Supervisory Hydrologic Technician, Rio Arriba Field Office Chief, New Mexico Water Science Center
Science and Products
Hydrogeologic and geochemical characterization and evaluation of two arroyos for managed aquifer recharge by surface infiltration in the Pojoaque River Basin, Santa Fe County, New Mexico, 2014–15
In order to provide long-term storage of diverted surface water from the Rio Grande as part of the Aamodt water rights settlement, managed aquifer recharge by surface infiltration in Pojoaque River Basin arroyos was proposed as an option. The initial hydrogeologic and geochemical characterization of two arroyos located within the Pojoaque River Basin was performed in 2014 and 2015 in cooperation w
Hydrology of the middle San Pedro area, southeastern Arizona
Runoff conditions in Utah for water year 2011
Water availability and use pilot: Methods development for a regional assessment of groundwater availability, southwest alluvial basins, Arizona
Hydrogeologic framework of the middle San Pedro watershed, southeastern Arizona
The continuous slope-area method for computing event hydrographs
Methods and Indicators for Assessment of Regional Ground-Water Conditions in the Southwestern United States
An Online Interactive Map Service for Displaying Ground-Water Conditions in Arizona
Assessing the likely value of gravity and drawdown measurements to constrain estimates of hydraulic conductivity and specific yield during unconfined aquifer testing
National Water-Quality Assessment Program (NAWQA) Rio Grande Valley Study
Rio Grande Compact and Pecos River Commission
Science and Products
- Publications
Hydrogeologic and geochemical characterization and evaluation of two arroyos for managed aquifer recharge by surface infiltration in the Pojoaque River Basin, Santa Fe County, New Mexico, 2014–15
In order to provide long-term storage of diverted surface water from the Rio Grande as part of the Aamodt water rights settlement, managed aquifer recharge by surface infiltration in Pojoaque River Basin arroyos was proposed as an option. The initial hydrogeologic and geochemical characterization of two arroyos located within the Pojoaque River Basin was performed in 2014 and 2015 in cooperation w
AuthorsAndrew J. Robertson, Jeffrey Cordova, Andrew Teeple, Jason Payne, Rob CarruthHydrology of the middle San Pedro area, southeastern Arizona
In the middle San Pedro Watershed in southeastern Arizona, groundwater is the primary source of water supply for municipal, domestic, industrial, and agricultural use. The watershed comprises two smaller subareas, the Benson subarea and the Narrows-Redington subarea. Early 21st century projections for heavy population growth in the watershed have not yet become a reality, but increased groundwaterAuthorsJeffrey T. Cordova, Jesse E. Dickinson, Kimberly R. Beisner, Candice B. Hopkins, Jeffrey R. Kennedy, Donald R. Pool, Edward P. Glenn, Pamela L. Nagler, Blakemore E. ThomasRunoff conditions in Utah for water year 2011
In May 2011, the snowpack conditions in the mountains of central and northern Utah had emergency planners and water managers preparing for levels of runoff similar to the record year of 1983. The SNOwpack TELemetry (SNOTEL) records from the Natural Resources Conservation Service (NRCS) reported that the amount of water contained in the snowpack in May 2011 was greater than it was in either May ofAuthorsJeffrey T. Cordova, Cory E. AngerothWater availability and use pilot: Methods development for a regional assessment of groundwater availability, southwest alluvial basins, Arizona
Executive Summary: Arizona is located in an arid to semiarid region in the southwestern United States and is one of the fastest growing States in the country. Population in Arizona surpassed 6.5 million people in 2008, an increase of 140 percent since 1980, when the last regional U.S. Geological Survey (USGS) groundwater study was done as part of the Regional Aquifer System Analysis (RASA) progrAuthorsFred D. Tillman, Jeffrey T. Cordova, Stanley A. Leake, Blakemore E. Thomas, James B. CallegaryHydrogeologic framework of the middle San Pedro watershed, southeastern Arizona
Water managers in rural Arizona are under increasing pressure to provide sustainable supplies of water despite rapid population growth and demands for environmental protection. This report describes the results of a study of the hydrogeologic framework of the middle San Pedro watershed. The components of this report include: (1) a description of the geologic setting and depositional history of basAuthorsJesse E. Dickinson, Jeffrey R. Kennedy, D. R. Pool, Jeffrey T. Cordova, John T. Parker, J. P. Macy, Blakemore ThomasThe continuous slope-area method for computing event hydrographs
The continuous slope-area (CSA) method expands the slope-area method of computing peak discharge to a complete flow event. Continuously recording pressure transducers installed at three or more cross sections provide water-surface slopes and stage during an event that can be used with cross-section surveys and estimates of channel roughness to compute a continuous discharge hydrograph. The CSA metAuthorsChristopher F. Smith, Jeffrey T. Cordova, Stephen M. WieleMethods and Indicators for Assessment of Regional Ground-Water Conditions in the Southwestern United States
Monitoring the status and trends in the availability of the Nation's ground-water supplies is important to scientists, planners, water managers, and the general public. This is especially true in the semiarid to arid southwestern United States where rapid population growth and limited surface-water resources have led to increased use of ground-water supplies and water-level declines of several hunAuthorsFred D. Tillman, Stanley A. Leake, Marilyn E. Flynn, Jeffrey T. Cordova, Kurt T. Schonauer, Jesse E. DickinsonAn Online Interactive Map Service for Displaying Ground-Water Conditions in Arizona
Monitoring the availability of the nation's ground-water supplies is of critical importance to planners and water managers. The general public also has an interest in understanding the status of ground-water conditions, especially in the semi-arid Southwestern United States where much of the water used by municipalities and agriculture comes from the subsurface. Unlike surface-water indicators sucAuthorsFred D. Tillman, Stanley A. Leake, Marilyn E. Flynn, Jeffrey T. Cordova, Kurt T. SchonauerAssessing the likely value of gravity and drawdown measurements to constrain estimates of hydraulic conductivity and specific yield during unconfined aquifer testing
Pumping of an unconfined aquifer can cause local desaturation detectable with high‐resolution gravimetry. A previous study showed that signal‐to‐noise ratios could be predicted for gravity measurements based on a hydrologic model. We show that although changes should be detectable with gravimeters, estimations of hydraulic conductivity and specific yield based on gravity data alone are likely to bAuthorsJoan B. Blainey, Ty P.A. Ferré, Jeffrey T. Cordova - Science
National Water-Quality Assessment Program (NAWQA) Rio Grande Valley Study
The New Mexico Water Science Center (NMWSC) has historically conducted NAWQA data collection of groundwater and surface water-data within the former Rio Grande Valley (RIOG) study unit, which covers about 45,700 square miles in Colorado, New Mexico, and Texas.Rio Grande Compact and Pecos River Commission
Rio Grande Compact and Pecos River Commission - News