Skip to main content
U.S. flag

An official website of the United States government

Hydrologic Monitoring and Trends

In cooperation with our partners, the New Mexico Water Science Center maintains over 180 active stream gages and collects information on the quality and quantity of New Mexico's groundwater at over 6,000 sites. These data are used for everything from recreational users planning for river trips to managers working to better understand the state’s water resources.

Filter Total Items: 47

Monitoring Network of the Groundwater Flow System and Stream-Aquifer Relations in the Mesilla Basin, Doña Ana County, New Mexico and El Paso County, Texas

The Mesilla Basin monitoring program was established in 1987 to document the hydrologic conditions of New Mexico’s southern-most, Rio Grande rift basin. The program’s data collection and reporting is conducted by the U.S. Geological Survey in cooperation with local, state, and federal agencies. Hydrologic data collected as part of the monitoring program provide valuable information to better...
link

Monitoring Network of the Groundwater Flow System and Stream-Aquifer Relations in the Mesilla Basin, Doña Ana County, New Mexico and El Paso County, Texas

The Mesilla Basin monitoring program was established in 1987 to document the hydrologic conditions of New Mexico’s southern-most, Rio Grande rift basin. The program’s data collection and reporting is conducted by the U.S. Geological Survey in cooperation with local, state, and federal agencies. Hydrologic data collected as part of the monitoring program provide valuable information to better...
Learn More

Debris flows and Floods from Extreme Precipitation in September 2013, Gila National Forest, NM

A record-breaking rainstorm in Glenwood, New Mexico and the surrounding areas occurred in September, 2013 leading to widespread and destructive flooding and debris flows, including watersheds burned the previous year by the Whitewater-Baldy Complex wildfire. In the area of the Whitewater-Baldy burn scar, a highway was overtopped by flash flooding on Whitewater Creek. Many side canyon tributaries...
link

Debris flows and Floods from Extreme Precipitation in September 2013, Gila National Forest, NM

A record-breaking rainstorm in Glenwood, New Mexico and the surrounding areas occurred in September, 2013 leading to widespread and destructive flooding and debris flows, including watersheds burned the previous year by the Whitewater-Baldy Complex wildfire. In the area of the Whitewater-Baldy burn scar, a highway was overtopped by flash flooding on Whitewater Creek. Many side canyon tributaries...
Learn More

Prewildfire Assessments of Postwildfire Debris-Flow Hazards

Debris flows are high-density slurries of water, rock fragments, soil, and mud that can have enormous destructive power. Wildfire can drastically increase the probability of debris flows in landscapes that have otherwise been stable. In 2010, the USGS developed the Cannon model to estimate postwildfire debris-flow probabilities and volumes in burned areas. In 2013, with the help of U.S. Forest...
link

Prewildfire Assessments of Postwildfire Debris-Flow Hazards

Debris flows are high-density slurries of water, rock fragments, soil, and mud that can have enormous destructive power. Wildfire can drastically increase the probability of debris flows in landscapes that have otherwise been stable. In 2010, the USGS developed the Cannon model to estimate postwildfire debris-flow probabilities and volumes in burned areas. In 2013, with the help of U.S. Forest...
Learn More

Postwildfire Debris-Flow Hazards

Wildfire is a natural process in forest ecosystems, and occurs with varying frequencies and severities depending on landscape characteristics, climatic conditions, and the historical fire regime. Although attention often is focused on the potential damages from wildfire in the wildland-urban interface, wildfire also presents a threat to critical infrastructure including flood water conveyances and...
link

Postwildfire Debris-Flow Hazards

Wildfire is a natural process in forest ecosystems, and occurs with varying frequencies and severities depending on landscape characteristics, climatic conditions, and the historical fire regime. Although attention often is focused on the potential damages from wildfire in the wildland-urban interface, wildfire also presents a threat to critical infrastructure including flood water conveyances and...
Learn More

Hydrologic Studies in the East Mountain Area of Bernalillo County, NM

Recent expansion of suburban development and population growth in the Sandia Mountains of eastern Bernalillo County, NM (East Mountain Area, EMA), has led to increased residential and commercial construction and increased demands on available water resources. Information about the spatial and temporal variability of water resources is needed for continued population and economic growth. USGS...
link

Hydrologic Studies in the East Mountain Area of Bernalillo County, NM

Recent expansion of suburban development and population growth in the Sandia Mountains of eastern Bernalillo County, NM (East Mountain Area, EMA), has led to increased residential and commercial construction and increased demands on available water resources. Information about the spatial and temporal variability of water resources is needed for continued population and economic growth. USGS...
Learn More

