Geoff Moret
Geoff Moret is a the studies chief of the Southern Nevada Hydrologic Studies Unit.
Professional Experience
2016 - Present: Studies Chief, U.S. Geological Survey, Boulder City, NV
Science and Products
Evaporation from Lake Mead and Lake Mohave, Lower Colorado River Basin, Nevada and Arizona
Since 2010, the U.S. Geological Survey (USGS) Nevada Water Science Center (NVWSC) has worked with with the Bureau of Reclamation to update evaporation estimates for Lake Mead.
Near-Continuous Depth-Dependent Water-Quality Data from Automatic Profiling Systems and Meteorological Data, Lakes Mead and Mohave, Arizona and Nevada, USA
The Colorado River is one of the most intensely used rivers in the western United States, providing recreational watercraft activities and domestic drinking, industrial, and irrigation water for over 22 million users in the desert southwest. The quality of this water must be maintained to guarantee a reliable and safe resource for its many uses. The Colorado River provides an estimated 97 percent...
Science in the Colorado River Basin
The Colorado River is one of the longest rivers in the Western United States. It begins in the Rocky Mountains of Colorado and flows southwestward until it reaches Mexico where it becomes a small stream or dry riverbed. The Colorado River forms the border between southeastern Nevada and northwestern Arizona. In Nevada, Hoover Dam and Davis Dam control the flow of the river and create two...
Evaluating Potential Refugia for the Endangered Mohave Tui Chub
The USGS Nevada Water Science Center (NVWSC), in partnership with the National Park Service (NPS), is evaluating and monitoring the basic water quality and sediment chemistry of two proposed refugia and three established habitats for the endangered Mohave Tui Chub over the course of the year. NVWSC will also compare and evaluate findings to U.S. Environmental Protection Agency screening levels and...
Groundwater Discharge by Evapotranspiration from Areas of Spring-Fed Riparian Vegetation, Stump Spring and Hiko Springs, Nev.
Stump Spring has been designated as an Area of Critical Environmental Concern by the Bureau of Land Management (BLM), and Hiko Springs currently is in the designation process. Both springs flow intermittently in drainages where the depth to groundwater is shallow. The shallow groundwater flowing to and from the springs sustain scarce desert riparian habitats. BLM has recognized a need for accurate...
Groundwater Discharge by Evapotranspiration, Flow of Water in Unsaturated Soil, and Stable Isotope Water Sourcing in Areas of Sparse Vegetation, Amargosa Desert, Nye County, Nevada
The USGS conducted a study to evaluate the potential for groundwater discharge from sparsely vegetated areas in the Amargosa Desert. The study objectives were to: (1) compute groundwater discharge based on evapotranspiration and precipitation measurements at instrumented sites, and (2) improve understanding of hydrologic-continuum processes controlling groundwater discharge through analysis of...
Water Quality of Springs in the Spring Mountains
The USGS Nevada Water Science Center, in cooperation with the Bureau of Land Management, is sampling and analyzing water from Grapevine, Kiup, and Rainbow Springs to determine the source of water to these springs. These Springs, located in the Spring Mountains in southern Nevada, provide habitat for endangered spring snail species including the southeast Nevada Pyrg (Pyrgulopsis turbatrix) and the...
Analysis of summer water temperatures of the lower Virgin River near Mesquite, Nevada, 2019–21 Analysis of summer water temperatures of the lower Virgin River near Mesquite, Nevada, 2019–21
The lower Virgin River is a sandy, shallow reach of the Virgin River that flows from northern Arizona to Lake Mead in Nevada. The Virgin River hosts several native fish species, including two endangered fish, woundfin (Plagopterus argentissimu) and Virgin River chub (Gila seminuda). All native fish species in the lower Virgin River have experienced reductions in population sizes in the...
Authors
Katherine J. Earp
Evaporation from Lake Mead and Lake Mohave, Nevada and Arizona, 2010–2019 Evaporation from Lake Mead and Lake Mohave, Nevada and Arizona, 2010–2019
Evaporation-rate estimates at Lake Mead and Lake Mohave, Nevada and Arizona, were based on eddy covariance and available energy measurements from March 2010 through April 2019 at Lake Mead and May 2013 through April 2019 at Lake Mohave. The continuous data needed to compute monthly evaporation were collected from floating-platform and land-based measurement stations located at each...
Authors
Katherine J. Earp, Michael T. Moreo
Evaporation from Lake Mead, Nevada and Arizona, March 2010 through February 2012 Evaporation from Lake Mead, Nevada and Arizona, March 2010 through February 2012
Evaporation from Lake Mead was measured using the eddy-covariance method for the 2-year period starting March 2010 and ending February 2012. When corrected for energy imbalances, annual eddy-covariance evaporation was 2,074 and 1,881 millimeters (81.65 and 74.07 inches), within the range of previous estimates. There was a 9-percent decrease in the evaporation rate and a 10-percent...
