Quantifying the influence of cold water intrusions in a shallow, coastal system across contrasting years: Green Bay, Lake Michigan

2018 ◽  
Vol 44 (5) ◽  
pp. 851-863 ◽  
Author(s):  
Brice K. Grunert ◽  
Shelby L. Brunner ◽  
Sajad A. Hamidi ◽  
Hector R. Bravo ◽  
J. Val Klump
1995 ◽  
Vol 52 (5) ◽  
pp. 1074-1082 ◽  
Author(s):  
Lars G. Rudstam ◽  
Paul E. Peppard ◽  
Thomas W. Fratt ◽  
Richard E. Bruesewitz ◽  
Daniel W. Coble ◽  
...  

We estimated prey consumption by burbot (Lota lota) based on diet, mortality, growth, maturity, thermal history, population density and a bioenergetics model derived for a similar, cold-water gadoid, the Atlantic cod (Gadus morhua). In Green Bay, Lake Michigan, burbot >400 mm fed primarily on fish; smaller burbot probably fed mostly on invertebrates and sculpins (Cottus sp.). Our calculations indicate that burbot of age ≥1 consumed 16 kg/ha of prey (12.2 kg/ha of fish) in 1988 in the Wisconsin waters of Green Bay including 3.3, 2.1, 1.9, 1.2, and 0.8 kg/ha of rainbow smelt (Osmerus mordax), sculpins, alewife (Alosa pseudoharengus), yellow perch (Perca flavescens), and bloater (Coregnus hoyi), respectively. On an areal basis, piscivory by burbot in Green Bay was higher than the reported lake-wide average for consumption by all salmonids in Lake Michigan. Burbot consumed about 25% of the lake-wide salmonid consumption of alewife per unit area and close to the estimated combined commercial and sport harvest of yellow perch in the Bay the same year (271 vs. 325 tons). Thus, burbot should be included when considering the balance between predatory demand and forage fish production in Green Bay and probably also in other areas of Lake Michigan.


1993 ◽  
Vol 27 (1) ◽  
pp. 75-87 ◽  
Author(s):  
Diane R. Achman ◽  
Keri C. Hornbuckle ◽  
Steven J. Eisenreich

Author(s):  
Andrew L. Ransom ◽  
Christopher J. Houghton ◽  
S. Dale Hanson ◽  
Scott P. Hansen ◽  
Lydia R. Doerr ◽  
...  

Chemosphere ◽  
1993 ◽  
Vol 26 (11) ◽  
pp. 2079-2084 ◽  
Author(s):  
D.E. Tillitt ◽  
T.J. Kubiak ◽  
G.T. Ankley ◽  
J.P. Giesy

1999 ◽  
Vol 45 (150) ◽  
pp. 201-213 ◽  
Author(s):  
E.M. Shoemaker

AbstractThe effect of subglacial lakes upon ice-sheet topography and the velocity patterns of subglacial water-sheet floods is investigated. A subglacial lake in the combined Michigan–Green Bay basin, Great Lakes, North America, leads to: (1) an ice-sheet lobe in the lee of Lake Michigan; (2) a change in orientations of flood velocities across the site of a supraglacial trough aligned closely with Green Bay, in agreement with drumlin orientations; (3) low water velocities in the lee of Lake Michigan where drumlins are absent; and (4) drumlinization occurring in regions of predicted high water velocities. The extraordinary divergence of drumlin orientations near Lake Ontario is explained by the presence of subglacial lakes in the Ontario and Erie basins, along with ice-sheet displacements of up to 30 km in eastern Lake Ontario. The megagrooves on the islands in western Lake Erie are likely to be the product of the late stage of a water-sheet flood when outflow from eastern Lake Ontario was dammed by displaced ice and instead flowed westward along the Erie basin. The Finger Lakes of northern New York state, northeastern U.S.A., occur in a region of likely ice-sheet grounding where water sheets became channelized. Green Bay and Grand Traverse Bay are probably the products of erosion along paths of strongly convergent water-sheet flow.


2018 ◽  
Vol 6 (1) ◽  
pp. 8-13 ◽  
Author(s):  
Charles P. Madenjian ◽  
Sarah E. Janssen ◽  
Ryan F. Lepak ◽  
Jacob M. Ogorek ◽  
Tylor J. Rosera ◽  
...  

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