.8, 0.8-0.9, and 0.9-1.0 are shown.
Video of Yuma Field Office staff demonstrating acoustic technology to members of Arizona Floodplain Managers Association on November 7, 2008
The USGS Yuma Field Office, which is headed by Hugh Darling, has a young and enthusiastic staff implementing new technology to improve the precision of data collected. The staff has embraced hydroacoustics using both Acoustic Doppler Velocity Meters (ADVM) and Acoustic Doppler Current Profilers (ADCP). Nearly 100 percent of stream flow measurements made by the Yuma Field Office staff are made with acoustic instruments while using current meters as quality assurance. One of the most critical roles the Yuma Field office plays is the quantification of flow in the Colorado River, its tributaries, and diversions. This video shows the Yuma Field Office staff demonstrating acoustic technology to members of Arizona Floodplain Managers Association on November 7, 2008.
Video of Havasu Canyon after August 17, 2008 high-flow event
The video describes observations made by AzWSC scientists on the high-flow event that occurred around August 17, 2008, in Havasu Canyon on the Havasupai Indian Reservation, northern Arizona. The Havasupai Indian Tribe lives in the remote Havasu Canyon, a tributary canyon to Grand Canyon National Park, and is only accessible by foot, horseback, or helicopter. The high-flow event caused massive erosion below the village of Supai, resulting in the creation of new water falls and the cessation of Navajo Falls. AzWSC scientists made assessments of the high-flow event on August 28th and 29th, 2008, and made an indirect measurement of the peak flow that passed through the village of Supai. A preliminary calculation of the peak flow is 6,000 cubic feet per second. (August 29, 2008 — narrated by Greg Fisk and Steve Wiele)
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Recent Publications
Scientific Investigations Report 2012-5275
Hydrogeologic Framework and Estimates of Groundwater Storage for the Hualapai Valley, Detrital Valley, and Sacramento Valley Basins, Mohave County, Arizona
by Margot Truini, L. Sue Beard, Jeffrey Kennedy, and David W. Anning |
Open-File Report 2013–1029
Water-Quality Data Collected to Determine the Presence, Source, and Concentration of Lead in the Drinking Water Supply at Pipe Spring National Monument, Northern Arizona
by Jamie P. Macy, David Sharrow, and Joel Unema |
Open-File Report 2012–1237
Establishment of Sentinel Sampling Sites to Monitor Changes in Water and Sediment Quality and Biota Related to Visitor Use at Lake Powell, Arizona and Utah, 2004–2006
by Robert J. Hart, Howard E. Taylor, and G.M. Anderson |
Scientific Investigations Report 2012-5276
Preliminary Hydrogeologic Assessment near Tassi and Pakoon Springs, Western Part of Grand Canyon-Parashant National Monument, Arizona
by Margot Truini |
Fact Sheet 2013-3001
Understanding and Managing the Effects of Groundwater Pumping on Streamflow
by Stanley A. Leake and Paul M. Barlow |
Scientific Investigations Map 3234
Maps of Estimated Nitrate and Arsenic Concentrations for Basin-Fill Aquifers of the Southwestern United States
by Kimberly R. Beisner, David W. Anning, Angela P. Paul, Tim S. McKinney, Jena M. Huntington, Laura M. Bexfield, and Susan A. Thiros |
Circular 1376
Streamflow Depletion by Wells—Understanding and Managing the Effects of Groundwater Pumping on Streamflow
by Paul M. Barlow and Stanley A. Leake |
Open-File Report 2012–1203
Biotic, Water-Quality, and Hydrologic Metrics Calculated for the Analysis of Temporal Trends in National Water Quality Assessment Program Data in the Western United States
by Stephen M. Wiele, Anne M.D. Brasher, Matthew P. Miller, Jason T. May, and Kurt D. Carpen |
Scientific Investigations Report 2012-5201
Aquifer Test at Well SMW-1 near Moenkopi, Arizona
by Robert L. Carruth and Donald J. Bills |
Open-File Report 2012–1206
Evaluation of Simulations to Understand Effects of Groundwater Development and Artificial Recharge on Surface Water and Riparian Vegetation, Sierra Vista Subwatershed, Upper San Pedro Basin, Arizona
by Stanley A. Leake and Bruce Gungle |
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