Authors
Michael T. Moreo, Amy Swancar
Science and Products
Evaporation from Lake Mead and Lake Mohave, Lower Colorado River Basin, Nevada and Arizona
Since 2010, the U.S. Geological Survey (USGS) Nevada Water Science Center (NVWSC) has worked with with the Bureau of Reclamation to update evaporation estimates for Lake Mead.
Near-Continuous Depth-Dependent Water-Quality Data from Automatic Profiling Systems and Meteorological Data, Lakes Mead and Mohave, Arizona and Nevada, USA
The Colorado River is one of the most intensely used rivers in the western United States, providing recreational watercraft activities and domestic drinking, industrial, and irrigation water for over 22 million users in the desert southwest. The quality of this water must be maintained to guarantee a reliable and safe resource for its many uses. The Colorado River provides an estimated 97 percent...
Science in the Colorado River Basin
The Colorado River is one of the longest rivers in the Western United States. It begins in the Rocky Mountains of Colorado and flows southwestward until it reaches Mexico where it becomes a small stream or dry riverbed. The Colorado River forms the border between southeastern Nevada and northwestern Arizona. In Nevada, Hoover Dam and Davis Dam control the flow of the river and create two...
Evaluating Potential Refugia for the Endangered Mohave Tui Chub
The USGS Nevada Water Science Center (NVWSC), in partnership with the National Park Service (NPS), is evaluating and monitoring the basic water quality and sediment chemistry of two proposed refugia and three established habitats for the endangered Mohave Tui Chub over the course of the year. NVWSC will also compare and evaluate findings to U.S. Environmental Protection Agency screening levels and...
Groundwater Discharge by Evapotranspiration from Areas of Spring-Fed Riparian Vegetation, Stump Spring and Hiko Springs, Nev.
Stump Spring has been designated as an Area of Critical Environmental Concern by the Bureau of Land Management (BLM), and Hiko Springs currently is in the designation process. Both springs flow intermittently in drainages where the depth to groundwater is shallow. The shallow groundwater flowing to and from the springs sustain scarce desert riparian habitats. BLM has recognized a need for accurate...
Groundwater Discharge by Evapotranspiration, Flow of Water in Unsaturated Soil, and Stable Isotope Water Sourcing in Areas of Sparse Vegetation, Amargosa Desert, Nye County, Nevada
The USGS conducted a study to evaluate the potential for groundwater discharge from sparsely vegetated areas in the Amargosa Desert. The study objectives were to: (1) compute groundwater discharge based on evapotranspiration and precipitation measurements at instrumented sites, and (2) improve understanding of hydrologic-continuum processes controlling groundwater discharge through analysis of...
Water Quality of Springs in the Spring Mountains
The USGS Nevada Water Science Center, in cooperation with the Bureau of Land Management, is sampling and analyzing water from Grapevine, Kiup, and Rainbow Springs to determine the source of water to these springs. These Springs, located in the Spring Mountains in southern Nevada, provide habitat for endangered spring snail species including the southeast Nevada Pyrg (Pyrgulopsis turbatrix) and the...
Analysis of summer water temperatures of the lower Virgin River near Mesquite, Nevada, 2019–21 Analysis of summer water temperatures of the lower Virgin River near Mesquite, Nevada, 2019–21
The lower Virgin River is a sandy, shallow reach of the Virgin River that flows from northern Arizona to Lake Mead in Nevada. The Virgin River hosts several native fish species, including two endangered fish, woundfin (Plagopterus argentissimu) and Virgin River chub (Gila seminuda). All native fish species in the lower Virgin River have experienced reductions in population sizes in the...
Authors
Katherine J. Earp
Evaporation from Lake Mead and Lake Mohave, Nevada and Arizona, 2010–2019 Evaporation from Lake Mead and Lake Mohave, Nevada and Arizona, 2010–2019
Evaporation-rate estimates at Lake Mead and Lake Mohave, Nevada and Arizona, were based on eddy covariance and available energy measurements from March 2010 through April 2019 at Lake Mead and May 2013 through April 2019 at Lake Mohave. The continuous data needed to compute monthly evaporation were collected from floating-platform and land-based measurement stations located at each...
Authors
Katherine J. Earp, Michael T. Moreo
Evaporation from Lake Mead, Nevada and Arizona, March 2010 through February 2012 Evaporation from Lake Mead, Nevada and Arizona, March 2010 through February 2012
Evaporation from Lake Mead was measured using the eddy-covariance method for the 2-year period starting March 2010 and ending February 2012. When corrected for energy imbalances, annual eddy-covariance evaporation was 2,074 and 1,881 millimeters (81.65 and 74.07 inches), within the range of previous estimates. There was a 9-percent decrease in the evaporation rate and a 10-percent...
Authors
Michael T. Moreo, Amy Swancar