Pat Manley and Tom Manley (both Geology) have received funding as part of a statewide grant awarded to the VT-EPSCoR program at the University of Vermont (UVM) by the National Science Foundation. The goal of this five-year grant, titled Basin Resiliency to Extreme Events (BREE), is to study and promote resiliency in the Lake Champlain Basin. Pat and Tom will be working with UVM researchers and Middlebury students to study circulation and sediment dynamics of the Winooski River outflow in order to better understand the delivery and disposition of sediment, nutrients, and potential contaminants into Lake Champlain. Year 1 of this 5 year program will focus on the deployment of 10 year-long subsurface moorings, high resolution bottom mapping of the region, and the deployment of 4 subsurface neutrally-buoyant Lagrangian drifters that will map water movement throughout the Main Lake at various depths. In subsequent years, these operations will be repeated to produce a long-term data set that will concurrently be used to calibrate a 3-dimensional numerical model of lake circulation.
Pat Manley and Tom Manley receive funding for research on Lake Champlain
Pat Manley and Tom Manley (both Geology) have received funding as part of a statewide grant awarded to the VT-EPSCoR program at the University of Vermont (UVM) by the National Science Foundation. The goal of this five-year grant, titled Basin Resiliency to Extreme Events (BREE), is to study and promote resiliency in the Lake Champlain Basin. Pat and Tom will be working with UVM researchers and Middlebury students to study circulation and sediment dynamics of the Winooski River outflow in order to better understand the delivery and disposition of sediment, nutrients, and potential contaminants into Lake Champlain. Year 1 of this 5 year program will focus on the deployment of 10 year-long subsurface moorings, high resolution bottom mapping of the region, and the deployment of 4 subsurface neutrally-buoyant Lagrangian drifters that will map water movement throughout the Main Lake at various depths. In subsequent years, these operations will be repeated to produce a long-term data set that will concurrently be used to calibrate a 3-dimensional numerical model of lake circulation.