several interior migration patKs startingat the breeding grounds on the Arctfctundra, Canada geese and diving ducks:incl uding canvasbacksp redheads and scaup~come from their breeding grounds on thegreat northern plains <strong>of</strong> central Canada,f 1 y southeaster1 y across the Great <strong>Lake</strong>s,crossing <strong>Lake</strong> <strong>Erie</strong> in the islands regionrand continue over the mountains <strong>of</strong>PennsylvanSa to winter along the Atlanticcoast in Chesapeake and Delaware Bays.Concurrently, dabbling ducks such asmallards, black ducks, and blue-wingedteals that have gathered tn southernOntario during the fall, also leave thefeeding grounds, cross western <strong>Lake</strong> <strong>Erie</strong>and proceed southwest over a course thatleads down the Ohio and MississippiValleys (Mississippi Flyway). However,part <strong>of</strong> this duck population, uponreaching the vicinity <strong>of</strong> the <strong>Lake</strong> St.Clair Delta, swings abruptly to thesoutheast, crosses the mountains, andwinters along the Atlantic coast (Lincoln1950) .<strong>The</strong> Mississippi Flyway is easily thelongest migration route <strong>of</strong> any in the<strong>Western</strong> Hemisphere. Its northern terminusis the Arctic coast <strong>of</strong> Alaska, while itssouthern end lies in the Patagonia region<strong>of</strong> Argentina. A1 though the main path <strong>of</strong>the flyway lies to the west <strong>of</strong> the Great<strong>Lake</strong>s, major branches follow the southerntrend <strong>of</strong> <strong>Lake</strong> Michigan and thesouthwestern trend <strong>of</strong> <strong>Lake</strong> <strong>Erie</strong> and theMaumee River valley. Some <strong>of</strong> the blackducks, mallards, and teals that cross theGreat <strong>Lake</strong>s in the vicinity <strong>of</strong> <strong>Lake</strong> St.Clair and western <strong>Lake</strong> <strong>Erie</strong> do not turnabruptly to the southeast, but continue onto the southwest as members <strong>of</strong> theMississippi Flyway bound for the Gulf <strong>of</strong>Mexico coast rather than the Atlanticseaboard.Fall waterfowl migration is at itspeak in September and October, but themain shorebird passage is underway inAugust. As in the spring the western <strong>Lake</strong><strong>Erie</strong> shoreline is an important factor inthe concentration <strong>of</strong> migrants. <strong>The</strong>waterfowl hunting season usually begins Snlate September or eariy October inresponse to this accumuiation Sn andaround the <strong>coastal</strong> marshes.Spring migration begins in lateFebruary with the appearance <strong>of</strong> ringbilledgulls in western <strong>Lake</strong> <strong>Erie</strong>. Marchand early Apri 1 bring heavy waterfowlmovement, ducks and 'loons (Gari_a sp.appearing in open leads as soon as the icebreaks up. Red-winged blackbirds move inlarge numbers starting in 1 ate March. <strong>The</strong>huge Canada goose movement at the west end<strong>of</strong> <strong>Lake</strong> <strong>Erie</strong> normally takes place in earlyApril. With April and May comes the majorpush <strong>of</strong> spring migration, especially amongthe landbirds. Migrants are lessselective than breeding birds in theirchoice <strong>of</strong> habitat, neverthelessrwaterbi rds prefer shore1 ines with pockets<strong>of</strong> vegetation. Coastal marshes and streammouths common1 y attract migrating dabbl ingducks. <strong>The</strong> open water shorelinesconcentrate the diving duck migrants andother waterbirds including loons, grebes,cormorants, tundra swans ((&anuscol umbianus) , red heads, canvasbacks,lesser scaups (Avthva affinis), and redbreastedmergansers (- gerrator).As waterfowl migrate between breedinggrounds and wintering areas, they stop torest and feed in wetlands. <strong>The</strong>se wetlandsare referred to as llconcentration areas."<strong>The</strong> <strong>coastal</strong> wetlands <strong>of</strong> western <strong>Lake</strong> <strong>Erie</strong>provide some <strong>of</strong> the best areas <strong>of</strong> thistype a1 ong the flyways. Concentrationareas are characterized by an abundance <strong>of</strong>waterfowl foods* as well as by low waveenergy and low human disturbance.Canvasbacks, redheads, American wigeons(Anas americanq) , ring-necked ducks(Avthva collaris), and coots feedextensively on submersed pl ants, whereasshovelers (m ~l v~eata 1, oldsquaws(Cl anaul a hvemal is), goldeneyes (Bucephal asp.), and mergansers appear to prefercrayfish, small fish, and other animalfoods. Black ducks, mallards, pintails,teals, scaups, and buffleheads (8.albeola) select from both plant and animalfoods. Canada geese and mallards als<strong>of</strong>eed heavily on waste grains inagricultural fields. Food availabil itymay be more important than foodpreference, especial 1 y during the springmigration when food supplfes are jessabundant. Food availabil ity in wetlandsis reduced by extreme higb and low waterieveis, neavy siitatSonp turbidityp heavyhunting pressure, and other disturbances.In <strong>Lake</strong> <strong>Erie</strong> marshes, Bednarik (1975)
