USGS hydrologic technician Aliesha Bradford measures streamflow on Warm Springs Creek near Mackay, Idaho. Photo by Ryan Moore, USGS.
How is a rating curve used to convert gage height into streamflow?
In order to convert gage height (or "stage", usually expressed as feet) into streamflow (or "discharge", usually expressed as cubic feet per second), USGS hydrographers must establish a relationship between them. This stage-discharge relationship is called a rating curve. It’s developed by making frequent manual discrete discharge measurements at stream gaging stations.
The rating curve depends on the physical characteristics of the stream channel and floodplain, and will vary over time at almost every station. There are often subtle changes to a natural stream channel, such as the growth of aquatic vegetation in the summer, frequent shifting of a sand-bed stream bottom, catastrophic changes due to floods, or man-made changes such as construction of a bridge. These changes might require only minor or temporary adjustments to the rating curve, or they could require the development of a new one.
Provisional rating curves for many USGS streamgages are posted in WaterWatch. Place your cursor over the site of interest and left-click. That generates a pop-up window with a rating tab on the far right. Or if you know the site number for a USGS streamgage, plug it into the Customized Rating Curve Builder. For more information about site-specific rating curves, contact the USGS Water Science Center that manages the site.
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Related
Is there a way to get alerts about streamflow conditions? Is there a way to get alerts about streamflow conditions?
Yes! The U.S. Geological Survey WaterAlert service provides notifications to your email or phone for changes in water conditions based on thresholds you choose.
What does the term "stream stage" mean? What does the term "stream stage" mean?
Stream stage (aka gage height) is an important concept when analyzing how much water is moving in a stream at any given moment. "Stage" is the water level above some arbitrary point in the river and is commonly measured in feet. For example, on a normal day when no rain has fallen for a while, a river might have a stage of 2 feet. If a big storm hits, the river stage could rise to 15 or 20 feet...
Does "stage" tell you how much water is flowing in a stream? Does "stage" tell you how much water is flowing in a stream?
Not directly. You cannot say that because a stream rises (doubles) from a 10-foot stage to a 20-foot stage that the amount of flowing water also doubles. Think of a cereal bowl with a rounded bottom. Pour one inch of milk in it. It doesn't take much milk to make it up to the one inch level because the bowl is at its narrowest near the bottom. Now, pour in milk until it is two inches deep -- it...
Why are there sometimes differences between USGS and National Weather Service river stages? Why are there sometimes differences between USGS and National Weather Service river stages?
At some USGS streamgage installations, NOAA’s National Weather Service (NWS) maintains a separate stage sensor that is serviced by NWS technicians. Calibration of any sensing device can occasionally drift from a "true" value, so there might be differences between USGS and NWS data reports. USGS personnel visit installations on an interval of 6 weeks or less to maintain equipment and make required...
Sometimes the USGS real-time stage data seems too high (or too low). Are the USGS data inaccurate? 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...
Where can I get real-time and historical streamflow information? Where can I get real-time and historical streamflow information?
Water Data for the Nation (WDFN) is the home for USGS streamflow, groundwater, and water quality data. Through WDFN you can find different tools to look at historic and real-time streamflow data, find sites of interest, and access using USGS water data application programming interfaces (APIs). State pages (e.g., California) allow you to discover real-time data in your state, or you can create a...
Why does the USGS use the spelling "gage" instead of "gauge"? Why does the USGS use the spelling "gage" instead of "gauge"?
The spelling of “gage” is part of our very rich USGS history. We have used that spelling for over a hundred years. In 1888, USGS Director John Wesley Powell met a very forward-thinking graduate student named Frederick Haynes Newell. Powell was so impressed that he made Newell the first full-time appointee to the new Irrigation Survey, which was created to investigate the potential for dams and...
Why might USGS streamflow data be revised? Why might USGS streamflow data be revised?
Real-time USGS streamflow data are PROVISIONAL, meaning that the data have not been reviewed or edited. These data might be subject to significant change and are not official until reviewed and approved by the USGS. Real-time streamflow data can be affected by: backwater from ice or debris such as log jams algae and aquatic growth in the stream sediment movement malfunction of recording equipment...
Measuring Streamflow on Warm Springs Creek near Mackay, Idaho
USGS hydrologic technician Aliesha Bradford measures streamflow on Warm Springs Creek near Mackay, Idaho. Photo by Ryan Moore, USGS.
Hydrologic technician measures streamflow in Tokul Creek
USGS Hydrologic Technician Katie Johnson measures streamflow in Tokul Creek near Snoqualmie, WA (12145000).
