Recent observations across the United States have indicated that a variety of rivers and streams are experiencing above-average streamflows, leading to concerns about potential flooding and the impacts on communities and ecosystems. The latest data from stream gauges reveal that the mighty Mississippi River is swelling considerably with its tributaries reporting high waters in states including Mississippi, Tennessee, Louisiana, and Illinois. Cities like Vicksburg, Memphis, Baton Rouge, and St. Louis should stay alert as weather forecasts predict more rain, which could exacerbate the situation. Meanwhile, the Atchafalaya River in Louisiana is also seeing significant flow increases, prompting close monitoring near Simmesport and Morgan City.
Watersheds such as Middle Tombigbee-Lubbub and Town in Alabama are flowing at over 600% of their normal levels, causing alarm among water management officials. Similarly, the Ohio Brush-Whiteoak watershed in Ohio is experiencing a dramatic surge in water levels, well beyond the normal range. Outdoors enthusiasts, particularly those interested in fishing and rafting, should be cautious and check local advisories as weather conditions continue to influence water levels.
Major cities along the affected rivers are on high alert for potential flooding, and water management agencies are working to mitigate any damage and ensure public safety. For the river outdoor enthusiast, these conditions may disrupt recreational activities but also present unique opportunities to witness the power of nature's waterways. As the situation evolves, so does the need for vigilant monitoring and proactive management to protect communities and preserve the integrity of these vital ecosystems.
Streamflow conditions across the USA vary significantly due to geographical and climatic factors. Historically, areas with high streamflows include the Pacific Northwest, parts of the Rocky Mountains, and the Upper Midwest, particularly during the spring months when snowmelt is at its peak. These regions experience abundant streamflow due to the melting of substantial snowpacks accumulated during winter. The Rocky Mountains, for instance, have numerous rivers fed by snowmelt, such as the Colorado and Yellowstone rivers, which see increased flow from late spring to early summer, crucial for agriculture, hydroelectric power generation, and replenishing groundwater levels.
Snowpacks play a crucial role in regulating streamflows across the US. In mountainous regions like the Sierra Nevada and the Cascades, snow accumulates during winter and gradually melts in spring and early summer, sustaining rivers like the Sacramento and Columbia. These rivers not only support ecosystems and agriculture but also provide vital water resources for cities and towns downstream. Streamflow levels directly impact recreational activities such as fishing and whitewater kayaking, as fish migration and water levels for rafting are closely tied to seasonal flow patterns. Balancing water usage with ecological and recreational needs remains critical in managing and sustaining healthy streamflow conditions nationwide.
Streamgauge | Discharge Change | Discharge |
---|---|---|
BLACK RIVER ABOVE MALAGA, NM | +6,455% | 1,960cfs |
RAYSE CREEK NEAR WALTONVILLE, IL | +3,093% | 1,060cfs |
MUSCATATUCK RIVER NEAR DEPUTY, IN | +2,762% | 2,590cfs |
HURRICANE CREEK NEAR MULBERRY GROVE, IL | +2,164% | 2,400cfs |
TOMBIGBEE RIVER AT ABERDEEN LOCK AND DAM, MS | +1,724% | 25,900cfs |
CAHOKIA CREEK AT EDWARDSVILLE, IL | +1,258% | 2,350cfs |
WHITEWATER RIVER NEAR ALPINE, IN | +1,059% | 3,790cfs |
SKUNA RIVER AT BRUCE, MS | +793% | 2,170cfs |
TOWN CREEK AT EASON BOULEVARD AT TUPELO, MS | +787% | 1,260cfs |
SHOAL CREEK AT IRON CITY, TN | +728% | 2,840cfs |
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 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 -0.39, signifying a La Nina 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.