This month’s long-range outlooks cover the time period from
January 27th through April 30th, 2009. Remember that these outlooks
are for planning purposes and give the probability of the river
exceeding various stages based on current conditions, and 50 years of
past precipitation and temperatures that occurred during the
period covered by this outlook.
Current snowpack conditions on the North Dakota side of the Red River
Basin: Snow depths of 20 to 30 inches exist in the headwaters of the
North Dakota Wild Rice River with water contents of 4 to 5 inches.
Portions of the Maple and lower Sheyenne River are covered with 15 to
20 inches of snow with 4 to 5 inches of water content. Elsewhere on
the North Dakota side of the Red River the Goose, Turtle, Park,
Forest and Pembina River Basins and northern Red River Valley have 8
to 15 inches of snow, with water contents of 2 to 4 inches.
On the Minnesota side of the Red River there are varied amounts of
snow depth. The Mustinka, Rabbit and lower Buffalo river basin have
16 to 20 inches of snow, with 3 to 4 inches of water content. The
Minnesota Wild Rice and Red Lake Basin have snow depths in the 12
to 16 inch range with water contents of 2 to 3 inches. The Minnesota
side of the northern Red River Valley also has 8 to 15 inches of
snow, with water contents of 2 to 4 inches.
Outlook for the rest of the winter and spring season: The development
of a La Nina in the equatorial Pacific will have an impact on the
late winter and spring snow-melt period. Historically, winter and
spring seasons with a La Nina are slightly cooler and wetter than
the long term average. At this time it is not possible to forecast
how much additional snow will accumulate through the start of the
melt cycle, but history suggests an additional 20 to 25 inches
of snow by the end of March. The outlooks already take into account
the threat of above normal precipitation, and these are represented
by the lower probabilities.
The conditions within the Red River Basin will change during the
spring, so subsequent outlooks will also change. As the hydrologic
picture develops; the outlooks will become more accurate and precise
as we get nearer to the spring flood. For factors influencing the
magnitude of flooding in the Red River Valley, see the Red River
flood factors link, or the link to the North Dakota Geological
Surveys flood factors article, both of which are available from the