USGS Hydrologic Technician Katie Johnson measures streamflow in Tokul Creek near Snoqualmie, WA (12145000).
Taking streamflow measurements in Acadia National Park
Hydrologic technician is taking streamflow measurements in Acadia National Park. A small creek is surrounded by grass and green foliage.
Hydrologic technician is taking streamflow measurements in Acadia National Park. A small creek is surrounded by grass and green foliage.
Hydrologic Technician makes a wading streamflow measurement during a spring flood event at Siskiwit Falls at Cornucopia, Wisconsin
linkHydrologic Technician Brandon Nelson makes a wading streamflow measurement during a spring flood event at Siskiwit Falls at Cornucopia, Wisconsin.
Hydrologic Technician makes a wading streamflow measurement during a spring flood event at Siskiwit Falls at Cornucopia, Wisconsin
linkHydrologic Technician Brandon Nelson makes a wading streamflow measurement during a spring flood event at Siskiwit Falls at Cornucopia, Wisconsin.
Measuring streamflow
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 Remnants
On April 29, hydrologic technicians Anthony Underwood and Jeremiah Pomerleau visited the USGS gaging station on the St. John River at Ninemile Bridge and found a sea of broken up, dirty ice left behind by a recent ice jam.
According to Anthony, photos don't do the size and scale of the ice chunks any justice.
On April 29, hydrologic technicians Anthony Underwood and Jeremiah Pomerleau visited the USGS gaging station on the St. John River at Ninemile Bridge and found a sea of broken up, dirty ice left behind by a recent ice jam.
According to Anthony, photos don't do the size and scale of the ice chunks any justice.
Under The Ice
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.
Time-Lapse of Measuring Streamflow
This time-lapse photo shows the process that U.S. Geological Survey hydrographers use to measure streamflow across the cross-section of a wadeable river. USGS hydrographers follow standard, documented techniques and methods to ensure high-qualtiy, reliable data.
This time-lapse photo shows the process that U.S. Geological Survey hydrographers use to measure streamflow across the cross-section of a wadeable river. USGS hydrographers follow standard, documented techniques and methods to ensure high-qualtiy, reliable data.
Streamflow and Water Level Measurements
USGS scientists John Miller and Brent Hall measure the streamflow and water levels at the flooded Ditch 14 near Mapleton, ND. What appears to be a lake is actually a flooded cornfield.
USGS scientists John Miller and Brent Hall measure the streamflow and water levels at the flooded Ditch 14 near Mapleton, ND. What appears to be a lake is actually a flooded cornfield.
Measuring Streamflow
USGS hydrologic technician measuring streamflow in the Merced River, near Happy Isles stream gage in Yosemite Valley.
USGS hydrologic technician measuring streamflow in the Merced River, near Happy Isles stream gage in Yosemite Valley.
Streamgages: The Silent Superhero
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.
Related
Is there a way to get alerts about streamflow conditions? Is there a way to get alerts about streamflow conditions?
Yes! The U.S. Geological Survey WaterAlert service provides notifications to your email or phone for changes in water conditions based on thresholds you choose.
What does the term "stream stage" mean? What does the term "stream stage" mean?
Stream stage (aka gage height) is an important concept when analyzing how much water is moving in a stream at any given moment. "Stage" is the water level above some arbitrary point in the river and is commonly measured in feet. For example, on a normal day when no rain has fallen for a while, a river might have a stage of 2 feet. If a big storm hits, the river stage could rise to 15 or 20 feet...
Does "stage" tell you how much water is flowing in a stream? Does "stage" tell you how much water is flowing in a stream?
Not directly. You cannot say that because a stream rises (doubles) from a 10-foot stage to a 20-foot stage that the amount of flowing water also doubles. Think of a cereal bowl with a rounded bottom. Pour one inch of milk in it. It doesn't take much milk to make it up to the one inch level because the bowl is at its narrowest near the bottom. Now, pour in milk until it is two inches deep -- it...
Why are there sometimes differences between USGS and National Weather Service river stages? Why are there sometimes differences between USGS and National Weather Service river stages?
At some USGS streamgage installations, NOAA’s National Weather Service (NWS) maintains a separate stage sensor that is serviced by NWS technicians. Calibration of any sensing device can occasionally drift from a "true" value, so there might be differences between USGS and NWS data reports. USGS personnel visit installations on an interval of 6 weeks or less to maintain equipment and make required...
