HOME : RESEARCH : Thrust Area 1
RESEARCH
PHYSICAL SCIENCE
• Spatial and Temporal Components of the Water Balance

• Basin Scale Water and Solute Balances

• Functioning of Riparian Systems


BEHAVIORAL SCIENCE
• Water as a Resource: Competition, Conflict, Planning and Policy

• Disaggregating Domestic Demand


INTEGRATIVE MODELING
• Multi-Resolution Integrated Modeling of Basin-Scale Processes


SCIENCE INTEGRATION
• Integration
• Scenarios
• Stakeholders


RESOURCES
• Field sites
• Labs & Equipment

Field Sites


USDA-ARS Walnut Gulch Experimental Watershed

The Walnut Gulch Experimental Watershed operated by the Southwest Watershed Research Center of USDA-Agricultural Research Service in Tucson, Arizona is a premiere semi-arid experimental watershed. The watershed (roughly an 80 minute drive from Tucson) drains 150 square kilometers in southeastern Arizona and is representative of the approximately 60 million hectares of grass- and brush-covered rangeland found throughout the semi-arid southwest and northern Mexico. It lies in a transition zone between the Chihuahuan and Sonoran Deserts. The scientific instrumentation and research infrastructure at Walnut Gulch are unparalleled. Detailed experiments and long-term observations are conducted to improve understanding of semi-arid rangeland hydrology and erosion. No comparable semi-arid hydrologic database exists in the world (see http://www.tucson.ars.ag.gov ).

The Walnut Gulch facility consists of 29 nested watersheds that range in drainage area from 0.002 to 150 square kilometers. Rainfall and runoff instrumentation (including 85 recording rain gauges) has been in place since 1964. Eleven of the nested watersheds are gauged for runoff with concrete supercritical flumes that are specially designed to give very accurate estimates of runoff (notoriously difficult to obtain in semi-arid regions). Extensive monitoring of erosion and sediment transport is conducted on eight of the smaller sub-watersheds. Hydro-meteorological instrumentation at two locations, one grass dominated and the other brush dominated, provide measurements of the energy balance, soil temperature, soil moisture and CO2 fluxes. Biotic characterization has been ongoing. A high-resolution GIS database for the watershed has been created. All of the recording instrumentation is currently undergoing conversion to digital systems with telemetry for remote data transfer. The NEXRAD radar system installed by the National Weather Service at Tucson provides radar coverage. The ARS Walnut Gulch headquarters facilities outside Tombstone include soils and sediment laboratories, and workshops for electronics, machine and welding/fabrication. The facilities and instrumentation are maintained by four full-time support staff, and on-site lodging is available for up to six visiting scientists.

The Walnut Gulch watershed and the containing San Pedro basin continue to be a venue for highly instrumented large-scale multidisciplinary research and watershed characterization conducted by a variety of agencies, universities, and members of the Upper San Pedro Partnership to more accurately estimate the semi-arid water balance and understand the water needs of the first Congressionally designated Riparian National Conservation Area. Ongoing ground, aircraft and satellite data remote sensing collections continue as these watersheds serve as the primary semi-arid validation site for NASA's Earth Observing System. SPOT and LANDSAT images are being routinely archived.


Arizona District of the United States Geological Survey

The U.S. Geological Survey conducts extensive research on the groundwater resources of the southwestern U.S. Many of the projects conducted by the Arizona district programs have great relevance to SAHRA's effort. In addition, scientists in the USGS National Research Program provide research tools and models that are standard to groundwater analysis and research in the United States.

The Arizona District of the USGS located in Tucson is leading a multidisciplinary groundwater project called the Southwestern Groundwater Project that is highly relevant to SAHRA. The project involves research and evaluation of the spatial and temporal variability of groundwater recharge and outflow in shallow aquifer systems, and provides several opportunities for collaboration SAHRA, including studies of ephemeral wash recharge and groundwater outflow in the middle Rio Grande basin near Albuquerque, New Mexico, and the San Pedro River National Conservation Area in southern Arizona. These investigations provide important research opportunities for students in the hydrology and ecology programs. Additionally, the USGS Arizona District office is conducting a detailed investigation of groundwater resources of the upper San Pedro River Basin. That project and SAHRA have continuing collaboration on data collection and analysis relating to the groundwater flow system.

USGS operates the most extensive set of streamflow gauging stations in the U.S., providing an essential long-term database from which to evaluate outflow from shallow groundwater systems such as the San Pedro River. The USGS also has geophysical tools for assessing characteristics of aquifer systems. A drill rig is maintained in Menlo Park, CA, and is available to the Arizona District for drilling high-quality monitoring wells. A national database system maintains information on wells and groundwater geochemistry.


Eddy Covariance Sites
The following sites are being used by SAHRA researchers:

Agricultural Research Service: 2 eddy covariance sites: one is at the Charleston Mesquite site in the San Pedro Riparian National Conservation Area (SPRNCA), 100 km from Tucson near Charleston, Arizona; the second is being set up in a mesquite bosque in spring 2003.

Los Alamos National Laboratory: 5 mobile eddy covariance stations

University of Arizona - HWR: SAHRA staff members based at the University of Arizona maintain a series of eddy covariance sites in diverse bioregions.
  • The Mt. Bigelow Field Site is located in a subalpine Douglas fir forest in the Santa Catalina Mountains north of Tucson. It includes a 30-m tall eddy covariance tower, with a supporting spatial network of three micrometeorological stations. Instrumentation includes the eddy covariance tower system with 4-way radiometer and three (elevational) levels of sensors, soil heat flux, net radiometers, infrared surface temperature, soil moisture probes, and soil temperature probes. A portable leaf gas exchange analyzer is also available for use at Mt. Bigelow or at the San Pedro sites (discussed below).
  • San Pedro - Two eddy covariance sites are also set up adjacent to one another at lower elevations near the San Pedro River, 100 km SE of Tucson, in a sacaton grassland and a mixed mesquite/grassland. Tower data will be integrated with that from flux towers at complementary regions.


Sevilleta LTER

This Long Term Ecological Research site (LTER) in New Mexico is used for watershed-scale and riparian research. Major advantages to conducting research on the LTER include: a) security, (it is fenced and patrolled), b) existing instrumentation networks for measuring rainfall, solar radiation, soil temperature and moisture, wind speed and direction, and other climate variables, c) ongoing hydrologic studies, and d) available satellite data. Eric Small (University of Colorado) and Will Pockman (UNM) have obtained additional funding from DOE for water addition experiments to parallel their SAHRA-sponsored drought experiments there.

The Sevilleta LTER Program is located primarily on the Sevilleta National Wildlife Refuge in Socorro County of central New Mexico, and includes biomes ranging from Great Plains grassland, Great Basin shrub-steppe, Chihuahuan desert, to montane coniferous forest. The area has a complex topography (1,350 to 2,797 m in elevation) and varied geology and soils, providing an ideal opportunity for researchers to study biome transition zones.

The major goal of Thrust Area 1 is to measure, estimate and model the spatial and temporal components of the basin-scale water balance (snow accumulation, distribution, and melt, rainfall, evapotranspiration/sublimation, runoff, and infiltration) by intensive and continuous field observations, coupled with modeling, in areas above the mountain front and a variety of ecological locations on the desert floor.

 




























©2005 Arizona Board of Regents. Read Disclaimer.