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<br />FLUCTUATING FLOWS AND BACKWATER HABITATS <br /> <br />1135 <br /> <br />250 (a) 0% Flow Variation 250 (b) 10% Flow Variation <br />200 200 <br />150 150 <br />100 100 <br />50 50 <br />0 0 <br />0 10 20 30 0 10 20 30 <br /> <br /> <br />- <br />N <br />E <br />~ <br />- <br /> <br />250 <br /> <br />(c) 20% Flow Variation <br /> <br />250 <br /> <br />(d) 30% Flow Variation <br /> <br />>- <br />~ <br />:c <br />~ <br />'iij <br />> <br /><C <br />Q) <br />- <br />f! <br />.c <br />Q) <br />~ <br />Q) <br />> <br />t: <br /> <br />200 <br /> <br />..IS.-.........."tl, <br /> <br />200 <br /> <br />50 <br /> <br /> <br />150 <br /> <br />.;..a--'-'-'n <br /> <br />150 <br /> <br />50 <br /> <br /> <br />...--..x <br /> <br />100 <br /> <br />100 <br /> <br />o <br />o <br /> <br />10 20 <br /> <br />30 <br /> <br />o <br />o <br /> <br />10 <br /> <br />20 <br /> <br />30 <br /> <br />250 <br /> <br />(e) 40% Flow Variation <br /> <br />Daily Mean Temperature (oC) <br /> <br />200 <br /> <br />150 <br /> <br />,,- <br /> <br />./!;'-'-'-,6. <br /> <br />Value of Flushina Calibration Parameter <br /> <br />100 <br /> <br />.-- <br /> <br />.,...." <br /> <br />.. <br /> <br />o <br />o <br /> <br />iJ;' <br />-,-:--:';.~~'_:_. .... <br /> <br /> <br />-t;,- 0,00 <br /> <br />-'-0.25 <br /> <br />-. - 0,50 <br /> <br />50 <br /> <br />-0-0,75 <br /> <br />x 1.00 <br /> <br />10 <br /> <br />20 <br /> <br />30 <br /> <br />Daily Mean Temperature (oC) <br /> <br />Figure 5, Simulated invertebrate availability (#, m -2) in backwater 5 as a function of within-day flow variation, daily mean backwater <br />temperature and the invertebrate flushing calibration parameter <br /> <br />over shOlt time intervals, This effect is likely due to our assumption t.hat mainst.em wat.er mixes completely as it <br />flows into the backwat.er during increasing river flow, and undoubtedly also reflects that. calibration data were <br />measured at one point in the backwater whereas the model simulated average temperature of the entire backwater. <br />In general, the water t.emperature model predict.s that, during the summer and fall, backwat.er temperat.ures t.end <br />to be lower than air temperature but higher than mainst.em water temperature. There is, however, daily variation in <br />this ranking depending on the backwater's size and the amount of mixing with the mainstem (Figure 6). <br /> <br />Invertebrate model sensitivity analysis <br /> <br />Of the three inputs evaluated, mean daily backwater temperature had the stTOngest and most direct effect on <br />invertebrate availability (p<O.OOI, r4f= 1,94 for each of the two backwaters). There were also significant <br />interactions between flow fluctuation magnitude and backwater temperature (p < 0,001, df = I, 94 for each of the <br />two backwaters) and fluctuation magnitude, backwater temperature and the flushing calibration parameter <br />(p <0.001, df=4, 94 for each of the two backwaters). <br /> <br />Copyright K;o 2006 John Wiley & Sons, Ltd, <br /> <br />River Res, Applic. 22: 1125-1142 (2006) <br />DOl: 10, I002!rra <br />