Chia-Ying, Lee.

Thesis (M.A.)--National Taiwan University Graduate Institute of Atmospheric Science. / Includes bibliographical references.

Storie, Eric S.

No description available.

May, Brian D.

No description available.

Johannessen, Sophia

No description available.

Andrew, Rex Kelley

No description available.

Kiss, Andrew Elek.

Thesis (Ph.D.)--Australian National University, 2000.

Konter, Jasper Gerard.

Thesis (Ph.D.)--University of California, San Diego, 2007. / Vita. Includes bibliographical references.

Li, Lorraine Kathleen.

Thesis (M. Sc.)--University of Hong Kong, 2006.

Harig, Sven.

University, Diss., 2004--Bremen.

Schweckendiek, Ulf.

University, Diss., 2003--Kiel.

Lüger, Heike.

University, Diss., 2004--Kiel.

Whittaker, Joanne.

Thesis (Ph. D.)--University of Sydney, 2008. / Includes graphs and tables. Includes list of publications. Title from title screen (viewed December 16, 2008). Submitted in fulfilment of the requirements for the degree of Doctor of Philosophy to the Division of Geology and Geophysics, School of Geosciences, Faculty of Science. Includes bibliographical references. Also available in print form.

Schattenhofer, Martha

Bremen, Univ., Diss., 2009

Brown, Adam C.

Thesis (M.S.)--Oregon State University, 2010. / Printout. Includes bibliographical references (leaves 45-48). Also available on the World Wide Web.

Brown, Adam C.

Thesis (M.S.)--Oregon State University, 2010. / Title from PDF title page (viewed Aug. 22, 2009). Includes bibliographical references (leaves 45-48).

Liu, Liyan. Jones, C. K. R. T.

Thesis (Ph. D.)--University of North Carolina at Chapel Hill, 2007. / Title from electronic title page (viewed Dec. 18, 2007). "... in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Department of Mathematics." Discipline: Mathematics; Department/School: Mathematics.

Knab, Nina Jeannette.

Bremen, University, Diss., 2007.

Straub, David Nicholas,

Thesis (Ph. D.)--University of Washington, 1990. / Vita. Includes bibliographical references (leaves [160]-162).

Sweet, William VanderVeer.

Thesis (Ph.D.)--North Carolina State University. / Includes vita. Includes bibliographical references.

Barendse, R. J.

Univ., Diss. u.d.T.: Barendse, Rene J.: Koningen, Compagnieën en kapers: de Arabische zeeën 1640 - 1700--Leiden, 1992. / Frühere Ausg. u.d.T.: Barendse, Rene J.: The Arabian seas 1640 - 1700.

Martin, David William,

Thesis (Ph. D.)--University of Wisconsin--Madison, 1968. / Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 138-144).

Frauenfeld, Oliver Wolfgang.

Thesis (Ph. D.)--University of Virginia, 2003. / Includes bibliographical references (leaves 182-195). Also available online through Digital Dissertations.

Hyrapiet, Shireen,

Thesis (M.S.)--Oklahoma State University, 2006. / Vita. Includes bibliographical references (p. 149-157).

Berkman, Paul Arthur, Jull, A.J.T., Nakamura, Toshio

第12回名古屋大学タンデトロン加速器質量分析計シンポジウム(平成11 (1999年度)報告 名古屋大学タンデトロン加速器質量分析計第1号機の研究実績と1号機,2号磯の利用計画

Senan, Retish

Climatological winds over the equatorial Indian Ocean (EqlO) are westerly most of the year. Twice a year, in April-May ("spring") and October-December ("fall"), strong, sustained westerly winds generate eastward equatorial jets in the ocean. There are several unresolved issues related to the equatorial jets. They accelerate rapidly to speeds over lms"1 when westerly wind stress increases to about 0.7 dyne cm"2 in spring and fall, but decelerate while the wind stress continues to be westerly; eac...

Zika, Jan David, Climate & Environmental Dynamics Laboratory, Faculty of Science, UNSW

The relationship between the general circulation of the ocean and, along-isopycnal and vertical mixing is explored. Firstly, advection down isopycnal tracer gradients is related to mixing in specific regions of the ocean. Secondly, a general inverse method is developed for estimating both mixing and the general circulation. Two examples of down gradient advection are explored. Firstly the region of Mediterranean outflow in the North Atlantic. Given a known transport of warm salty water out of t...

Jennings, Joe C.

Meridional fluxes of silica across the Southern Ocean polar front are attributed to two different processes which generally act in opposite directions. Equatorward low frequency fluxes of silica inferred from ISOS current meter data in the Drake Passage are approximately balanced by poleward meridional diffusion of silica along surfaces of constant potential density. Considering only these two processes, a balance of the silicon budget in the Circumpolar Current can be achieved. The poleward dif...

Hager, Stephen W.

Graduation date: 1969

Amstutz, David E.

Graduation date: 1977

Bodvarsson, Gudrun M.

