694  
FGUS73 KBIS 261847  
ESFBIS  
NDC001-007-011-015-021-025-029-031-033-037-041-043-045-047-051-053-  
055-057-059-061-065-083-085-087-089-093-103-105-270300-  
 
PROBABILISTIC HYDROLOGIC OUTLOOK  
NATIONAL WEATHER SERVICE BISMARCK ND  
1247 PM CST THU FEB 26 2026  
   
..SPRING FLOOD AND WATER RESOURCES OUTLOOK
 
 
 
THIS SPRING FLOOD AND WATER RESOURCES OUTLOOK IS FOR THE MISSOURI  
AND JAMES RIVER BASINS OF NORTH DAKOTA, COVERING THE PERIOD OF 01  
MARCH THROUGH 30 MAY, 2026. THIS OUTLOOK IS THE SECOND OF THREE IN  
A SERIES OF OUTLOOKS THAT THE NATIONAL WEATHER SERVICE COLLECTIVELY  
REFERS TO AS THE SPRING FLOOD AND WATER RESOURCES OUTLOOKS. THIS  
WILL BE FOLLOWED BY THE FINAL SPRING FLOOD AND WATER RESOURCES  
OUTLOOK TO BE ISSUED ON 12 MARCH, 2026. ON MARCH 26TH, THE NATIONAL  
WEATHER SERVICE WILL REVERT BACK TO ITS NORMAL ISSUANCE OF THE  
90-DAY PROBABILISTIC OUTLOOKS, USUALLY ON, OR ABOUT THE 4TH THURSDAY  
OF EVERY MONTH.  
 
THE FOLLOWING MESSAGE HAS FOUR SECTIONS. THE FIRST PROVIDES SOME  
TEXT ON THE HIGHLIGHTS OF THIS OUTLOOK AND CONDITIONS AFFECTING THE  
LOCAL HYDROLOGY. THE SECOND SECTION GIVES THE CURRENT AND HISTORICAL  
RISKS OF FLOODING AS DETERMINED BY THE ENSEMBLE STREAMFLOW FORECAST  
MODEL OF THE NATIONAL WEATHER SERVICE. THE THIRD SECTION GIVES THE  
CURRENT PROBABILITIES FOR REACHING FLOOD STAGE AT THE LISTED  
FORECAST LOCATIONS. AND FINALLY, THE FOURTH SECTION COVERS THE RISK  
OF THE RIVER SITES FALLING BELOW THE LISTED STAGES.  
   
..FLOOD OUTLOOK HIGHLIGHTS
 
 
IN GENERAL, THE MODELS DO NOT CURRENTLY REFLECT MUCH RISK OF  
WIDESPREAD FLOODING ACROSS THE JAMES AND MISSOURI RIVER BASIN  
FORECAST LOCATIONS. THIS IS LARGELY DUE TO THE LOSS OF MOST OF THE  
SNOW RECEIVED EARLY THIS WINTER DURING LENGTHY WARM PERIODS OF TIME  
WHERE THE SNOW MELTED AND EITHER RAN OFF INTO THE LOCAL STREAMS, OR  
INFILTRATED INTO THE GROUND SURFACE. THE DOWNSIDE TO THIS EARLY LOSS  
OF THE SNOWPACK WAS THAT THE GROUND IS NOW NEARLY IMPERMEABLE TO  
FURTHER INFILTRATION OF RAINFALL AND RUNOFF GENERATED BY MELTING  
SNOW.  
 
THIS NEARLY IMPERMEABLE SURFACE OF THE GROUND IS WHAT CREATES THE  
CURRENT FLOOD RISK. GIVEN THE TIME OF YEAR, IT IS HIGHLY LIKELY THAT  
THE AREA WILL AGAIN RECEIVE MORE SNOW, EVEN THOUGH IT WOULD BE  
UNLIKELY TO ENTER THE SPRING MELT SEASON WITH AN EXCEPTIONAL  
SNOWPACK. HOWEVER, THE REGION IS ALSO NOW ENTERING THE TIME OF YEAR  
WHERE AN EARLY SPRING RAIN COULD FALL ON THIS NEAR IMPERMEABLE  
SURFACE AND CREATE A SURPRISING AMOUNT OF RUNOFF. SO, WHILE THE  
SNOWPACK IS CURRENTLY INSUFFICIENT TO GENERATE MUCH CONCERN...THERE  
REMAINS A DISTINCTLY NON-ZERO RISK OF FLOODING, ESPECIALLY IF THE  
REGION WERE TO EXPERIENCE A WARM COLORADO LOW BRINGING HEAVY SPRING  
RAINS BEFORE THE SOILS THAW AND BECOME AVAILABLE TO INFILTRATION OF  
MELTWATER AND RAINFALL.  
 