Changes in Groundwater Levels in the Albuquerque Metropolitan Area

The U.S. Geological Survey, in cooperation with the Albuquerque Bernalillo County Water Utility Authority (ABCWUA) has been investigating the effects of groundwater withdrawal on groundwater levels throughout the Albuquerque metropolitan area in the Middle Rio Grande Valley of central New Mexico (fig. 1). Historically, the water supply requirements of the Albuquerque metropolitan area were met...
link

Changes in Groundwater Levels in the Albuquerque Metropolitan Area

The U.S. Geological Survey, in cooperation with the Albuquerque Bernalillo County Water Utility Authority (ABCWUA) has been investigating the effects of groundwater withdrawal on groundwater levels throughout the Albuquerque metropolitan area in the Middle Rio Grande Valley of central New Mexico (fig. 1). Historically, the water supply requirements of the Albuquerque metropolitan area were met...
Learn More

Aquifer Compaction, Recovery, and Land-surface Elevation Change in the Albuquerque Basin

In many groundwater basins in the arid to semiarid western United States, permanent regional-scale land-surface elevation change has resulted from substantial drawdown of groundwater levels. By the end of 2008, groundwater drawdown from municipal pumping in the Albuquerque area had reached as much as 120 feet below predevelopment (~1950s) water levels. In 2014 the USGS, in cooperation with the...
link

Aquifer Compaction, Recovery, and Land-surface Elevation Change in the Albuquerque Basin

In many groundwater basins in the arid to semiarid western United States, permanent regional-scale land-surface elevation change has resulted from substantial drawdown of groundwater levels. By the end of 2008, groundwater drawdown from municipal pumping in the Albuquerque area had reached as much as 120 feet below predevelopment (~1950s) water levels. In 2014 the USGS, in cooperation with the...
Learn More

Bandelier National Monument Postwildfire Flood Support

In the summer of 2011, the Las Conchas Fire burned 156,593 acres in the Jemez Mountains in northern NM including the upper watersheds of Frijoles and Capulin Canyons in Bandelier National Monument. The drastic removal of vegetation in the upper watersheds of these popular tourist destinations left them susceptible to dangerous and record breaking floods. As long as the threat of large post...
link

Bandelier National Monument Postwildfire Flood Support

In the summer of 2011, the Las Conchas Fire burned 156,593 acres in the Jemez Mountains in northern NM including the upper watersheds of Frijoles and Capulin Canyons in Bandelier National Monument. The drastic removal of vegetation in the upper watersheds of these popular tourist destinations left them susceptible to dangerous and record breaking floods. As long as the threat of large post...
Learn More
link

USGS Post-Wildfire Hydrologic Monitoring in New Mexico

USGS Gages in New Mexico Wildfire Areas
Learn More

Continuous Water Quality Monitoring on the Pecos River in Southern New Mexico

High levels of salinity in the Pecos River render it less useful for various purposes. It is believed that underground salt deposits in the Malaga area contribute to the increase in the salinity in the Pecos River as it flows through this area.
link

Continuous Water Quality Monitoring on the Pecos River in Southern New Mexico

High levels of salinity in the Pecos River render it less useful for various purposes. It is believed that underground salt deposits in the Malaga area contribute to the increase in the salinity in the Pecos River as it flows through this area.
Learn More

Floods Analysis

Accurate estimations of flood discharges at bridge or culvert sites is required to provide cost-effective design of that structure. Streamflow-gaging stations, for which flood data are available, are usually located in major perennial drainage basins that are not representative of sites where common bridge and culvert designs are needed. In 1942, the USGS, in cooperation with the New Mexico...
link

Floods Analysis

Accurate estimations of flood discharges at bridge or culvert sites is required to provide cost-effective design of that structure. Streamflow-gaging stations, for which flood data are available, are usually located in major perennial drainage basins that are not representative of sites where common bridge and culvert designs are needed. In 1942, the USGS, in cooperation with the New Mexico...
Learn More

Rio Grande Travel Times

The City of Albuquerque will begin accepting delivery of imported San Juan-Chama water to supplement present municipal water supplies as part of the City's Drinking Water Project (DWP). The City's San Juan-Chama water will be diverted from the Rio Grande near Alameda Bridge in Albuquerque, transported to a treatment facility, and eventually distributed to customers. Water in the Rio Grande is...
link

Rio Grande Travel Times

The City of Albuquerque will begin accepting delivery of imported San Juan-Chama water to supplement present municipal water supplies as part of the City's Drinking Water Project (DWP). The City's San Juan-Chama water will be diverted from the Rio Grande near Alameda Bridge in Albuquerque, transported to a treatment facility, and eventually distributed to customers. Water in the Rio Grande is...
Learn More
Was this page helpful?