found that preferred natural foods <strong>of</strong>diving ducks, such as wild celery,appeared to be more adversely affected byturbidity and stltatlon than foods <strong>of</strong>dabbling ducks and geese.<strong>The</strong> wintering areas for ducks, geese,swans, coots, and other waterfowl havebeen mapped in detaf 1 by Be1 1 rose ( 19761.<strong>The</strong> Rockefeller Refuge In southwestLouisiana is a well-known wintering areafor migratory waterfowl which cross theGreat <strong>Lake</strong>s. Like the concentrationareas, qua1 ity wintering habitat mustprovide abundant food and protect ion fromwaves and human disturbance. Over theyears, certain waterfowl, particul arl yCanada geese, have modified thei rwintering activity by stopping at sitessomewhat north <strong>of</strong> their former winterareas. In general, most stateconservation agencies do not encourage thecreation <strong>of</strong> resident wintering flocks,particularly in the <strong>Lake</strong> <strong>Erie</strong> region,because <strong>of</strong> the problem <strong>of</strong> waterfowlstarvation during severe winters.Waterfowl that reach the sprlng breedinggrounds in good condition tend to exhibitgreater nesting success than those whichare undernourished.W1iBQdlL;hlr<strong>The</strong>se ducks are socalled because they normally do not divebelow the water for food, but merelydabble on the bottom in shallow water.Annually about 17,500,000 mallards andpintai 1s migrate down f 1 tght corridorsfrom Canada to the Uni ted States east <strong>of</strong>the Rocky Mountains (Bell rose 1968). <strong>The</strong>largest portion, about 12,275r000~ enterthe geographical conflnes <strong>of</strong> theMisslssfppf Flyway from the northern GreatPlajns. About 20% <strong>of</strong> these bi rds continueacross the Mfssissippl Flyway and movedown the Atlantic Flyway. In addition,another 650.000 b1 ack ducks move southfrom Ontario and Quebec.Several corridors carrying dabblingducks cross the Great takes regfon (Figure67 1. An estimated 65,000 ma1 1 ards, 35,000wlgeons, and 25,000 p intaf 1 s move eastwardalong the Chesapeake Bay Corrfdor,startfng in the upper Mississippi Riverval 'ley and progressing through W I scons i n ,Michigan, and Ohlo, It encompasses themarshes <strong>of</strong> <strong>Lake</strong> <strong>Erie</strong> from MonroerMichigan* to Sandusk~r Ohio. From thesemarshes 5% Is a 645-km, nonstop f7 lght toChesapeake Bay, where most <strong>of</strong> these duckswinter. <strong>The</strong> Black Duck Corridor extendssouthwestward from eastern Ontario* acrossthe west end <strong>of</strong> <strong>Lake</strong> Erfe t o theconfluence <strong>of</strong> the Wabash and Oh10 rivers,and on south to Arkansas. Approximately35.000 black ducks use this path.Qfvina ducks, As the name suggests*these ducks normally dive below the waterfor food. About 4,200,000 diving ducksannually migrate south into the UnitedStates east <strong>of</strong> the Rockies (Be11 rose1968). $1 ightly over 60% <strong>of</strong> these arescaup, mostly lesser scaups. Redheads aresecond in abundance at 20%, whilecanvasbacks and ring-necked ducks eachform about 7% <strong>of</strong> the population. As withthe dabbling ducks, numerous diving duckmigration corridors cross the Great <strong>Lake</strong>sregion (Figure 68).