Flow Reports by State
Flow Report - UNITED STATES
April 27 2024
Streamgauge | Percent Increase | Discharge |
---|---|---|
LITTLE OSAGE R. AT HORTON, MO | +40,580% | 3,710cfs |
BRUSH CREEK AT WARD PARKWAY IN KANSAS CITY, MO | +28,714% | 1,360cfs |
MARMATON RIVER NEAR NEVADA, MO | +13,395% | 4,440cfs |
CEDAR CREEK NEAR PLEASANT VIEW, MO | +10,903% | 3,730cfs |
LITTLE SAC RIVER NEAR MORRISVILLE, MO | +8,696% | 4,310cfs |
JAMES RIVER NEAR SPRINGFIELD, MO | +6,444% | 4,260cfs |
SPRING RIVER NEAR QUAPAW, OK | +4,117% | 14,800cfs |
SAC RIVER AT HWY J BELOW STOCKTON, MO | +2,621% | 2,430cfs |
TURNBACK CREEK ABOVE GREENFIELD, MO | +2,154% | 2,060cfs |
SAC RIVER NEAR CAPLINGER MILLS, MO | +1,931% | 3,920cfs |
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?
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.
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 |
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.
Location | Discharge |
---|---|
MISSISSIPPI RIVER AT VICKSBURG, MS | 947,000cfs |
MISSISSIPPI RIVER AT MEMPHIS, TN | 827,000cfs |
MISSISSIPPI RIVER AT BATON ROUGE, LA | 800,000cfs |
(COE) ATCHAFALAYA RIVER AT SIMMESPORT, LA | 342,000cfs |
OHIO RIVER AT OLD SHAWNEETOWN, IL-KY | 259,000cfs |
OHIO RIVER AT CANNELTON DAM AT CANNELTON, IN | 177,000cfs |
WAX LAKE OUTLET AT CALUMET, LA | 169,000cfs |
SAVANNAH RIVER AT FORT PULASKI, GA | 164,000cfs |
LOWER ATCHAFALAYA RIVER AT MORGAN CITY, LA | 160,000cfs |
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.