Article posted by Canada Sentinel Photo by Steven J. Myers
At no other point in recorded history have water levels risen as much on Lake Superior and Michigan-Huron over the same two-year period. Since September 2014, all of the Great Lakes have been above their seasonal averages for the first time since the late 1990s.
“The recent surge in water levels brings to an end a 15-year period of persistent below-average water levels on Lakes Superior and Michigan-Huron,” said Drew Gronewold, a research hydrologist with NOAA’s Great Lakes Environmental Research Laboratory. “However, it is uncertain if, years from now, water levels will continue to rise, or if they will fall again to below-average levels.”
Docks were high and dry
Low water levels
were the story on Lake Michigan and across the Great Lakes in early
2013, as pictured here in Grand Traverse Bay, Michigan. (Michigan Sea
Grant)
The current surge in water levels has largely provided relief to communities, businesses and industries that depend on the Great Lakes, including commercial shipping, hydropower, recreational boating and tourism. However, high water levels can have negative effects as well, including coastal erosion, flooding, and property damage along the shoreline. The severe storm in October 2014 that lashed the shores of southern Lake Michigan is just one example.
Research from NOAA, the Army Corps, Environment Canada, and regional academic institutions indicates that increases in seasonal precipitation are the major cause of the recent water level surge. Measurements from a growing network of off-shore evaporation monitoring stations indicate that evaporation rates in the recent two-year period have not been particularly low despite recent cold winter temperatures and record high ice cover. So while high evaporation rates were a major factor in keeping water levels low between 1998 and 2013, an increase in precipitation appears to be the major driver of the recent water level surge.
Data suggests that precipitation in the Lake Superior and Lake Michigan-Huron basins was about 10 percent above long-term averages in both 2013 and 2014, while precipitation in 2012 (a year of drought that preceded the record low water levels on Michigan-Huron) was roughly 10 percent below the long-term average.
NOAA and Army Corps scientists are also studying how a changing climate may contribute to water level changes. To improve the understanding of the relationship between climate change and Great Lakes water levels, GLERL researchers and their academic partners analyze relationships between evaporation from the lakes, seasonal ice cover, and long-term heat storage in the lakes.
This research would not be possible without the continuous operational water level and meteorological monitoring networks provided by U.S. and Canadian federal agencies, as well as the research-oriented monitoring stations of partner academic institutions. The water level stations maintained by the NOAA/National Ocean Service Center for Operational Oceanographic Products and Services (CO-OPS), for example, provide one of the longest high quality hydrometeorological data sets in North America, with data beginning in 1860. Research and monitoring of Great Lakes water levels and regional meteorological conditions is an important part of NOAA’s mission to understand and predict changes in climate, weather, oceans, and coasts.