<strong>The</strong> Southern Michigan Corridor takesthe main flow <strong>of</strong> diving duck passage fromeastern Wisconsin, across southern Michiganto Saglnaw Bay and the <strong>Lake</strong> St.Clair-Detroit River-<strong>Lake</strong> <strong>Erie</strong> wetlandsareas. Diving ducks congregate on SaginawBay to the extent that peak numbersInclude 22,000 lesser scaups, 22,000redheads, and 7,000 canvasbacks. App roximately160 km t o the south, peakpopulations <strong>of</strong> 380,000 1 esser scaups,260r000 canvasbacks, and 42,000 redheadshave been observed from <strong>Lake</strong> St. Cl ai r towestern <strong>Lake</strong> Erle. Although as many as15,000 dlving ducks may winter on theDetroit River, at least 700,000 fly onfrom <strong>Lake</strong> <strong>Erie</strong> to wintering grounds in theAtlantic Flyway. This route is known asthe Chesapeake Bay Corridor and is astmilar route to the one taken by mallardsand pintails. <strong>The</strong> Central Ohio Corrido-ris a flight path that extends southwardfrom <strong>Lake</strong> Erfe to Florida. Radarobservations <strong>of</strong> diving ducks movdng southpast Columbus, Ohlo, and band recoveriesfrom lesser scaups and redheads f ndicate apassage <strong>of</strong> over 100,000 divers along thiscorridor.GeeseA More than any other species<strong>of</strong> waterfowl, Canada geese have radicallyaltered their mlgratfon routes In the pastfew decades. Bell rose (1968) attributesthis great change fn their migrationhabfts to their rapid adoption <strong>of</strong> newly
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Cover, Aerial view of Uld Womn Gree
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PREFACEThis proti lc on the coastal
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CONTENTSPALTACE ...................
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Pap ai thc Great lakes drainage bas
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This report sl~oultl hc ci ttstl a'
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CONVERSlON FACTORSFOR METRIC (SI) U
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Dimensions of Western Lake Erie Coa
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Average monthly precipitation at fo
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TABLESNumber12345678910111213141516
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CHAPTER 1.INTRODUCTION1.1 COASTAL W
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Tabla 1. Cornparisor1 of ~oastai we
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Figure 2. Study droa in Vichlgan, O
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major wetland local l t fes. Reader
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Cedar Point marshes extend westward
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0 WEST SISTER ISLANDFigure 8. Locat
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Figure 11. Heron and egret nests in
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Figure 13. East end of Sandusky Bay
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Figure 15. Big Island, an experir-i
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eds of floating-leaved species. In
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?ark EnlrAncaSarlctuarv PondWest Cr
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-I he yortion of the Central Lowlan
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the northward plunging end of the F
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'alJ3 ayP1 uJa$san ub steoqs pue 's
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GYPSUMPRESENTCAVESWDERGROUNDLAKE-P
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Figure 28. gap of promtnprit beach
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?and surface had been depressed by
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(Herdendorf and Braidech 1972). Thl
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Redmond st a 1, 11971) mapped thema
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05- low pressure systems from the G
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indicate no regular, predictable cy
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Figure 40. Dontinant surface and bo
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of falling into the lake. The highe
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epresents a retrieved STORET summar
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Table 9.Mean dally solar radiation
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WIthfn the last 50 years the marshe
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Bednarik, K.E. 1975. Environmental
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Dennfs, C.A. 1938. Aquatic gastropo
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tieraendorf, C.E., and S.t. Herdend
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iangj~lz, T.:!. 35a65. Foi-tage Ri$
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Reutter, V.M., and 3.M- Reutter*Pw,
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Sullivan, C.R, 1953. A phytoplankto
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The Ecoloav of Coastal Marshes of W