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Page 10 A,1" L ~C Summer 1999 <br /> <br />State Climatology Office <br />DNR Waters <br />The winter of 1998-1999 followed an autumn of <br />mild temperatures and well-placed precipitation <br />patterns. Figure 1 shows above normal September <br />through November precipitation in northeastern <br />Minnesota. This region experienced a very dry growing <br />season, therefore, the additional precipitation brought <br />welcome relief. Conversely, much needed dry weather <br />benefitted southeastern Minnesota, an area where the <br />growing season had been quite damp. <br />Temperatures in the autumn continued ayear-long <br />trend of warmth. The statewide average temperature <br />was two to four degrees above normal in October and <br />November. Above normal temperatures in November <br />came even though a period of cold weather followed a <br />massive storm on November 10th. This storm brought <br />heavy snow, damaging winds and arecord-breaking <br />low pressure to many locations. The weather soon <br />modified and late November was extraordinarily warm. <br />The warmth continued into early December. <br />Minnesota was 15 to 20 degrees above normal for the <br />first two weeks of the month. Many locations broke all- <br />time high temperature records. The mild weather <br />permitted outdoor activity not typically seen during a <br />Minnesota December. Warm temperatures in November <br />and. early December resulted in a delay of lake freeze- <br />up across the state. <br />Historical records of <br />"ice-in" dates are <br />sketchy, however, it <br />appears that many lakes <br />experienced their latest <br />permanent "ice-in" date <br />of the century. Another <br />interesting hydrologic <br />impact of this balmy <br />weather was unusually <br />high December stream <br />flows in many rivers. <br />December precipitation <br />was very light, but the <br />mild temperatures <br />allowed. water in small <br />tributaries to contribute <br />flow to the larger sys- <br />tems. Typically these <br />smaller streams and <br />ditches are ice-bound in <br />early December. Arctic <br />air finally reached <br />Minnesota by mid- <br />December, dropping <br />temperatures below the <br />average. The landscape, <br />free of snow, was <br />exposed to the arctic <br />blast. This caused the <br />soil to freeze rapidly. <br />continued on page 11... <br />