Thesis (M.S.)--Wisconsin. / Includes bibliographical references (leaves 172-174).

Thesis (M.S. - Hydrology and Water Resources)--University of Arizona. / Includes bibliographical references (leaves 57-59).

Thesis (Ph.D. - Applied Mathematics)--University of Arizona. / Includes bibliographical references (leaves 129-136).

Thesis (M.E.)--University of Canterbury, 2007. / Typescript (photocopy). Includes bibliographical references (leaves 133-135). Also available via the World Wide Web.

Thesis (Ph. D.)--University of Texas at Austin, 2006. / Vita. Includes bibliographical references.

Catch rates of age-0 and adult crappies Pomoxis spp. were compared between floodplains and coves to determine if differences in densities existed between habitats, and to determine if water levels influenced density relationships. Habitat in a cove and a floodplain of Enid Reservoir was mapped to describe differences in vegetation. Adult crappies were collected with electrofishing and age-0 crappies were collected with trap nets. Coves had the greatest spring densities of adults in 2009 and 2010, whereas floodplains attracted adults earlier in the spawning season. Recruitment of age-0 crappies was related inversely to high water levels during months preceding the spawning period, but related directly to high water levels during the spawning period. Floodplains had the greatest densities of age-0 crappies in most years and reservoirs. These results suggest that management to improve recruitment could focus on timing of water level rises and protection of floodplain habitats.

No description available.

This dissertation is a mathematical investigation of the so-called lake and the great lake equations, which are shallow water equations that describe the long-time motion of an inviscid, incompressible fluid contained in a shallow basin with a slowly spatially varying bottom, a free upper surface and vertical side walls, under the influence of gravity and in the limit of small characteristic velocities and very small surface amplitude. It is shown that these equations are globally well-posed, i.e. that they possess unique global weak solutions that depend continuously on the initial data and on the bottom topography. Provided the initial data is in a class of sufficiently differentiable functions, it remains a member of that class for all times. In other words, the lake and great lake equations have global classical solutions. Moreover, if the equations are posed on a space-periodic domain and the initial data is real analytic, the solution remains real analytic for all times. The proof is based on a characterization of Gevrey classes in terms of decay of Fourier coefficients. Finally, a partial mathematical justification of the formal derivation of the lake equations is given. It is shown that solutions of the lake equation stay close to solutions of the rigid lid equations—the three dimensional Euler equations in the limit of small surface wave amplitude—in the following sense: For every error bound 6 there exists a time T = T(ε) such that for all times t ∈ [0, T] the difference between a solution to the lake equations and the solution to the rigid lid equation corresponding to the same initial data is less than E in a suitably chosen norm. Moreover, T tends to infinity as the aspect ratio of the basin tends to zero.

Thesis (M.S.)--Oregon State University, 2006. / Printout. Includes bibliographical references (leaves 66-69). Also available on the World Wide Web.

No description available.