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23 result(s) for “date 2020 site support mozilla org site computed zeitung de site:www.usgs.gov” · 797 ms

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Study Sites: Site 1: Colorado River below Hoover Dam Site
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https://www.usgs.gov/staff-profiles/jon-mason
Study Sites: Site 1: Colorado River below Hoover Dam Site

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https://www.usgs.gov/staff-profiles/liam-schenk
Geological Survey (USGS) computes time-series of total phosphorus (TP) and suspended-sediment concentrations (SSC) and loads entering Upper Klamath Lake using continuous turbidity sensor records, discrete TP and SSC data, and continuously computed streamflow

Estimation of Dissolved-Solids Concentrations Using Continuous Water

https://www.usgs.gov/centers/arizona-water-science-center/science/estimation-dissolved-solids-concentrations-using
The study developed site-specific relations of specific conductance, water temperature, and dissolved-solids concentrations at four monitoring sites in the Yuma area between Imperial Dam and the United States–Mexico southerly international boundary to predict dissolved-solids concentrations using surrogate

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https://www.usgs.gov/streamstats/streamstats-fundamentals
StreamStats incorporates (1) a map-based user interface for the site selection; (2) a relational data base that contains information for data-collection stations and regression equations used to estimate flow statistics for ungaged sites; (3) a GIS program that allows locating sites of interest in the user interface

Estimation of dissolved-solids concentrations using continuous water

https://www.usgs.gov/publications/estimation-dissolved-solids-concentrations-using-continuous-water-quality-monitoring
The continuous specific conductance data for the site downstream from Cooper wasteway were corrected using mean specific conductance values computed from cross-section measurements collected during site visits

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https://www.usgs.gov/mission-areas/water-resources/peakfq-software-user-notice
   Based on current understanding (March 17, 2022), the impacts of the identified issues on most at-site flood frequency estimates, and to an even lesser extent USGS regional regression equations, appear to be limited

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https://www.usgs.gov/streamstats/data
txt) for the respective periods of record (through the 2020 or 2021 water year) for seven USGS streamgages in the upper Esopus Creek watershed in upstate New York

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https://www.usgs.gov/streamstats/common-user-questions
In a series of estimated flow statistics for an ungaged site, such as peak-flows at various recurrence intervals or flow-duration statistics, why do I sometimes get estimates for lower flows that are higher than estimates for higher flows

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https://www.usgs.gov/staff-profiles/james-leenhouts
Recharge potential is not independently measurable, but is instead formulated as a site-specific, qualitative parameter

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https://www.usgs.gov/observatories/hvo/science/monitoring-earthquakes-hawaii
This type of seismometer is significantly more expensive than other options and is more sensitive to local site conditions

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https://www.usgs.gov/special-topic/water-science-school/science/100-year-flood
Likewise, using a frequency analysis (Interagency Advisory Committee on Water Data, 1982) there is a 1 in 100 chance that a streamflow of 15,000 cubic feet per second (ft3/s) will occur during any year at a certain streamflow-measurement site

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https://www.usgs.gov/special-topics/water-science-school/science/water-science-glossary
Here's a list of water-related terms, compiled from several different resources, that might help you understand our site better

Near-field remote sensing of surface velocity and river discharge using

https://www.usgs.gov/publications/near-field-remote-sensing-surface-velocity-and-river-discharge-using-radars-and
Near-field remote sensing of surface velocity and river discharge using radars and the probability concept at 10 USGS streamgages | U

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https://www.usgs.gov/centers/florence-bascom-geoscience-center/science/holocene-synthesis-project
gov website belongs to an official government organization in the United States

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https://www.usgs.gov/data/data-potomac-river-watershed-accumulated-wastewater-viewer
gov website belongs to an official government organization in the United States

Shallow lake, strong shake: Record of seismically triggered lacustrine

https://www.usgs.gov/publications/shallow-lake-strong-shake-record-seismically-triggered-lacustrine-sedimentation-1959
gov website belongs to an official government organization in the United States

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https://www.usgs.gov/streamstats/news/streamstats-version-4300-released
gov website belongs to an official government organization in the United States

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https://www.usgs.gov/staff-profiles/kenneth-fossum
gov website belongs to an official government organization in the United States

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https://www.usgs.gov/water-science-school/science/monthly-and-yearly-streamflow-patterns
gov website belongs to an official government organization in the United States

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https://www.usgs.gov/special-topic/water-science-school/science/how-streamflow-measured
In general, river discharge is computed by multiplying the area of water in a channel cross section by the average velocity of the water in that cross section: discharge = area x velocity The USGS uses numerous methods and types of equipment to measure velocity and cross-sectional area, including the following current

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https://www.usgs.gov/centers/california-water-science-center/science/klamath-dam-removal-studies
gov website belongs to an official government organization in the United States

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https://www.usgs.gov/centers/western-geographic-science-center/science/aridland-water-harvesting-study
gov website belongs to an official government organization in the United States

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https://www.usgs.gov/centers/pcmsc/science/global-seabed-mineral-resources
gov website belongs to an official government organization in the United States