Bibliografie tematiche / Physical oceanography

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Letteratura scientifica selezionata sul tema "Physical oceanography"

Autore: Grafiati
Pubblicato: 4 giugno 2021
Ultima modifica: 5 ottobre 2024

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Articoli di riviste sul tema "Physical oceanography"

1

Hodson, Richard. "Physical oceanography". Nature 575, n. 7782 (13 novembre 2019): S1. http://dx.doi.org/10.1038/d41586-019-03463-x.

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Pelegrí, Josep L., Enrique Álvarez-Fanjul, Manuel Espino, Jordi Font, Gregorio Parrilla e Agustín Sánchez-Arcilla. "Crucial times for Spanish physical oceanography". Scientia Marina 76, S1 (31 agosto 2012): 11–28. http://dx.doi.org/10.3989/scimar.03604.20a.

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3

Wunsch, Carl. "Henry Melson Stommel. 27 September 1920—17 January 1992". Biographical Memoirs of Fellows of the Royal Society 43 (gennaio 1997): 493–502. http://dx.doi.org/10.1098/rsbm.1997.0027.

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Henry Melson Stommel, probably the most original and important physical oceanographer of all time, was in large measure the creator of the modern field of dynamical oceanography. He contributed and inspired many of its most important ideas over a 45–year period. Hank, as many called him, was known throughout the world oceanographic community not only as a superb scientist, but as raconteur, explosives amateur, printer, painter, gentleman farmer, fiction writer and host with a puckish sense of humour and booming laugh.
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Charnock, Henry. "Descriptive physical oceanography". Marine Pollution Bulletin 22, n. 6 (giugno 1991): 313. http://dx.doi.org/10.1016/0025-326x(91)90814-9.

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Biescas, Berta, Barry Ruddick, Jean Kormann, Valentí Sallarès, Mladen R. Nedimović e Sandro Carniel. "Synthetic Modeling for an Acoustic Exploration System for Physical Oceanography". Journal of Atmospheric and Oceanic Technology 33, n. 1 (gennaio 2016): 191–200. http://dx.doi.org/10.1175/jtech-d-15-0137.1.

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AbstractMarine multichannel seismic (MCS) data, used to obtain structural reflection images of the earth’s subsurface, can also be used in physical oceanography exploration. This method provides vertical and lateral resolutions of O(10–100) m, covering the existing observational gap in oceanic exploration. All MCS data used so far in physical oceanography studies have been acquired using conventional seismic instrumentation originally designed for geological exploration. This work presents the proof of concept of an alternative MCS system that is better adapted to physical oceanography and has two goals: 1) to have an environmentally low-impact acoustic source to minimize any potential disturbance to marine life and 2) to be light and portable, thus being installed on midsize oceanographic vessels. The synthetic experiments simulate the main variables of the source, shooting, and streamer involved in the MCS technique. The proposed system utilizes a 5-s-long exponential chirp source of 208 dB relative to 1 μPa at 1 m with a frequency content of 20–100 Hz and a relatively short 500-m-long streamer with 100 channels. This study exemplifies through numerical simulations that the 5-s-long chirp source can reduce the peak of the pressure signal by 26 dB with respect to equivalent air gun–based sources by spreading the energy in time, greatly reducing the impact to marine life. Additionally, the proposed system could be transported and installed in midsize oceanographic vessels, opening new horizons in acoustic oceanography research.
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Yokota, K., K. Katsumata, M. Yamashita, Y. Fukao, S. Kodaira e S. Miura. "Seismic Oceanography: physical oceanography using MCS data". Oceanography in Japan 19, n. 6 (5 novembre 2010): 317–26. http://dx.doi.org/10.5928/kaiyou.19.6_317.

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7

Barclay, David R. "Introduction to the Acoustical Oceanography Technical Committee". Journal of the Acoustical Society of America 155, n. 3_Supplement (1 marzo 2024): A29. http://dx.doi.org/10.1121/10.0026673.

