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Short-period temperature oscillations in the vicinity of Monterey BayMiller, Robert H. January 1965 (has links)
Thesis (M.S.)--United States Naval Postgraduate School, 1965. / Includes bibliographical references (leaf 39).
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Small scale temperature structure of the upper oceanSimpson, James J. (James Joseph) 18 April 1977 (has links)
Graduation date: 1977
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Sea surface temperatures derived from VAS multispectral dataBates, John Joseph. January 1982 (has links)
Thesis (M.S.)--University of Wisconsin--Madison, 1982. / Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 33-35).
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The influence of winds and relative humidity on the seasonal thermocline at ocean station "P",Clark, Marion J. January 1961 (has links)
Thesis (M.S.)--United States Naval Postgraduate School, 1961. / Bibliography: leaf 41.
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Distribucion de temperatura en la Bahia de Todos los Santos (Junio-Octubre 1971)Cabrera Muro, Homero R. January 1972 (has links)
Thesis--Universidad Autónoma de Baja California, 1972. / Includes bibliographical references (leaves 35-38).
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A numerical model study of long-term planetary wave predictabilityWobus, Richard Lee, January 1981 (has links)
Thesis (Ph. D.)--University of Wisconsin--Madison, 1981. / Typescript. Vita. Includes bibliographical references (leaves 190-194).
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A statistical analysis of the relationship between sea surface temperatures and three atmospheric parameters over the North Pacific and North AtlanticSecora, David Norbert. January 1980 (has links)
Thesis (M.S.)--University of Wisconsin--Madison. / Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 81-82).
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On the reduction and interpretation of ocean-floor temperature and heat flow dataShih, Keh-gong 14 November 1967 (has links)
In this thesis, the interpretation and reduction of ocean heat
flow measurements are discussed on the basis of theoretical models.
The instrument effect x heat flow measurements is investigated for the
case of long period measurements by studying the heat conduction
along the measurement probe for both steady and unsteady state bottom
temperatures. This effect is found to be unimportant. Measurement
errors due to recent bottom temperature transients are studied
and the possible magnitude of such errors is estimated. Moreover,
effects of climatic variation on the ocean floor temperature are estimated
on the basis of diffusion models. It is shown that climatic variations
with periods longer than one thousand years will be unattenuated
and will affect the entire ocean floor.
The perturbation method is used to study the effects of an irregular
topography and a variable thickness of ocean floor sediments on the heat flow. Some special examples are given to provide a comparison
between the perturbation solutions and exact solutions of similar
problems. The perturbation method is also applied to a buried body
with different thermal conductivity from its surroundings and the reliability
of the perturbation solution is examined.
Heat flow anomalies due to heat transport by magma intruded
into crustal layers is studied by solving the heat conduction equation.
It is shown that magmatic intrusions can lead to very large surface
heat flow anomalies.
Finally, the possibility of deriving the ocean floor thermal gradient
on the basis of on-ship measurements performed on sediment
cores is investigated. The results appear positive. The temperature
variations in flowing wells and the temperature variation in a cylindrical
sediment core influenced by the movement of water along the
axis of the core are also studied. / Graduation date: 1968
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On the abyssal temperatures of the world oceansOlson, Boyd Ellertson 02 August 1967 (has links)
In comparison with solar radiation, the energy of geothermal
heat flowing through the sea bottom is extremely small; nevertheless,
this energy is not insignificant in the circulation of the bottom water.
Calculations indicate that in the deep basins of the South Atlantic the
water volume transport necessary to remove this heat is at least
one-tenth of the total northward flow of Antarctic Bottom Water.
Plots of mean values of near bottom salinity and oxygen versus mean
potential temperatures help to trace the movement of the bottom
water.
Geothermal and adiabatic warming associated with downslope
flow combine to produce a deep temperature (in situ) minimum in
portions of most of the deep basins of the world. Adiabatic or near
adiabatic temperature gradients have been measured near the bottom
in many of these basins. Evidence of superadiabatic gradients from
temperature measurements made with reversing thermometers is
inconclusive; however, careful measurements with closely spaced
thermometers suggest that such gradients do exist over vertical distances
of a few hundred meters in some of the deepest basins.
Decreasing potential density with depth, as found in some of the
Atlantic Basins in association with sharp temperature and salinity
gradients, is not necessarily an indication of unstable equilibrium.
This is demonstrated by the results of stability calculations in the
manner prescribed by Hesselberg and Sverdrup (1915). / Graduation date: 1968
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Temperature and velocity fields near the deep ocean floor west of OregonKorgen, Benjamin Jeffry 09 May 1969 (has links)
Graduation date: 1969
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