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Base flow, Floods, and Sediment Loads of Lake Superior Tributaries By Faith A. Fitzpatrick U.S. Geological Survey, WRD, Middleton, Wis.

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Presentation on theme: "Base flow, Floods, and Sediment Loads of Lake Superior Tributaries By Faith A. Fitzpatrick U.S. Geological Survey, WRD, Middleton, Wis."— Presentation transcript:

1 Base flow, Floods, and Sediment Loads of Lake Superior Tributaries By Faith A. Fitzpatrick U.S. Geological Survey, WRD, Middleton, Wis.

2 Base Flow, Floods, and Sediment Loads How do tributaries vary in these characteristics because of geology geomorphology, and land use? What implications do these natural and human-caused variations have for fisheries management and restoration?

3 Other Clay Loam Peat Sand/gravel Pigeon Washington Knife Montreal Trap Rock Ontonagon Fish St. Louis Deer Bois Brule Bad Whittlesey White Sturgeon Tahquamenon Au Train Nemadji

4 Base flow – geologic setting important

5 # # # ## # # # # # # # # # #.. tm. Baseflow, August 2002 (cubic feet per second) Whittlesey Creek Base flow complexities…….. 0-0.10 0.1-10 10-19

6 Contributing Area from Deep Flow System Whittlesey “watershed” North Fish Creek Whittlesey Creek Sioux River

7 Floods—geologic setting and land use

8 U.S. Suspended Sediment Contributions to Lake Superior Average Daily Loads (Robertson, 1996)

9 Post-settlement annual sediment budget (metric tons per year) North Fish Creek

10 Sediment—Importance of Bed Load and Yield Descriptions Suspended load Total load (kg/ha/yr) Bad River 1,030 no data Fish Creek 1,450 4,380 Suspended load Total load (dump trucks/day) (dump trucks/day) Bad River58176?? Fish Creek 2 5

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12 North Fish Creek—Floods 2 times and sediment loads 2.5 times pre-settlement rates

13 Estimated bankfull discharge, m 3 /s 15 1995 10 <1906 60 0 8 DISTANCE FROM MOUTH (KILOMETERS) ALTITUDE (METERS) 40 20 0 200 300 400 25 meters 1995 10 <1946 60 0 12 4 Brook trout originally found throughout entire stream Limited sustained brook trout in headwaters

14 Habitat Protection and Restoration: l Focus efforts on reducing watershed runoff and erosion-control in upper main stem l Use restoration techniques similar to those for urban streams–keep/restore pre- development storm hydrographs

15 Rehabilitation techniques geared toward reducing watershed runoff and bank erosion l Detention, infiltration basins in headwaters l Increase forest cover in watershed l Grade control structures in upper main stem l Bank protection in upper main stem l Large woody debris l Beaver l (Do nothing)

16 Acknowledgments This presentation contains results from cooperative studies among the Wisconsin Department of Natural Resources, University of Wisconsin-Madison, Bayfield County, U.S. Fish and Wildlife Service, and the U.S. Geological Survey Special thanks to Dennis Pratt (WDNR) and Dave Saad (USGS) for slide contribution


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