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Filters: Types: Citation (X) > partyWithName: U.S. Geological Survey (X) > partyWithName: Karen R Ryberg (X)

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A comma separated values (csv) file that is a snapshot of the U.S. Geological Survey peak flow file on November 19, 2008. The file lists agency, station identification, water year, peak date, peak values, peak qualification codes, gage height values, gage height qualification codes and year of last peak for all stream gaging stations for which peak streamflow has been recorded.
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A comma separated values (csv) file that is a snapshot of percent difference between November 19, 2008 and November 14, 2016 peak streamflow. The file lists station identification, water year, original (2008) peak Q, current (2016) peak Q and percent difference calculated per water year. The percent difference was calculated as the absolute value of [(current peak Q - original peak Q)/(original peak Q) x 100], where current peak Q is the 2016 peak and the original peak Q is the 2008 peak. When an original peak Q value is 0, the resultant percent difference calculation is undefined because of division by 0. In these cases, the percent difference field is populated with NA. Those entries are included in the data file...
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A comma separated values (csv) file that is a snapshot of the U.S. Geological Survey peak flow file on November 14, 2016. The file lists agency, station identification, water year, peak date, peak values, peak qualification codes, gage height values, gage height qualification codes, and year of last peak for all stream gaging stations for which peak streamflow has been recorded.
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These data provide a public summary of the changes made to the U.S. Geological Survey peak-flow file since formal Nation-wide checking began in 2008. Coverage includes peak-flow sites in the United States and territories.
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The Red River of the North (Red River) transports phosphorus from North Dakota, Minnesota, and South Dakota, to Manitoba, Canada, and eventually into Lake Winnipeg. Phosphorus load (or flux) is the amount of total phosphorus (TP) transported by the Red River. The effect of TP load on water quality is a concern, especially with respect to downstream eutrophication issues in Lake Winnipeg, Manitoba, Canada. There is interest at the State and International level to reduce TP flux – an expensive proposition, depending on the method (controlling sources, settling ponds, buffer strips, changes in land use) that is not always effective during spring runoff. The purpose of the study for which these data were developed...


    map background search result map search result map Total Phosphorus Load and Ancillary Data Related to Sources of Total Phosphorus in the Red River of the North Basin Data Documenting the U.S. Geological Survey Peak-Flow File Data Verification Project, 2008-16 Peak Flow File November 14 2016 Peak Flow File November 19 2008 Percentage Differences Streamflow Total Phosphorus Load and Ancillary Data Related to Sources of Total Phosphorus in the Red River of the North Basin Peak Flow File November 14 2016 Peak Flow File November 19 2008 Percentage Differences Streamflow Data Documenting the U.S. Geological Survey Peak-Flow File Data Verification Project, 2008-16