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On the distribution of lake temperatures in central Canada as observed from the airPeterson, James T. January 1965 (has links)
Thesis (M.S.)--University of Wisconsin--Madison, 1965. / eContent provider-neutral record in process. Description based on print version record. Bibliography: l. 33-34.
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A laboratory and mathematical study of the 'thermal bar'Elliott, Gillian Hope January 1970 (has links)
The 'migrating thermal bar' phenomenon, known to occur in certain large, dimictic, freshwater lakes, has been studied in laboratory and mathematical models. The temperature fields observed in the laboratory agreed with those observed in Lake Ontario and a linear physical model for the speed of the 'thermal bar', based on negligible horizontal advection and diffusion of heat, gave reasonable values for both the laboratory model and Lake Ontario. Observations were also made of the associated velocity field. On the basis of this laboratory model, which suggests that horizontal advection and diffusion of heat were not of primary importance, mathematical models were developed. First the temperature field was calculated from the one-dimensional heat diffusion equation. Then the velocity field was calculated assuming that the flow was driven by buoyancy forces and balanced by viscous forces. On the basis of the similitude between the temperature fields found in my models and those observed in the lakes, it seems possible that the velocity field of the models also provides a good approximation to the circulation associated with the bar in lakes. There are no direct measurements of the velocities associated with the bar in lakes and they will be difficult to obtain as such velocities are expected, in Lake Ontario, to be only of the order of 1 cm sec⁻¹. / Science, Faculty of / Physics and Astronomy, Department of / Graduate
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Monitoring river restoration using fiber optic temperature measurements in a modeling framework /Huff, Julie A. January 1900 (has links)
Thesis (M.S.)--Oregon State University, 2010. / Printout. Includes bibliographical references (leaves 114-123). Also available on the World Wide Web.
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Heat source : stream, river and open channel temperature predictionBoyd, Matthew S. 10 October 1996 (has links)
Reach defined analysis concentrated on the water temperature change that
occurred in a stream/river segment over the course of one full diurnal cycle. Digital
thermistors, data loggers and computer model development were utilized in reach analysis
to link parameters of the stream system to a specific temperature change. The
methodology employed was relatively simple and fast, and many successive stream
segments were analyzed simultaneously. Reach analysis of stream temperature change
identified the existing components of the stream system that caused increased water
temperature and predicted the effectiveness of managed improvements to the stream
system.
Stream and river temperature regulation has focused on system and basin wide
management. Often, the source of increased water temperature originates in only a part of
the stream system. Reach defined analysis identified the portions of the stream system in
which most water temperature change occurred, offered an explanation for the
temperature response and provided specific information about the alternate strategies that
may ameliorate undesired water temperatures.
The development of the computer model Heat Source included physically based
mathematical descriptions of stream energy and hydrologic processes. An implicit finite
difference numerical method was implemented for simultaneous solution. The
methodology presented in Heat Source is portable and applicable to all streams, rivers and
open channels. / Graduation date: 1997
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Summertime water temperature trends in Steamboat Creek Basin, Umpqua National Forest /Holaday, Steven A. January 1992 (has links)
Thesis (M.S.)--Oregon State University, 1992. / Typescript (photocopy). Includes bibliographical references (leaves 85-90). Also available on the World Wide Web.
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Summertime stream temperatures in the North and South Forks of the Sprague River, south central Oregon /Friedrichsen, Paul T. January 1996 (has links)
Thesis (M.S.)--Oregon State University, 1997. / Typescript (photocopy). Includes bibliographical references (leaves 119-125). Also available on the World Wide Web.
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Water temperature effect on sand transport by size fraction in the Lower Mississippi RiverAkalin, Suleyman. January 2002 (has links)
Thesis (Ph. D.)--Colorado State University, 2002. / Title from citation and abstract page (viewed Nov. 17, 2004). Includes bibliographical references.
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Summertime temperature and circulation patterns in Lake SuperiorSmith, Ned P. January 1972 (has links)
Thesis (Ph. D.)--University of Wisconsin--Madison. / Typescript. Vita. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references.
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Anomalous effects while cooling liquid waterSardo, Rachel. January 2007 (has links)
Thesis (M.S.)--State University of New York at Binghamton, Department of Physics, 2007. / Includes bibliographical references (leaves 79-82).
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Thermally induced mixing in lakesRuppel, James Harold, January 1968 (has links)
Thesis (M.S.)--University of Wisconsin--Madison, 1968. / Vita. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references.
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