UNTIL SUCH TIME AS THE GROUND SURFACE THAWS, ANY SPRING RAIN OR  
MELTING OF FUTURE SNOW WILL CREATE A SURPRISINGLY GENEROUS AMOUNT OF  
RUNOFF FROM A GIVEN AMOUNT OF RAIN OR SWE CONTENT ON THE GROUND.  
 
LASTLY, WARM WEATHER DURING THE FIRST WEEK OF MARCH WILL FURTHER  
MELT AND ERODE THE SNOWPACK ACROSS THE MISSOURI AND JAMES RIVER  
BASINS. HOWEVER, THE EXTENT OF THIS MELT AND HOW MUCH RUNOFF WILL BE  
GENERATED FROM THIS WARM SPELL IS JUST A LITTLE TOO FAR IN THE  
FUTURE FOR MUCH CERTAINTY.  
   
..SNOWPACK CONDITIONS
 
 
WHILE THE SNOW ACCUMULATION SEASON HAD A ROBUST BEGINNING IN EARLY  
DECEMBER, MOST OF THE MISSOURI AND JAMES RIVER BASINS HAVE SINCE  
LOST MUCH OF THEIR SNOWPACK TO MELTING AND SUBLIMATION. MUCH, BUT  
NOT ALL, OF THIS MELTWATER RAN INTO THE LOCAL STREAMS AND IS NOW  
DRAINED OFF THE COUNTRYSIDE.  
 
WHAT REMAINS NOW ACROSS MOST OF THE JAMES AND MISSOURI RIVER BASINS  
IS SWE IN THE FORM OF ICE ON THE GROUND SURFACE, OR A RECENTLY  
RECEIVED MODEST SNOWPACK. IN THE SOUTHWESTERN CORNER OF THE STATE,  
SWE CONTENT IS NOW WELL BELOW ONE-HALF OF AN INCH, AND BUILDS  
SLIGHTLY TO AROUND TWO INCHES OF SWE IN THE UPPER JAMES RIVER BASIN.  
IN AND OF ITSELF, THE EXISTING SNOWPACK DOES NOT CREATE MUCH  
CONCERN, BUT UP TO SEVERAL WEEKS REMAIN IN THE SNOW ACCUMULATION  
SEASON. NONETHELESS, IT REMAINS TO BE SEEN HOW MUCH TOTAL SWE WILL  
BE ON THE GROUND FOR THE EVENTUAL SPRING MELT SEASON. SWE TOTALS  
NEARING THREE ACROSS LARGE AREAS WOULD BE CAUSE FOR CONCERN THIS  
YEAR GIVEN THE DEMONSTRATED IMPERMEABLE NATURE OF THE SURFACE SOILS.  
   
..THE MISSOURI AND YELLOWSTONE RIVERS WEST OF WILLISTON
 
 
THE MISSOURI AND YELLOWSTONE RIVERS WEST OF WILLISTON ARE SLIGHTLY  
ELEVATED FOR THIS TIME OF YEAR AS RUNOFF FROM THE EARLY FEBRUARY  
MELT CONTINUES MAKING ITS WAY TOWARDS LAKE SAKAKAWEA. WHILE FLOODING  
IS NOT A LARGE CONCERN AT THIS POINT, UNSTABLE ICE ALONG THE  
FREE-FLOWING PORTIONS OF THE YELLOWSTONE AND MISSOURI RIVERS WEST OF  
WILLISTON IS A DANGER TO OUTDOOR ENTHUSIASTS RECREATING ON AND ALONG  
THE RIVERS.  
   
..THE MISSOURI RIVER BELOW GARRISON DAM
 
 
THE MISSOURI RIVER BELOW GARRISON DAM IS LARGELY OPEN DOWN THROUGH  
THE WASHBURN AREA. FROM WILTON TO THE BISMARCK/MANDAN AREA, THERE  
ARE A FEW SPOTS SHOWING OPEN WATER BUT IT GENERALLY REMAINS COVERED  
IN ICE. THIS SUGGESTS THAT EVEN WITH SEASONABLE TEMPERATURES, ENOUGH  
ICE REMAINS ON THE MISSOURI RIVER TO PRODUCE ICE JAM(S) IF THE  
REGION WERE TO EXPERIENCE A SUDDEN LARGE RUNOFF EVENT. FOR EXAMPLE,  
A WARM COLORADO LOW STORM SYSTEM BRINGING EXCESSIVE RAINFALL TO THE  
AREA BEFORE THE SOILS THAW SUFFICIENTLY TO RESTORE THE SOIL'S  
ABILITY TO MINIMIZE RUNOFF, WOULD BE SUCH AN EVENT.  
   
