The U-M Water Center addresses regional and national water resource challenges by engaging faculty and students at U-M. Science teams collaborate with natural resource managers and others to foster the co-production of science.
Larger-than-average summer ‘dead zone’ predicted for Chesapeake Bay
A U-M ecologist and colleges from several institutions forecasted a larger-than-average “dead zone” in Chesapeake Bay. Last summer’s Chesapeake Bay hypoxic or “dead zone,” an area of low to no oxygen that can kill fish and aquatic life, was expected to be approximately 1.89 cubic miles — nearly the volume of 3.2 million Olympic-size swimming pools.
Research Partners:
Department of Naval Architecture and Marine Engineering, Adventurers & Scientists for Conservation, the Great Canadian Shoreline Cleanup in Canada and the Alliance for the Great Lakes' Adopt-a-Beach program in the United StatesProtecting the Great Lakes
Protecting the Great Lakes
A five-year, $20 million grant from the federal government will support research focused on sustainable management of the Great Lakes. The Cooperative Institute for Great Lakes Research will focus on four themes in line with research areas at NOAA’s Ann Arbor lab: observing systems and advanced technology, invasive species and food-web ecology, hydrometeorological and ecosystem forecasting, and protection and restoration of resources.
Funded by the National Oceanic and Atmospheric Administration, the institute represents a partnership between nine universities across the Great Lakes region, as well as multiple nongovernmental organizations and private businesses.
Research Partners:
Central Michigan University, Cornell University, Grand Valley State University, University of Michigan, Michigan State University, University of Minnesota-Duluth, Ohio State University, University of Windsor, University of Wisconsin-MilwaukeeRising sea levels
New findings from U-M explain an Ice Age paradox and add to the mounting evidence that climate change could bring higher seas than most models predict. The study shows how small spikes in the temperature of the ocean, rather than the air, likely drove the rapid disintegration cycles of the expansive ice sheet that once covered much of North America. Jeremy Bassis, U-M associate professor of climate and space sciences and engineering, developed a model to mathematically describe how ice breaks and flows which has led to a deeper understanding of how the Earth’s store of ice could react to changes in air or ocean temperatures, and how that might translate to sea level rise.