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The Acoustical Oceanography Technical Committee is responsible for representing and fostering Acoustical Oceanography within the Acoustical Society of America. It is concerned with the development and use of acoustical techniques to measure and understand the physical, biological, geological, and chemical parameters and processes of the sea. Several acoustical methods are used to quantitatively study various oceanographic processes. Approaches include ocean parameter estimation by acoustical methods, remote sensing by passive and active acoustics, acoustic imaging, inversion, and tomography, and developing acoustical instrumentation for oceanographic studies.
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Mellor, George, e Rui Xin Huang. "Introduction to Physical Oceanography". American Journal of Physics 65, n. 10 (ottobre 1997): 1028–29. http://dx.doi.org/10.1119/1.18716.

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Brink, Kenneth H. "Coastal Physical Oceanography Workshop". Eos, Transactions American Geophysical Union 69, n. 14 (1988): 204. http://dx.doi.org/10.1029/88eo00127.

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A., Balagiu. "Elements of oceanographic terminology in english and romanian". Scientific Bulletin of Naval Academy XXII, n. 1 (15 luglio 2019): 200–205. http://dx.doi.org/10.21279/1454-864x-19-i1-028.

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Oceanography is a vast domain dealing with various aspects of marine life, physical and chemical aspects of the seas and oceans of the world. Searching available oceanographic documents of the 19th, 20th and 21st century, the aim of the paper is to emphasize the specific terminology of at least one of the branches of oceanography. The branches of oceanography deal with marine biology, ocean chemistry, marine geology and marine physics. The differences between the Romanian and English terminology according to the etymology are brought into discussion and conclusions drawn according to the similarities and differences.
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Tesi sul tema "Physical oceanography"

1

Buffett, Grant George. "Seismic Oceanography: A New Tool to Characterize Physical Oceanographic Structures and Processes". Doctoral thesis, Universitat de Barcelona, 2011. http://hdl.handle.net/10803/1939.

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Large scale global oceanic circulation redistributes heat and freshwater and therefore affects global climate. One of its main forcing mechanisms is, in addition to surface heat and freshwater fluxes, the diapycnal (across lines of equal density) mixing in the ocean interior. The energy needed to drive the mixing processes is mainly provided by tides and wind [Wunsch, 2002]. It is transformed into internal wave energy, cascading through a range of smaller scales leading finally into turbulence and molecular dissipation. Water masses in the ocean are stratified and often separated by relatively thin layers with strong gradients in temperature and/or salinity across which heat and mass transfer occur in order to maintain global circulation and stratification. However, these processes are difficult to observe in practice. Below a few meters, the ocean is opaque to light, and thus to direct optical observations of deep processes [Thorpe, 2005]. Therefore, the development of scientific methodologies and instruments to directly or indirectly measure processes in the ocean interior are of high importance to understanding those processes and their implications.

The motivation behind this research is two-tier: 1) broadly, and academically, it is the scientific curiosity of understanding the ocean in order to better comprehend its role in the context of Earth systems; 2) expressly, the motivation is to develop the methodological toolset necessary to observe the ocean on a spatial and temporal scale not possible with traditional oceanographic techniques, thus allowing the foundation of more accurate models of ocean circulation and thereby, ocean-climate interactions.

The toolset is emerging as a robust technique of physical oceanography known as 'seismic oceanography'. By definition, seismic oceanography is the application of multichannel seismic (MCS) reflection profiling to physical oceanography. This definition, however, could be subject to future revision and refinement because the development of seismic oceanography observational tools will inevitably lead to newer perspectives.

