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Last modified
1/25/2010 6:46:43 PM
Creation date
10/5/2006 12:45:55 AM
Metadata
Fields
Template:
Floodplain Documents
County
Statewide
Basin
Statewide
Title
Overview of River-Floodplain Ecology in the Upper Mississippi River Basin
Date
12/9/1996
Prepared By
USGS
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br /> <br />52 <br /> <br />OVERVIEW OF RIVER-FLOODPLAIN ECOLOGY IN THE UPPER MISSISSIPPI RIVER BASIN <br /> <br /> <br />- _ Canada <br />-- <br />Unit;; Stat;;- - - <br /> <br /> <br />Fort Peck (Fort Peck Dam) (RK 2,651) <br /> <br />Sakakawea (Garrison Dam) (RK 2,237) <br /> <br />Oahe (Oahe Dam) (RK 1,725) <br /> <br />Sharpe (Big Bend Dam) IRK 1,566) <br /> <br />Francis Case (Fort Randall Dam) <br />IRK 1,416) <br /> <br />Yankton (RK 1,295) <br /> <br />Lewis and Clark (Gayins Point Dam) <br />RK 1,305) <br /> <br />Figure 5-3. Missouri River basin showing most of the civil works projects completed by the U.S. Army Corps of Engineers and <br />U.S. Bureau of Reclamation. RK, river kilometer (source: Hesse and others, 1989a). <br /> <br />Figure 5-4. Mean (solid line), maximum (doned line), and <br />minimum (dashed line) stages of the preregulated (upper panel) <br />and postregulated (lower panel) Missouri River at Omaha, <br />Nebraska (river kilometer 1107). Preregulated stages are based <br />on averages of daily stage recordings between 1880 and 1899, <br />and postregulated stages are based on averages between 1966 <br />and 1985 (modified from Hesse and Me"'. 1993). <br /> <br />Rocky Mountains, to about 45 centimeters in the Great <br />Plains, and more than 90 centimeters in the interior high- <br />lands (Hesse and olhers, 1989a). <br />Annual Missouri River discharge to the Mississippi <br />River is about 7.0 x 1010 cubic meters. 1\\10 seasonal peri- <br />ods of flooding occurred prior to impoundmenl (fig, 5-4). <br />The first, or March rise, was caused by snowmelt in the <br />Greal Plains and breakup of ice in the main channel and <br />tributaries. The second, or June rise, was produced by run- <br />off from snowmelt in Ihe Rocky Mounlains and rainfall <br />throughout the basin, <br />In presettlement times the Missouri River was one of <br />the most turbid river systems in North America. earning it <br />the nickname Big Muddy. The magnitude of the Missouri <br />River's sediment load can besl be iIluslrated by its influence <br />on the Mississippi River. Average turbidity of Ihe Missis- <br /> <br />600 <br />500 <br />400 <br /> <br />300 <br />~ <br />.!l <br />~ <br />.5 <br />c <br />~ <br />.!!- <br /><= <br />o <br />~ <br />iii <br /> <br />200 <br /> <br /> <br />100 <br /> <br />-.' ~ ~ - ~- <br /> <br />" <br /> <br />'"....' <br /> <br />.. ~".. - -, -.. <br /> <br />" <br /> <br />600' <br /> <br />500 <br /> <br />400 <br /> <br />300 <br /> <br />200 <br /> <br />100 <br />o <br /> <br />':": <br /> <br /> <br />~ ... #..' ..'" -,...,.., -,.,..... -... - - , '. <br />, <br /> <br />, ,...-1 <br />.If,." ... <br /> <br />, <br />, " <br />,,' <br /> <br />o <br /> <br />60 <br /> <br />120 180 240 <br />Julian date <br /> <br />300 <br /> <br />360 <br /> <br />sippi River upstream of the preimpounded Missouri River <br />was reponed by Platner (I946) as 300 pans per million, <br />whereas below the mouth of the Missouri River the average <br />increased to 1,800 pans per million. <br />
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