Flow Reports by State
Flow Report - UNITED STATES
May 1 2024
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Flow Reports by State
Flow Reports by State
Flood Monitor
|
Neosho River
River / Tributary |
464% |
|
Suwannee River
River / Tributary |
196% |
|
Grand River
River / Tributary |
380% |
|
Portneuf River
River / Tributary |
182% |
|
Sabine River
River / Tributary |
271% |
|
Sulphur River
River / Tributary |
243% |
|
Blackwater River
River / Tributary |
471% |
|
Navasota River
River / Tributary |
666% |
|
Owyhee River
River / Tributary |
377% |
|
Humboldt River
River / Tributary |
243% |
|
Marmaton River
River / Tributary |
378% |
|
Trinity River
River / Tributary |
338% |
|
Missouri River
River / Tributary |
209% |
|
South Fabius River
River / Tributary |
466% |
|
Neches River
River / Tributary |
202% |
|
Calcasieu River
River / Tributary |
253% |
|
Brazos River
River / Tributary |
981% |
|
Bird
Watershed |
2301% |
|
Blackwater
Watershed |
471% |
|
Lower Suwannee
Watershed |
196% |
|
Middle Sabine
Watershed |
461% |
|
West Fork San Jacinto
Watershed |
1008% |
|
East Fork San Jacinto
Watershed |
2355% |
|
Lower Sulphur
Watershed |
243% |
|
Sulphur Headwaters
Watershed |
276% |
|
Lower Marais Des Cygnes
Watershed |
447% |
|
Little Osage
Watershed |
470% |
|
Marmaton
Watershed |
378% |
|
Navasota
Watershed |
666% |
|
Lower Neches
Watershed |
204% |
|
Upper Neches
Watershed |
157% |
|
Village
Watershed |
1537% |
|
Upper Calcasieu
Watershed |
253% |
|
Middle Humboldt
Watershed |
243% |
|
Upper Trinity
Watershed |
348% |
|
South Fork Salt
Watershed |
379% |
|
La Moine
Watershed |
568% |
|
Portneuf
Watershed |
182% |
|
South Fabius
Watershed |
466% |
|
Lower Grand
Watershed |
380% |
|
Lower Missouri-Moreau
Watershed |
201% |
|
Lower Trinity
Watershed |
239% |
|
Lower Trinity-Kickapoo
Watershed |
463% |
|
Polecat-Snake
Watershed |
2440% |
|
Lake O'Cherokees
Watershed |
392% |
|
Middle Neosho
Watershed |
545% |
|
Upper Sabine
Watershed |
373% |
|
Lake Fork
Watershed |
381% |
|
Lower Sabine
Watershed |
230% |
|
Middle Brazos-Palo Pinto
Watershed |
981% |
|
Buffalo-San Jacinto
Watershed |
1260% |
|
Los Angeles
Watershed |
658% |
|
Middle Neches
Watershed |
205% |
|
Lower Owyhee
Watershed |
377% |
|
Lower Missouri
Watershed |
226% |
Surging Streamflows
| Streamgauge | Percent Increase | Discharge |
|---|---|---|
| JOE CREEK AT 61ST ST AT TULSA, OK | +33,411% | 4,390cfs |
| LITTLE HAIKEY CREEK AT 101ST ST SOUTH AT TULSA, OK | +25,187% | 1,320cfs |
| HAIKEY CREEK AT 101ST ST SOUTH AT TULSA, OK | +15,947% | 1,380cfs |
| BLACK WARRIOR RIVER AT NORTHPORT AL | +2,799% | 5,480cfs |
| SOUTH PLATTE RIVER NEAR CROOK, CO. | +1,365% | 1,480cfs |
| BRAZOS RV NR PALO PINTO, TX | +1,303% | 10,300cfs |
| PAINT ROCK RIVER NEAR WOODVILLE AL | +1,167% | 2,230cfs |
| BRAZOS RV NR GRAFORD, TX | +1,065% | 8,600cfs |
| MILWAUKEE R @ JONES ISLAND MOUTH-AT MILWAUKEE, WI | +941% | 17,600cfs |
| E FK SAN JACINTO RV NR NEW CANEY, TX | +522% | 18,300cfs |
What is a Streamgage?
Surface flow data in the US is crucial for managing our water resources sustainably. Thousands of streamgages across the nation provide vital insight for understanding hydrological patterns, forecasting floods and droughts, and guiding water management decisions. But what is a streamgage exactly?
Strong El Nino Climate Pattern
Oceanic Nino Index
The Oceanic Niño Index (ONI) is a rolling 3-month average temperature anomaly, and used for tracking El Niño-Southern Oscillation climate patterns. Based on the latest data for the last 3 months (JFM), the Oceanic Nino Index is currently 1.5, signifying a strong El Nino period. A persistent above average sea surface temperature may signify an El Niño episode. Conversely, a below average sea surface temperature will signal the onset of La Nina occurences.
Popular Whitewater Destinations
Featured river runs and paddling destinations
| Location | Discharge | Status |
|---|---|---|
| GREENWOOD TO MAMMOTH BAR | 1,390cfs | Runnable |
| TUNNEL RUN (RALSTON POWERHOUSE TO GREENWOOD) | 1,390cfs | Runnable |
| GENERATION AND GIANT GAPS (TADPOLE TO COLFAX-IOWA HILL ROAD) | 1,390cfs | Runnable |
| YANKEE JIM ROAD TO PONDEROSA WAY (SHIRTTAIL) | 1,390cfs | Runnable |
| CHILI BAR | 1,390cfs | Runnable |
| COLOMA TO GREENWOOD - (C TO G) | 1,390cfs | Runnable |
| SUNRISE AVENUE TO WATT AVENUE | 1,020cfs | Too High |
| ROYAL GORGE (SODA SPRINGS TO TADPOLE CREEK) | 817cfs | Runnable |
| CHRISTOPHER CREEK | 443cfs | Too High |
| INDIAN GARDENS | 30cfs | Too Low |
Flood Monitoring
The consequences of floods are far-reaching and can be devastating. Property damage, destruction of critical infrastructure, disruption of transportation networks, and loss of human life are all significant impacts of flooding events. Communities may experience prolonged displacement, economic hardships, and increased vulnerability to subsequent disasters.
Highest Streamflows
Top streamflows across the nation
| Location | Discharge |
|---|---|
| MISSISSIPPI RIVER AT VICKSBURG, MS | 918,000cfs |
| MISSISSIPPI RIVER AT BATON ROUGE, LA | 788,000cfs |
| MISSISSIPPI RIVER AT MEMPHIS, TN | 551,000cfs |
| MISSISSIPPI RIVER AT ST. LOUIS, MO | 464,000cfs |
| MISSISSIPPI RIVER AT CHESTER, IL | 433,000cfs |
| MISSISSIPPI RIVER AT THEBES, IL | 417,000cfs |
| (COE) ATCHAFALAYA RIVER AT SIMMESPORT, LA | 337,000cfs |
| MISSOURI RIVER AT ST. CHARLES, MO | 295,000cfs |
| MISSOURI RIVER AT HERMANN, MO | 275,000cfs |
Some notable tributaries with traditionally high stream flow include the mighty Mississippi, the iconic Colorado, and the scenic Columbia. In addition, there are numerous reservoirs and dams across the country that play a pivotal role in water storage and distribution. Understanding surface flow data is critical for ensuring water security and supporting sustainable development.
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