..CURRENT DROUGHT CONDITIONS
 
 
THERE ARE NO CURRENT DROUGHT DESIGNATIONS IN THE MISSOURI AND JAMES  
RIVER BASINS OF NORTH DAKOTA.  
   
..RESERVOIRS AND NATURAL WETLANDS
 
 
NATURAL WETLANDS AND ARTIFICIAL RESERVOIRS ARE GENERALLY WITHIN THE  
LONG-TERM NORMAL RANGE FOR THIS TIME OF THE YEAR. FLOOD CONTROL  
FEATURES ARE ALREADY AT, OR BELOW THEIR NORMAL DRAW-DOWN LEVELS IN  
PREPARATION FOR THE EVENTUAL SPRING MELT SEASON. THIS SUGGESTS THAT  
LOCAL WATER STORAGE WILL PROVIDE A NORMAL AMOUNT OF FLOOD MITIGATION  
COME THE SPRING MELT SEASON. MANY SMALLER WATER STORAGE FEATURES,  
SUCH AS STOCK DAMS AND DUGOUTS HAVE ALREADY EXPERIENCED CONSIDERABLE  
RISES DUE TO THE FEBRUARY MELTING OFF OF THE LOCAL SNOWPACK.  
   
..SOIL CONDITIONS
 
 
SOIL TEMPERATURES ARE HIGHLY VARIED THIS YEAR. IN PLACES WHERE THE  
SNOW LARGELY MELTED OFF DURING THE MULTIPLE WARM PERIODS IN LATE  
DECEMBER, EARLY JANUARY AND AGAIN IN EARLY FEBRUARY ARE NOW POORLY  
INSULATED AND THIS HELPS INCREASE FROST DEPTH. BELOW FREEZING  
TEMPERATURES CAN GO DOWN TO AROUND 30 INCHES IN SOME AREAS, WITH  
ABOUT 24 INCHES BEING NORMAL. THESE SOIL TEMPERATURES ARE GENERALLY  
NEAR NORMAL FOR THIS TIME OF YEAR. WHAT IS QUITE A BIT MORE UNUSUAL  
IS THE SOIL MOISTURE PROFILE ACROSS THE MISSOURI AND JAMES RIVER  
BASINS. SINCE THE EARLY SNOW FELL ON WARM SOILS AND SUBSEQUENTLY  
EXPERIENCED A LOT OF MELTING, THE GROUND SURFACE AND NEAR SURFACE  
SOILS BECAME VERY WET. A SECOND WARM PERIOD IN EARLY FEBRUARY  
CREATED A SURPRISINGLY GENEROUS RUNOFF FROM THAT MELTING SNOW AND  
ICE DUE TO THE NEAR IMPERMEABLE GROUND SURFACE.  
   
..WEATHER OUTLOOK
 
 
THE NEAR-TERM 6-10 AND 8-14 DAY WEATHER OUTLOOKS FAVOR ABOVE NORMAL  
TEMPERATURES AND ABOVE NORMAL PRECIPITATION. THE ONE-MONTH OUTLOOKS  
FOR THE MONTH OF MARCH PUTS ALL OF THE JAMES AND MISSOURI RIVER  
BASINS IN THE EQUAL CHANCES CATEGORY FOR BELOW NORMAL, NEAR NORMAL,  
OR ABOVE NORMAL TEMPERATURE AND PRECIPITATION.  
 
LOOKING EVEN LONGER TERM, THE 3-MONTH OUTLOOKS COVERING MARCH,  
APRIL, AND MAY ALSO PLACE THIS AREA IN THE EQUAL CHANCES CATEGORY  
FOR TEMPERATURE AND PRECIPITATION.  
 
IN TABLE 1 BELOW, THE CURRENT (CS) AND HISTORICAL (HS) OR NORMAL  
PROBABILITIES OF EXCEEDING MINOR...MODERATE...AND MAJOR FLOOD STAGE  
ARE LISTED FOR THE VALID TIME PERIOD.  
 
CS VALUES INDICATE THE PROBABILITY OF REACHING A FLOOD CATEGORY  
BASED ON CURRENT CONDITIONS.  
 
HS VALUES INDICATE THE PROBABILITY OF REACHING A FLOOD CATEGORY  
BASED ON HISTORICAL OR NORMAL CONDITIONS.  
 