Sometimes the USGS real-time stage data seems too high (or too low). Are the USGS data inaccurate? 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...
Where can I get real-time and historical streamflow information? Where can I get real-time and historical streamflow information?
Water Data for the Nation (WDFN) is the home for USGS streamflow, groundwater, and water quality data. Through WDFN you can find different tools to look at historic and real-time streamflow data, find sites of interest, and access using USGS water data application programming interfaces (APIs). State pages (e.g., California) allow you to discover real-time data in your state, or you can create a...
Why does the USGS use the spelling "gage" instead of "gauge"? Why does the USGS use the spelling "gage" instead of "gauge"?
The spelling of “gage” is part of our very rich USGS history. We have used that spelling for over a hundred years. In 1888, USGS Director John Wesley Powell met a very forward-thinking graduate student named Frederick Haynes Newell. Powell was so impressed that he made Newell the first full-time appointee to the new Irrigation Survey, which was created to investigate the potential for dams and...
Why might USGS streamflow data be revised? Why might USGS streamflow data be revised?
Real-time USGS streamflow data are PROVISIONAL, meaning that the data have not been reviewed or edited. These data might be subject to significant change and are not official until reviewed and approved by the USGS. Real-time streamflow data can be affected by: backwater from ice or debris such as log jams algae and aquatic growth in the stream sediment movement malfunction of recording equipment...
Measuring Streamflow on Warm Springs Creek near Mackay, Idaho
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.
Hydrologic technician measures streamflow in Tokul Creek
USGS Hydrologic Technician Katie Johnson measures streamflow in Tokul Creek near Snoqualmie, WA (12145000).
USGS Hydrologic Technician Katie Johnson measures streamflow in Tokul Creek near Snoqualmie, WA (12145000).
Taking streamflow measurements in Acadia National Park
Hydrologic technician is taking streamflow measurements in Acadia National Park. A small creek is surrounded by grass and green foliage.
Hydrologic technician is taking streamflow measurements in Acadia National Park. A small creek is surrounded by grass and green foliage.
Hydrologic Technician makes a wading streamflow measurement during a spring flood event at Siskiwit Falls at Cornucopia, Wisconsin
linkHydrologic Technician Brandon Nelson makes a wading streamflow measurement during a spring flood event at Siskiwit Falls at Cornucopia, Wisconsin.
Hydrologic Technician makes a wading streamflow measurement during a spring flood event at Siskiwit Falls at Cornucopia, Wisconsin
linkHydrologic Technician Brandon Nelson makes a wading streamflow measurement during a spring flood event at Siskiwit Falls at Cornucopia, Wisconsin.
Measuring streamflow
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 Remnants
On April 29, hydrologic technicians Anthony Underwood and Jeremiah Pomerleau visited the USGS gaging station on the St. John River at Ninemile Bridge and found a sea of broken up, dirty ice left behind by a recent ice jam.
According to Anthony, photos don't do the size and scale of the ice chunks any justice.
On April 29, hydrologic technicians Anthony Underwood and Jeremiah Pomerleau visited the USGS gaging station on the St. John River at Ninemile Bridge and found a sea of broken up, dirty ice left behind by a recent ice jam.
According to Anthony, photos don't do the size and scale of the ice chunks any justice.
Under The Ice
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.
Time-Lapse of Measuring Streamflow
This time-lapse photo shows the process that U.S. Geological Survey hydrographers use to measure streamflow across the cross-section of a wadeable river. USGS hydrographers follow standard, documented techniques and methods to ensure high-qualtiy, reliable data.
This time-lapse photo shows the process that U.S. Geological Survey hydrographers use to measure streamflow across the cross-section of a wadeable river. USGS hydrographers follow standard, documented techniques and methods to ensure high-qualtiy, reliable data.
Streamflow and Water Level Measurements
USGS scientists John Miller and Brent Hall measure the streamflow and water levels at the flooded Ditch 14 near Mapleton, ND. What appears to be a lake is actually a flooded cornfield.
USGS scientists John Miller and Brent Hall measure the streamflow and water levels at the flooded Ditch 14 near Mapleton, ND. What appears to be a lake is actually a flooded cornfield.
Measuring Streamflow
USGS hydrologic technician measuring streamflow in the Merced River, near Happy Isles stream gage in Yosemite Valley.
USGS hydrologic technician measuring streamflow in the Merced River, near Happy Isles stream gage in Yosemite Valley.
Streamgages: The Silent Superhero
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.
Updated Date: March 13, 2025