During the evening of Sunday, March 14th, a very large storm system began to move out into the plains with a broad circulation across most of the Northern Plains/Upper Midwest. The surface low was centered across Kansas with several weaker shortwaves moving around the broad circulation through Monday night, March 15th. Initially, very dry air below 15,000 feet was noted from Sunday evening and Monday morning soundings at the Chanhassen NWS. This kept most of the precipitation from reaching the ground until the atmosphere started to saturate from the continuous feed of mid-level moisture.
Surface observations at Fairmont, Minnesota reported light precipitation around 1 AM CST. This area of precipitation slowly spread northward during the morning, reaching Redwood Falls, New Ulm, Mankato, and Waseca around 330 AM CST. The precipitation didn't reach the southwest metro area until 9-10 AM CST as the dry easterly flow continued.
As the system began to pivot and the deeper moisture moved northward, the precipitation ended in portions of southwest Minnesota. However, one continuous feed of mid-level moisture across southeast Minnesota, and into south-central Minnesota kept a steady area of moderate to heavy snowfall. This area of heavier precipitation was able to move as far north as the southern Twin Cities metro area during the mid-late afternoon. However, most of the forcing with this system was weakening and the precipitation started to end. By the early evening, the steadier snowfall had ended with some lingering light snow across east-central and central Minnesota.
The heavier snowfall occurred in a 25-50 mile band from New Ulm, southeast and east toward Mankato, Waseca, and Owatonna. The heaviest was reported around Mankato where there were a couple of reports of 10 to 11 inches in a 12 hour period. Another 10 to 11 inch report was near Nicollet, Minnesota.