WHEN THE VALUE OF CS IS GREATER THAN HS...THE PROBABILITY OF  
EXCEEDING THAT LEVEL IS HIGHER THAN NORMAL. WHEN THE VALUE OF CS IS  
LESS THAN HS...THE PROBABILITY OF EXCEEDING THAT LEVEL IS LOWER  
THAN NORMAL.  
   
..TABLE 1--PROBABILITIES FOR MINOR...MODERATE AND MAJOR FLOODING
 
 
VALID PERIOD: 03/01/2026 - 05/30/2026  
 
: CURRENT AND HISTORICAL  
: CHANCES OF EXCEEDING  
: FLOOD CATEGORIES  
: AS A PERCENTAGE (%)  
CATEGORICAL :  
FLOOD STAGES (FT) : MINOR MODERATE MAJOR  
LOCATION MINOR MOD MAJOR : CS HS CS HS CS HS  
-------- ----- ----- ----- : --- --- --- --- --- ---  
:PIPESTEM  
PINGREE 11.0 13.0 15.0 : <5 12 <5 <5 <5 <5  
:JAMES RIVER  
GRACE CITY 12.0 14.0 15.0 : 6 16 5 13 <5 9  
LAMOURE 14.0 16.0 18.0 : <5 17 <5 8 <5 <5  
:MISSOURI RIVER  
WILLISTON 22.0 24.0 26.0 : <5 27 <5 10 <5 8  
:CANNONBALL RIVER  
REGENT 22.0 24.0 26.0 : <5 <5 <5 <5 <5 <5  
:CEDAR CREEK  
RALEIGH 12.0 14.0 16.0 : <5 9 <5 5 <5 <5  
:CANNONBALL RIVER  
BREIEN 10.0 20.0 23.0 : 12 58 <5 <5 <5 <5  
:BEAVER CREEK  
LINTON 12.0 14.0 16.0 : 19 41 <5 31 <5 13  
:LITTLE MUDDY RIVER  
WILLISTON 10.0 12.0 14.0 : 10 66 <5 33 <5 10  
:LITTLE MISSOURI RIVER  
MARMARTH 18.0 23.0 30.0 : <5 6 <5 <5 <5 <5  
MEDORA 15.0 18.0 20.0 : 6 18 5 9 <5 6  
WATFORD CITY 20.0 24.0 30.0 : 5 14 <5 5 <5 <5  
:KNIFE RIVER  
MANNING 15.0 17.0 20.0 : <5 20 <5 <5 <5 <5  
:SPRING CREEK  
ZAP 14.0 18.0 20.0 : 6 25 <5 14 <5 8  
:KNIFE RIVER  
HAZEN 21.0 24.0 25.0 : 8 43 7 25 <5 23  
:HEART RIVER  
MANDAN 27.0 33.0 38.0 : <5 20 <5 <5 <5 <5  
:APPLE CREEK  
MENOKEN 15.0 16.0 17.0 : 37 55 20 52 <5 34  
 
LEGEND  
CS = CONDITIONAL SIMULATION (CURRENT OUTLOOK)  
HS = HISTORICAL SIMULATION  
FT = FEET  
 
IN TABLE 2 BELOW...THE 95 THROUGH 5 PERCENT COLUMNS INDICATE THE  
PROBABILITY OF EXCEEDING THE LISTED STAGE LEVELS (FT) FOR THE VALID  
TIME PERIOD.  
   
..TABLE 2--EXCEEDANCE PROBABILITIES
 
 
CHANCE OF EXCEEDING STAGES  
AT SPECIFIC LOCATIONS  
VALID PERIOD: 03/01/2026 - 05/30/2026  
LOCATION 95% 90% 75% 50% 25% 10% 5%  
-------- ------ ------ ------ ------ ------ ------ ------  
:PIPESTEM  
PINGREE 5.2 5.2 5.3 5.6 6.2 9.1 10.5  
:JAMES RIVER  
GRACE CITY 5.5 5.5 5.7 6.1 6.9 11.1 13.5  
LAMOURE 7.8 7.8 7.9 8.4 10.8 13.1 13.8  
:MISSOURI RIVER  
WILLISTON 16.1 16.3 16.9 17.4 18.4 19.2 21.2  
:CANNONBALL RIVER  
REGENT 5.2 5.3 6.1 6.7 7.5 8.7 9.4  
:CEDAR CREEK  
RALEIGH 2.2 2.7 3.1 4.4 5.5 6.4 6.6  
:CANNONBALL RIVER  
BREIEN 3.4 3.8 4.7 6.7 8.4 10.6 11.3  
:BEAVER CREEK  
LINTON 5.8 5.9 6.6 8.8 11.3 12.8 13.0  
:LITTLE MUDDY RIVER  
WILLISTON 5.2 5.2 5.7 6.9 8.8 10.0 11.6  
:LITTLE MISSOURI RIVER  
MARMARTH 1.4 1.4 2.8 4.7 6.2 12.0 16.5  
MEDORA 3.7 3.7 4.5 5.6 8.0 13.2 17.1  
WATFORD CITY 8.4 8.5 10.4 11.5 13.6 16.7 20.2  
:KNIFE RIVER  
MANNING 6.2 6.2 7.1 8.1 9.1 10.5 12.8  
:SPRING CREEK  
ZAP 5.2 5.7 7.0 7.7 9.6 11.9 14.8  
:KNIFE RIVER  
HAZEN 1.2 2.0 6.0 9.1 13.6 17.3 24.8  
:HEART RIVER  
MANDAN 12.2 12.3 14.1 15.5 18.4 20.4 24.2  
:APPLE CREEK  
MENOKEN 5.7 5.9 9.1 13.1 15.7 16.7 17.0  
 