Graduation date: 1975

Cabrera-Muro, Homero

The Geochemical Ocean Sections Study (GEOSECS) program has carried out an intensive study of physical and chemical parameters in the Pacific and Atlantic Ocean. As a result, an enormous collection of high quality data has been amassed for these two oceans. To analyze the Pacific data, fourteen stations extending from about 50°N to 69°S near 180°longitude have been selected for this study. The section chosen provides a good continuous north-south section in the Pacific from near the Bering Sea to...

Frey, John Richard

This study is an investigation of the endogenous, or internal, rhythms of activity in the ocean shrimp, Pandalus jordani, Groups of shrimp were kept in constant light and temperature conditions in the laboratory, and activity was monitored visually and with infrared photography. Other groups of animals were exposed to 24-hour light-. dark cycles of blue-green light; the activity of these animals was recorded with infrared photography after the light cycle was terminated. It was found that shrimp...

Cutshall, N. H.

Radioactive chromium-51, a waste byproduct from operation of nuclear reactors at Hanford, Washington, has been followed down the Columbia River and into the Pacific Ocean. Chemical factors influencing the partitioning of ⁵¹Cr between solution and sediment have been considered. Chromium-5l, in a hexavalent oxyanion when introduced into the Columbia River, largely remains in solution in a hexavalent anion during its passage through the lower river and after its entrance into the Pacific Ocean. A m...

Johnson, Ron (Ronald E.)

The distribution of Antarctic Intermediate Water in the South Pacific has been examined using a model of horizontal advection, along the Sigma-t surface 27.10, with three point vertical mixing. The core of the Antarctic Intermediate Water mass was traced from the Antarctic Convergence northward. The charts used to describe the distribution were those of core depth, salinity, percentage composition, Equivalent Thickness, and acceleration potential. The percentage composition of Antarctic Intermed...

Spoering, Thomas James

Observations between 20 and 40 m depth were made with a towed thermostor chain in the North Pacific. Despite the rapid vertical variation of buoyancy frequency, spectra of isotherm displacements are in fair agreement with other observations and with the Garrett-Munk model. The spectra show evidence of a shoulder and break in slope at a wavelength of 1 km. There is no evidence of significant variation of spectral levels as a function of buoyancy frequency, tow direction, or wind speed. A peak at ...

Howard, Susan L.

Graduation date: 1998

Jefferts, Katharine

Graduation date: 1983

Simpson, James J. (James Joseph)

Graduation date: 1977

Lin, Huan

Stochastic analysis procedures have been recently applied to analyze nonlinear dynamical systems. In this study, nonlinear responses, stochastic and/or chaotic, are examined and interpreted from a probabilistic perspective. A multi-point-moored ocean structural system under regular and irregular wave excitations is analytically examined via a generalized stochastic Melnikov function and Markov process approach. Time domain simulations and associated experimental observations are employed to assi...

NICOLAS, Guillaume

No description available.

Hay, Carling

A rapidly melting ice sheet produces a distinctive geometry of sea level (SL) change. Thus, a network of SL observations may, in principle, be used to infer sources of meltwater flux. We outline a new method, based on a Kalman smoother, for using tide gauge observations to estimate the individual sources of global SL change. The Kalman smoother technique iteratively calculates the maximum likelihood estimate of Greenland and West Antarctic ice sheet melt rates at each time step, and it allows fo...

Gottlieb, Oded

Complex nonlinear and chaotic responses have been recently observed in various compliant ocean systems. These systems are characterized by a nonlinear mooring restoring force and a coupled fluid-structure interaction exciting force. A general class of ocean mooring system models is formulated by incorporating a variable mooring configuration and the exact form of the hydrodynamic excitation. The multi-degree of freedom system, subjected to combined parametric and external excitation, is shown to...

Semedo, Alvaro

Ocean wind waves represent the atmosphere-ocean boundary, playing a central role in the air-sea exchanging processes. Heat, mass and momentum are transferred across this boundary, with waves mediating the exchange of principally the momentum between the winds and the ocean surface. During the generation process waves are called wind sea. When they leave their generation area or outrun their generating wind they are called swell. The wave field can be said to be dominated either by wind sea or sw...

Ascani, Francois

Thesis (Ph.D.)--University of Hawaii at Manoa, 2008. / For weak Yanai wave amplitude, currents resembling the TEJs are obtained, but only within the beam. They are the mean Eulerian flow, which cancels the Stokes drift of the Yanai waves, yielding a zero-mean Lagrangian flow: the water parcels conserve their potential vorticity (PV) and are stationary over a wave cycle. With stronger amplitude, the Yanai waves become unstable, and lose their energy to small vertical scales where it is dissipated...

Chang, Chin-wen

No description available.

Gritzke, Arnold Richard., Johnson, Robert Henry.

No description available.

Markham, David Gregory.

No description available.

Rovero, Peter Joshua

No description available.

Friese, Laurence Victor

No description available.

Mosey, David Michael

No description available.