USGS hydrologic technician Aliesha Bradford measures streamflow on Warm Springs Creek near Mackay, Idaho. Photo by Ryan Moore, USGS.
Sometimes the USGS real-time stage data seems too high (or too low). Are the USGS data inaccurate?
There can be occasional equipment or database problems where erroneous data are reported for short periods of time until corrections can be made. This is why it is important to look at a record of streamflow (like the 7-day hydrograph plots) rather than a single point in time. However, most of the time the USGS has a high level of confidence in its real-time stage data.
During low streamflow conditions, aquatic grasses, debris, or rocks near the gage can produce artificial increases in water level readings. During extreme cold weather, ice can affect stage and discharge determinations at some stations. Adjustment of data for ice effects requires detailed analysis.
Learn more:
- National Water Information System (NWIS) Mapper - Active USGS Surface Water sites with data
- Streamgaging Basics
Related
How often are real-time streamflow data updated?
Is there a way to get alerts about streamflow conditions?
How can I obtain river forecasts (flood forecasts)?
Does "stage" tell you how much water is flowing in a stream?
What does the term "stream stage" mean?
Why are there sometimes differences between USGS and National Weather Service river stages?
How is a rating curve used to convert gage height into streamflow?
Why might USGS streamflow data be revised?
Where can I get real-time and historical streamflow information?
Why do some real-time streamgaging stations stop transmitting data for extended periods of time?
How do we benefit from USGS streamgages?

USGS hydrologic technician Aliesha Bradford measures streamflow on Warm Springs Creek near Mackay, Idaho. Photo by Ryan Moore, USGS.
USGS hydrographer measuring streamflow using a handheld Acoustic Doppler Velocimeter in fast moving floodwater Cajon Creek near Keenbrook, California.
USGS hydrographer measuring streamflow using a handheld Acoustic Doppler Velocimeter in fast moving floodwater Cajon Creek near Keenbrook, California.

U.S. Geological Survey Hydrologic Technician Patrick Anzman installs a new streamgage February 23 over the Schuylkill River in the Philadelphia neighborhood of Manayunk. Photo by Mason Manis, USGS.
U.S. Geological Survey Hydrologic Technician Patrick Anzman installs a new streamgage February 23 over the Schuylkill River in the Philadelphia neighborhood of Manayunk. Photo by Mason Manis, USGS.
Ice jam on Little Wind River Ice jam on Little Wind River (06235500), February 2017. Streamgage destoryed soon after photo taken.
Ice jam on Little Wind River Ice jam on Little Wind River (06235500), February 2017. Streamgage destoryed soon after photo taken.
Neil Yobbi, U.S. Geological Survey hydrologic technician, uses an Acoustic Doppler Velocimeter to measure stream flow on Curlew Creek in Tampa, Florida. While Hurricane Hermine might have made landfall almost 200 miles away in St.
Neil Yobbi, U.S. Geological Survey hydrologic technician, uses an Acoustic Doppler Velocimeter to measure stream flow on Curlew Creek in Tampa, Florida. While Hurricane Hermine might have made landfall almost 200 miles away in St.
Ice jam at White River near Interior, SD (USGS streamgage 06446500). More information on this site is available at https://waterdata.usgs.gov/sd/nwis/inventory/?site_no=06446500&agency_cd=USGS&.
Ice jam at White River near Interior, SD (USGS streamgage 06446500). More information on this site is available at https://waterdata.usgs.gov/sd/nwis/inventory/?site_no=06446500&agency_cd=USGS&.
On February 26, Nick Stasulis and Charlie Culbertson visited USGS station 01054200 Wild River at Gilead, Maine to make a streamflow measurement through the ice. For these measurements, 20-30 holes are drilled through the ice and a current meter (the spinning yellow cups) is used to measure velocity. River depths and distance across the channel are also measured.
On February 26, Nick Stasulis and Charlie Culbertson visited USGS station 01054200 Wild River at Gilead, Maine to make a streamflow measurement through the ice. For these measurements, 20-30 holes are drilled through the ice and a current meter (the spinning yellow cups) is used to measure velocity. River depths and distance across the channel are also measured.
Jeff Bailes (foreground) of the USGS Colorado Science Center disassembles streamflow-measuring equipment on the Big Thompson River while Ben Glass (background) inspects a USGS rapid deployment streamgage. The river is one of many that flooded during a significant September 2013 rain event along Colorado's Front Range, damaging or destroying several USGS streamg
Jeff Bailes (foreground) of the USGS Colorado Science Center disassembles streamflow-measuring equipment on the Big Thompson River while Ben Glass (background) inspects a USGS rapid deployment streamgage. The river is one of many that flooded during a significant September 2013 rain event along Colorado's Front Range, damaging or destroying several USGS streamg

USGS employee, Hanna Coy, talks about stream gauging.
USGS employee, Hanna Coy, talks about stream gauging.