IN TABLE 3 BELOW...THE 95 THROUGH 5 PERCENT COLUMNS INDICATE THE  
PROBABILITY OF FALLING BELOW THE LISTED STAGE LEVELS (FT) FOR  
THE VALID TIME PERIOD.  
   
..TABLE 3--NONEXCEEDANCE PROBABILITIES
 
 
CHANCE OF FALLING BELOW STAGES  
AT SPECIFIC LOCATIONS  
VALID PERIOD: 03/01/2026 - 05/30/2026  
LOCATION 95% 90% 75% 50% 25% 10% 5%  
-------- ------ ------ ------ ------ ------ ------ ------  
:PIPESTEM  
PINGREE 5.0 5.0 4.9 4.8 4.8 4.8 4.8  
:JAMES RIVER  
GRACE CITY 4.0 4.0 4.0 4.0 4.0 4.0 4.0  
LAMOURE 7.6 7.6 7.5 7.1 6.9 6.8 6.8  
:MISSOURI RIVER  
:CANNONBALL RIVER  
REGENT 4.9 4.9 4.8 4.8 4.8 4.8 4.8  
:CEDAR CREEK  
RALEIGH 0.8 0.8 0.7 0.6 0.5 0.4 0.4  
:CANNONBALL RIVER  
BREIEN 2.1 2.1 2.0 1.9 1.8 1.7 1.7  
:BEAVER CREEK  
LINTON 4.7 4.7 4.5 4.5 4.4 4.4 4.4  
:LITTLE MUDDY RIVER  
WILLISTON 4.7 4.6 4.5 4.5 4.5 4.5 4.5  
:LITTLE MISSOURI RIVER  
MARMARTH 1.4 1.3 1.3 1.3 1.3 1.3 1.3  
MEDORA 2.5 2.4 2.4 2.4 2.3 2.3 2.3  
WATFORD CITY 8.2 8.2 8.2 8.2 8.1 8.1 8.1  
:KNIFE RIVER  
MANNING 6.2 6.2 6.1 6.1 6.0 6.0 6.0  
:SPRING CREEK  
ZAP 4.8 4.8 4.7 4.7 4.7 4.7 4.7  
:KNIFE RIVER  
HAZEN 0.7 0.7 0.6 0.5 0.5 0.3 0.3  
:HEART RIVER  
MANDAN 10.7 10.6 10.6 10.5 10.4 10.3 10.3  
:APPLE CREEK  
MENOKEN 4.8 4.8 4.7 4.1 3.9 3.5 3.5  
 
THESE LONG-RANGE PROBABILISTIC OUTLOOKS CONTAIN FORECAST VALUES THAT  
ARE CALCULATED USING MULTIPLE SEASON SCENARIOS FROM 30 OR MORE YEARS  
OF CLIMATOLOGICAL DATA...INCLUDING CURRENT CONDITIONS OF THE  
RIVER...SOIL MOISTURE...SNOW COVER AND 30 TO 90 DAY LONG-RANGE  
OUTLOOKS OF TEMPERATURE AND PRECIPITATION. BY PROVIDING A RANGE  
OF PROBABILITIES...THE LEVEL OF RISK ASSOCIATED WITH LONG-RANGE  
PLANNING DECISIONS CAN BE DETERMINED. THESE PROBABILISTIC  
FORECASTS ARE PART OF THE NATIONAL WEATHER SERVICE'S ADVANCED  
HYDROLOGIC PREDICTION SERVICE.  
 
VISIT OUR WEB SITE WEATHER.GOV/BIS FOR MORE WEATHER AND WATER  
INFORMATION.  
 
THE NEXT OUTLOOK WILL BE ISSUED BY 12 MARCH.  
 

 
 
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