ALL RIVERS AND STREAMS ARE UNDER NORMAL WINTER CONDITIONS WITH NO
RIVER OR STREAM IN THE BASIN CURRENTLY ABOVE FLOOD STAGE.
HOWEVER...NEARLY ALL RIVER GAGES ARE RECORDING STAGES THAT ARE AT
THE UPPER END OF THE NORMAL RANGE FOR THIS TIME OF YEAR.
THE PROBABILITIES OF FLOODING CONTAINED IN THIS HYDROLOGIC OUTLOOK
WERE DEVELOPED USING SNOWFALL AND SNOW WATER EQUIVALENT DATA CURRENT
THROUGH 16 FEBRUARY 2010. GIVEN THE SIGNIFICANTLY ABOVE NORMAL
SNOWPACK ACROSS MOST OF THE STATE...THE RISKS FOR FLOODING ARE ALSO
WELL ABOVE NORMAL AS WE APPROACH THE SPRING MELT SEASON. EVEN MORE
APPARENT TO THOSE WHO FOLLOW THESE PROBABILITY CHARTS...MOST
LOCATIONS HAVE SEEN THE RISK OF FLOODING INCREASE SINCE THE LAST
ISSUANCE OF THIS DATA. RECENT UPDATES TO THE WATER EQUIVALENT DATA IN
MANY BASINS FROM FIELD SAMPLING CONTINUES TO PROVIDE A CLEARER
UNDERSTANDING OF WATER ON THE GROUND.
THE SOURIS BASIN HAS BEEN SPARED SIGNIFICANT RAIN SO FAR THIS WINTER
BUT HEAVY SNOWFALL HAS RESULTED IN A SNOWPACK THAT IS IN MANY WAYS
COMPARABLE TO THAT OF LAST YEAR AT THIS TIME...ESPECIALLY IN THE
IMMEDIATE MINOT AREA. THE AREAS NORTH AND WEST OF MINOT HOLD
LESS SNOW AND WATER EQUIVALENT OVERALL AND CONTINUES TO DECREASE
UPSTREAM OF LAKE DARLING. PARTLY BECAUSE OF THE AMOUNT OF WATER IN
THE SNOW...AND LOCATION OF THE HIGHEST WATER CONTENT...PROBABILITIES
FOR REACHING AT LEAST MINOR FLOODING ARE HIGHEST FOR THE SOURIS RIVER
AT FOXHOLM AND AREAS DOWNSTREAM OF MINOT. SOME DOWNSTREAM AREAS
CURRENTLY HAVE A GREATER THAN 90 PERCENT CHANCE OF MINOR FLOODING
WITH TOWNER AND BANTRY HAVING A 96 PERCENT CHANCE OF MODERATE
FLOODING. THE WILLOW CREEK AND WINTERING RIVER SITES OF WILLOW CITY
AND KARLSRUHE ALSO HAVE A GREATER THAN 98 PERCENT PROBABILITY OF
MINOR FLOODING.
ANOTHER PROBLEM...ESPECIALLY AROUND THE MINOT AREA...ARE THE SMALLER
UNGAGED STREAMS AND OVERLAND FLOODING. GIVEN A QUICK MELT OR ANY
PRECIPITATION DURING THE MELT...TOWNSHIP AND COUNTY ROADS ARE LIKELY
TO BE FLOODED AND CREATE TRAVEL DIFFICULTIES IN RURAL AREAS.
ONE SHOULD NOTE THOUGH THAT WHILE THE SOURIS RIVER BASIN AS A WHOLE
CURRENTLY HAS A SNOWPACK CAPABLE OF GENERATING FLOODING...THERE ARE
OTHER FACTORS WHICH WILL WEIGH HEAVILY IN SPRING FLOODING. THE
AMOUNT OF MOISTURE ACCUMULATED BETWEEN NOW AND THE MELT ALONG WITH
EXACT WEATHER CONDITIONS DURING THE SPRING MELT ARE UNPREDICTABLE
AND WILL LARGELY CONTROL THE LOCATION AND SEVERITY OF FLOODING.
IMPORTANTLY...THE PROBABILITIES FOR FLOODING IN THIS HYDROLOGIC
OUTLOOK DO NOT INCLUDE RISK ASSOCIATED WITH ICE JAM RELATED
FLOODING. TIMING AND SEVERITY OF ICE JAMS DEFY STATISTICAL
FORECASTING METHODS ALTHOUGH ICE JAMS DO TEND TO FORM IN
HISTORICALLY KNOWN LOCATIONS TYPICALLY ASSOCIATED WITH BRIDGES...
MEANDERS IN CHANNEL...OR OTHER FEATURES THAT IMPEDE FLOW.