A rainbow over the USGS streamflow station gage house at the outlet of Bass Harbor Marsh in Maine (monitoring location 010228955).
A rainbow over the USGS streamflow station gage house at the outlet of Bass Harbor Marsh in Maine (monitoring location 010228955).
Whether you drink water from your tap, use electricity or canoe down your local river, chances are you benefit from USGS streamgage information. So what is a streamgage and what does it do for you? This CoreCast episode gives you the inside scoop on your silent superhero.
Transcript and captions available soon.
Whether you drink water from your tap, use electricity or canoe down your local river, chances are you benefit from USGS streamgage information. So what is a streamgage and what does it do for you? This CoreCast episode gives you the inside scoop on your silent superhero.
Transcript and captions available soon.
Pew Creek below Johnson Road, Lawrenceville, Ga. The metal structure is a "V" weir. A sediment dam was built on either side of it to force the water through the weir. Scientists can calculate gallons per minute flow in the stream by timing how long the flow took to fill a bucket.
Pew Creek below Johnson Road, Lawrenceville, Ga. The metal structure is a "V" weir. A sediment dam was built on either side of it to force the water through the weir. Scientists can calculate gallons per minute flow in the stream by timing how long the flow took to fill a bucket.
USGS Oklahoma Water Science Center Hydrologic Technician Rick Hanlon prepares to conduct a streamflow measurement off of a bridge over the North Canadian River near Oklahoma City.
USGS Oklahoma Water Science Center Hydrologic Technician Rick Hanlon prepares to conduct a streamflow measurement off of a bridge over the North Canadian River near Oklahoma City.
A model uncertainty quantification protocol for evaluating the value of observation data
Compilation of streamflow statistics calculated from daily mean streamflow data collected during water years 1901–2015 for selected U.S. Geological Survey streamgages
U.S. Geological Survey water resources Internet tools
How does a U.S. Geological Survey streamgage work?
Discharge measurements at gaging stations
From the River to You: USGS Real-Time Streamflow Information...from the National Streamflow Information Program
StreamStats: A U.S. Geological Survey Web Application for Stream Information
The stream-gaging program of the U.S. Geological Survey
Related
How often are real-time streamflow data updated?
Is there a way to get alerts about streamflow conditions?
How can I obtain river forecasts (flood forecasts)?
Does "stage" tell you how much water is flowing in a stream?
What does the term "stream stage" mean?
Why are there sometimes differences between USGS and National Weather Service river stages?
How is a rating curve used to convert gage height into streamflow?
Why might USGS streamflow data be revised?
Where can I get real-time and historical streamflow information?
Why do some real-time streamgaging stations stop transmitting data for extended periods of time?
How do we benefit from USGS streamgages?

USGS hydrologic technician Aliesha Bradford measures streamflow on Warm Springs Creek near Mackay, Idaho. Photo by Ryan Moore, USGS.
USGS hydrologic technician Aliesha Bradford measures streamflow on Warm Springs Creek near Mackay, Idaho. Photo by Ryan Moore, USGS.
USGS hydrographer measuring streamflow using a handheld Acoustic Doppler Velocimeter in fast moving floodwater Cajon Creek near Keenbrook, California.
USGS hydrographer measuring streamflow using a handheld Acoustic Doppler Velocimeter in fast moving floodwater Cajon Creek near Keenbrook, California.

