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<br />I <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Backwater <br /> <br />GLOSSARY <br /> <br />A body of water with no measurable velocity, created by a drop in water level which cuts off <br />flow through a secondary channel or a portion of the main river channel. Access to the main <br />river channel is not blocked. Backwaters ice over early and are one of the first habitats to <br />form solid ice cover. <br /> <br />cfs Cubic feet per second; 35.31 cfs = 1 ems <br /> <br />Free Water Depth <br /> <br />Frazil Ice <br /> <br />Depth of water above substrate and below ice cover (includes both surface ice and <br />frazil ice). Does not include water between ice layers. <br /> <br />Form of ice found on frozen rivers, caused by supercooled water in motion and formed as <br />variable size crystals; forms solid surface ice at low velocities or anchor ice at high velocities. <br /> <br />Freezing Point Depression ('d') Measure of the solute content of a solution, and hence its water diffusion <br />pressure through tissue membranes. Most freshwater teleosts (modem bony <br />fishes) have a 'd' for blood and plasma of about -O.570C. <br /> <br />Ice Lenses <br /> <br />Jam Ice <br /> <br />Surface Ice <br /> <br />Type of surface ice formed under fluctuating flow conditions. Typically an ice lens is formed <br />during high flow, then breaks from shore and collapses as the free water drops out beneath <br />it Ice lenses can form daily with daily fluctuating flows, forming and collapsing on top of <br />each other, creating a thick ice layer formed of many different lenses. <br /> <br />Form of ice mass found on frozen rivers, characterized by broken and dislodged blocks of ice <br />mixed with frazi1 ice. <br /> <br />Form of ice found on the surface of rivers and streams; formed by frazi1 ice crystals in areas <br />with current <br /> <br />17 <br />