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Hydrologic Assessment and Modeling

Scientists at the New Mexico Water Science Center collect weather, geologic and hydrologic data to assess the past and current state of New Mexico's water resources. These data are also used to develop and calibrate hydrologic models. These models can help water-resource managers understand trends in water availability and risks to the resources under different water-use and climate scenarios. 

Filter Total Items: 35

Upper Rio Grande Basin Focus Area Study

The Upper Rio Grande Basin (URGB) of Colorado, New Mexico, Texas, and northern Mexico was chosen as a focus area study (FAS) for the USGS National Water Census. The conjunctive use of water in the URGB takes place under a myriad of legal constraints including the Rio Grande Compact agreement between the States, an international treaty with Mexico, and several federal water projects. Development of...
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Upper Rio Grande Basin Focus Area Study

The Upper Rio Grande Basin (URGB) of Colorado, New Mexico, Texas, and northern Mexico was chosen as a focus area study (FAS) for the USGS National Water Census. The conjunctive use of water in the URGB takes place under a myriad of legal constraints including the Rio Grande Compact agreement between the States, an international treaty with Mexico, and several federal water projects. Development of...
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Drilling Replacement Monitoring Wells near the San Juan Coal Mine, NW New Mexico

The San Juan Coal Mine, an underground mine located about 12 miles west-northwest of Farmington, NM, supplies coal to the adjacent San Juan Generating Station.
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Drilling Replacement Monitoring Wells near the San Juan Coal Mine, NW New Mexico

The San Juan Coal Mine, an underground mine located about 12 miles west-northwest of Farmington, NM, supplies coal to the adjacent San Juan Generating Station.
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Changes in Watershed Hydrologic Response Time with Post-wildfire Changes in Vegetation and Surface Fuels Along a Severely-burned, High-desert Canyon, Bandelier National Monument, NM

Flash flooding can be a destructive and life-threatening response of watersheds to intense rainfall events, particularly in sparsely­ vegetated, or burned watersheds. Studies have been conducted to estimate the magnitude of hydrologic responses of burned watersheds to rainfall events, however the time that it takes a flood to travel through a burned watershed and reach a critical or populated area...
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Changes in Watershed Hydrologic Response Time with Post-wildfire Changes in Vegetation and Surface Fuels Along a Severely-burned, High-desert Canyon, Bandelier National Monument, NM

Flash flooding can be a destructive and life-threatening response of watersheds to intense rainfall events, particularly in sparsely­ vegetated, or burned watersheds. Studies have been conducted to estimate the magnitude of hydrologic responses of burned watersheds to rainfall events, however the time that it takes a flood to travel through a burned watershed and reach a critical or populated area...
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Post-Wildfire Investigation: Analysis of Soil Properties Based on Burn Severity

The Las Conchas fire started on June 26, 2011, near the small community of Las Conchas in the Jemez Mountains of north-central New Mexico. When the fire was contained on August 3, 2011, it had burned 156,593 acres of mixed conifer, pinyon/juniper and ponderosa forest and at the time was the largest wildfire in New Mexico history. Peak burn severity was extreme; over 60,000 acres of the total...
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Post-Wildfire Investigation: Analysis of Soil Properties Based on Burn Severity

The Las Conchas fire started on June 26, 2011, near the small community of Las Conchas in the Jemez Mountains of north-central New Mexico. When the fire was contained on August 3, 2011, it had burned 156,593 acres of mixed conifer, pinyon/juniper and ponderosa forest and at the time was the largest wildfire in New Mexico history. Peak burn severity was extreme; over 60,000 acres of the total...
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Water Resource Assessment of the Rio San Jose Basin, West-Central New Mexico

Water resources in the Rio San Jose Basin are limited, and development for public supply, mining, agriculture, and commercial activities have the potential to affect the water availability and quality at a basin-wide scale. This study is designed to provide water-resource managers with better information to plan for potential effects of increased or shifting demands and changes of climatic...
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Water Resource Assessment of the Rio San Jose Basin, West-Central New Mexico

Water resources in the Rio San Jose Basin are limited, and development for public supply, mining, agriculture, and commercial activities have the potential to affect the water availability and quality at a basin-wide scale. This study is designed to provide water-resource managers with better information to plan for potential effects of increased or shifting demands and changes of climatic...
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Streamgaging: Silent Sentinels

Streamflow data are needed at many sites on a daily basis for forecasting flow extremes, making water-management decisions, assessing current water availability, managing water quality, and meeting legal requirements. These activities require streamflow information at a given location for a specified time. These needs generally are best satisfied by operating a station to produce a continuous...
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Streamgaging: Silent Sentinels

Streamflow data are needed at many sites on a daily basis for forecasting flow extremes, making water-management decisions, assessing current water availability, managing water quality, and meeting legal requirements. These activities require streamflow information at a given location for a specified time. These needs generally are best satisfied by operating a station to produce a continuous...
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URGWOM: Upper Rio Grande Water Operations Model

The Upper Rio Grande (URG) River Basin extends from the headwaters in Colorado to the USGS streamflow gage Rio Grande near Fort Quitman, Texas, and includes both native water and transmountain water from the Colorado River Basin. Because of surface-water allotment issues, input from various sources of water (native and transmountain), numerous reservoirs, and complex stream-aquifer relations...
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URGWOM: Upper Rio Grande Water Operations Model

The Upper Rio Grande (URG) River Basin extends from the headwaters in Colorado to the USGS streamflow gage Rio Grande near Fort Quitman, Texas, and includes both native water and transmountain water from the Colorado River Basin. Because of surface-water allotment issues, input from various sources of water (native and transmountain), numerous reservoirs, and complex stream-aquifer relations...
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Lee Acres Landfill Superfund Site, Farmington, NM

Lee Acres Landfill is 40 acres of public land in San Juan County southeast of Farmington, New Mexico. On May 1, 1962 the Bureau of Land Management (BLM) leased land to San Juan County to operate a county landfill. The landfill consists of an undetermined number of solid waste trenches and unlined waste lagoons.
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Lee Acres Landfill Superfund Site, Farmington, NM

Lee Acres Landfill is 40 acres of public land in San Juan County southeast of Farmington, New Mexico. On May 1, 1962 the Bureau of Land Management (BLM) leased land to San Juan County to operate a county landfill. The landfill consists of an undetermined number of solid waste trenches and unlined waste lagoons.
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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...
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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...
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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...
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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...
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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...
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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...
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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...
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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...
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