U.S. Geological Survey Hydrologic Technician Patrick Anzman installs a new streamgage February 23 over the Schuylkill River in the Philadelphia neighborhood of Manayunk. Photo by Mason Manis, USGS.
U.S. Geological Survey Hydrologic Technician Patrick Anzman installs a new streamgage February 23 over the Schuylkill River in the Philadelphia neighborhood of Manayunk. Photo by Mason Manis, USGS.
Ice jam on Little Wind River Ice jam on Little Wind River (06235500), February 2017. Streamgage destoryed soon after photo taken.
Ice jam on Little Wind River Ice jam on Little Wind River (06235500), February 2017. Streamgage destoryed soon after photo taken.
Neil Yobbi, U.S. Geological Survey hydrologic technician, uses an Acoustic Doppler Velocimeter to measure stream flow on Curlew Creek in Tampa, Florida. While Hurricane Hermine might have made landfall almost 200 miles away in St.
Neil Yobbi, U.S. Geological Survey hydrologic technician, uses an Acoustic Doppler Velocimeter to measure stream flow on Curlew Creek in Tampa, Florida. While Hurricane Hermine might have made landfall almost 200 miles away in St.
Ice jam at White River near Interior, SD (USGS streamgage 06446500). More information on this site is available at https://waterdata.usgs.gov/sd/nwis/inventory/?site_no=06446500&agency_cd=USGS&.
Ice jam at White River near Interior, SD (USGS streamgage 06446500). More information on this site is available at https://waterdata.usgs.gov/sd/nwis/inventory/?site_no=06446500&agency_cd=USGS&.
On February 26, Nick Stasulis and Charlie Culbertson visited USGS station 01054200 Wild River at Gilead, Maine to make a streamflow measurement through the ice. For these measurements, 20-30 holes are drilled through the ice and a current meter (the spinning yellow cups) is used to measure velocity. River depths and distance across the channel are also measured.
On February 26, Nick Stasulis and Charlie Culbertson visited USGS station 01054200 Wild River at Gilead, Maine to make a streamflow measurement through the ice. For these measurements, 20-30 holes are drilled through the ice and a current meter (the spinning yellow cups) is used to measure velocity. River depths and distance across the channel are also measured.
Jeff Bailes (foreground) of the USGS Colorado Science Center disassembles streamflow-measuring equipment on the Big Thompson River while Ben Glass (background) inspects a USGS rapid deployment streamgage. The river is one of many that flooded during a significant September 2013 rain event along Colorado's Front Range, damaging or destroying several USGS streamg
Jeff Bailes (foreground) of the USGS Colorado Science Center disassembles streamflow-measuring equipment on the Big Thompson River while Ben Glass (background) inspects a USGS rapid deployment streamgage. The river is one of many that flooded during a significant September 2013 rain event along Colorado's Front Range, damaging or destroying several USGS streamg

USGS employee, Hanna Coy, talks about stream gauging.
USGS employee, Hanna Coy, talks about stream gauging.

A rainbow over the USGS streamflow station gage house at the outlet of Bass Harbor Marsh in Maine (monitoring location 010228955).
A rainbow over the USGS streamflow station gage house at the outlet of Bass Harbor Marsh in Maine (monitoring location 010228955).
Whether you drink water from your tap, use electricity or canoe down your local river, chances are you benefit from USGS streamgage information. So what is a streamgage and what does it do for you? This CoreCast episode gives you the inside scoop on your silent superhero.
Transcript and captions available soon.
Whether you drink water from your tap, use electricity or canoe down your local river, chances are you benefit from USGS streamgage information. So what is a streamgage and what does it do for you? This CoreCast episode gives you the inside scoop on your silent superhero.
Transcript and captions available soon.
Pew Creek below Johnson Road, Lawrenceville, Ga. The metal structure is a "V" weir. A sediment dam was built on either side of it to force the water through the weir. Scientists can calculate gallons per minute flow in the stream by timing how long the flow took to fill a bucket.
Pew Creek below Johnson Road, Lawrenceville, Ga. The metal structure is a "V" weir. A sediment dam was built on either side of it to force the water through the weir. Scientists can calculate gallons per minute flow in the stream by timing how long the flow took to fill a bucket.
USGS Oklahoma Water Science Center Hydrologic Technician Rick Hanlon prepares to conduct a streamflow measurement off of a bridge over the North Canadian River near Oklahoma City.
USGS Oklahoma Water Science Center Hydrologic Technician Rick Hanlon prepares to conduct a streamflow measurement off of a bridge over the North Canadian River near Oklahoma City.