The Mediterranean Outflow Water (henceforth, MOW) is a natural laboratory for seismic oceanography. The MOW was chosen to test seismic reflection in oceanography for three main reasons: 1) The strong oceanographic signature of the MOW. Due to the penetration of the MOW into the North Atlantic through the Strait of Gibraltar, strong characteristic contrasts in temperature (1.5 °C) and salinity (0.3 psu) and thus, density (0.4 kg/m3) are observed between the MOW and the surrounding Atlantic waters [Baringer and Price, 1997]. These contrasts in density (along with sound speed) are the contributing factors to reflection coefficient, making the identification of structures and processes possible. 2) The large variety of oceanographic and topographic features, such as a continental slope, undulating seafloor (including seamounts and basins) and mesoscale Mediterranean salt lenses (meddies). These structures and processes are believed to play an important role in maintaining the temperature and salinity distribution in the north Atlantic [Bower et. al., 1997]. 3) Finally, extensive archived data sets of bothoceanographic and seismic data place interpretive constraints on the data collected.

Part I of this thesis consists of two peer-reviewed papers published by the author and coauthors (Chapters 1 and 2), one manuscript submitted for publication (Chapter 3) and two published peer-reviewed research letters that the author played a lesser role developing (Chapter 4). Part II of the thesis addresses the seismological (Chapter 5) and oceanographic backgrounds (Chapter 6) in the context of some of the structures and processes that are amenable to seismic ensonification. Part III consists of general discussions and conclusions (Chapter 7) and potential future research and development (Chapter 8).
La motivació que hi ha al darrera d'aquest treball es pot separar en dos nivells: 1) En termes generals, i acadèmicament, és la curiositat purament científica d'estudiar l'oceà per tal de comprendre millor el seu paper en el context de les Ciències de la Terra; 2) Concretament, la motivació és desenvolupar les eines necessàries per a observar l'oceà a una escala espaial i temporal que no és possible amb les tècniques tradicionals oceanogràfiques, permetent així generar models més precisos de circulació oceànica i, per tant, de les interaccions oceà-clima.

L'objectiu a curt i mitjà termini d'aquesta tesi és el desenvolupament de noves eines d'oceanografia física que proporcionin noves perspectives sobre la dinàmica oceànica. Aquest conjunt d'eines està emergint com una metodologia sòlida dins de l'oceanografia física coneguda com 'oceanografia sísmica'. Per definició, l'oceanografia sísmica és l'aplicació de la sísmica de reflexió multicanal (MCS) a l'oceanografia física. Aquesta definició, però, podria estar subjecte a una futura revisió i perfeccionament, ja que el desenvolupament d'eines d'oceanografia sísmica inevitablement donarà lloc a noves perspectives.

La part principal d'aquesta tesi la constitueixen quatre articles, publicats per l'autor i co-autors al llarg del seu període d'investigació (capítols 1, 2 i 4); així com un article sotmès (Capítol 3). En la segona part, com a suport per als lectors no familiaritzats, s'aborden els antecedents sismològics (Capítol 5) i oceanogràfics (Capítol 6) en el context d'algunes de les estructures i processos que són susceptibles de ser identificats mitjançant la sísmica. Les conclusions generals es presenten en el Capítol 7 i en el Capítol 8 es donen algunes recomanacions per a futures investigacions i desenvolupaments (Part III). La tesi es complementa amb quatre apèndixs, on a banda d'un ampli resum en català (Apèndix I), hi ha els diagrames de flux utilitzats per l'autor en el processament de les dades sísmiques (Apèndix II), un conjunt de set desplegables de les seccions sísmiques en gran format (Apèndix III) i finalment un glossari de termes útils per ajudar als lectors no iniciats en qualsevol de les branques de la sismologia o l'oceanografia (Apèndix IV).
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Veilleux, Lorraine. "Physical oceanography of northern estuaries". Thesis, McGill University, 1990. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=59830.

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Within the context of oceanographic research on northern estuaries in James Bay and Hudson Bay, and in relation with hydroelectric developments and their impact on the physical environment, two studies were undertaken. Both concern the importance of bottom topography, tidal motion and fresh water input on the estuarine processes in these areas.
The first one, in Rupert Bay (south-eastern corner of James Bay), describes tidal and local wind effects on circulation and mixing patterns for summer conditions. An estimate of terms in the lateral momentum equation shows that the centrifugal acceleration, the Coriolis force and the baroclinic pressure gradient are the most important forces at a mid-bay cross section transect.
The second study is concerned with the freshwater plume of Great Whale River (south-eastern Hudson Bay). CTD measurements were used to examine the lift-off point of the plume for under-ice and increasing discharge conditions. Comparison with existing models shows them to be inappropriate for under-ice conditions. Finally, the presence of supercooled water masses in the region of the study is reported.
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Mondello, Nicholas. "Physical oceanography off the South Coast of Western Australia". Thesis, Mondello, Nicholas (2017) Physical oceanography off the South Coast of Western Australia. Honours thesis, Murdoch University, 2017. https://researchrepository.murdoch.edu.au/id/eprint/40163/.

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Compared to neighbouring regions of ocean, the south coast of Western Australia (WA) has received relatively little scientific attention despite a range of Australian Commonwealth marine protected areas having been established in the region as of 2012. The ocean off the south coast of WA is characterised by a canyon-dense continental shelf edge including the Bremer Canyon, a shelf edge canyon of approximately 8 km width. There are also two main currents in the region, the eastward flowing Leeuwin Current (LC) situated above the continental shelf edge, and the westward flowing Flinders Current (FC) situated south of the continental shelf. The Blue-link Reanalysis (BRAN) ocean forecasting model simulates the currents, temperature and salinity around Australia at daily intervals from 1994 – 2016 with 1/10th degree resolution. It has been speculated that these currents may interact with the canyons along the shelf edge to induce oceanographic conditions conducive to increased pelagic productivity and ecological diversity. This study was a two-part investigation of the physical oceanography off the south coast of WA with a focus on shelf edge dynamics near Bremer Canyon. It involved the use of the (BRAN) model and in situ data including conductivity, temperature and depth (CTD) profiles during January 2017 and temperature logger measurements from near Bremer Canyon between 2015 and 2017. The BRAN outputs were in close agreement with previous studies of the LC and FC and showed that the mixed layer depth (MLD) was shallowest (<50 m) in summer and deepest in winter (>200 m), in sync with seasonal heat flux. The CTD results were within one SD of the average BRAN profiles and MLD results for January. The volume transport of the LC and strong westerly wind events were dominant drivers of the temperature variation along the shelf edge during autumn and winter of 2015 as the warm LC water was forced downwards. In spring and summer, the volume transport of the LC was lowest (1.6 Sv) and other factors became dominating drivers of the shelf edge temperature variation including eddy kinetics and canyon-related processes. The BRAN outputs effectively simulated the mesoscale features examined in this study including the volume transport of the LC, westerly wind forced response and the influence of mesoscale eddies. These processes have the potential to influence the pelagic ecology through vertical mixing and upwelling.
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Jarvis, Marley. "Physical Oceanography, Larval Dispersal, and Settlement Across Nearshore Fronts". Thesis, University of Oregon, 2015. http://hdl.handle.net/1794/18711.

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The larvae of coastal species interact with nearshore currents that are complex and can alter dispersal. I investigated two sites in southern Oregon with different nearshore hydrodynamics: the first site, Sunset Bay, is a small cove with a topographic front that extends across the mouth during upwelling-favorable winds. Using holey sock drogues at 1.5 m and 5.5 m depths and surface drifters at 10 cm depth, I found that, when the front was present, water at 1.5 m was retained within the bay whereas water was exchanged across the front at a depth of 5.5 m. Surface drifters indicated a surface convergence. Surface plankton tows on either side and within the frontal convergence (a shore-parallel foam line) found significantly higher concentrations of barnacle cyprids, crab megalopae and zoea, polychaete larvae, platyhelminthes juveniles, isopods, amphipods, harpacticoid copepods, and fish eggs. Crustacean nauplii (barnacle, euphausiid, and copepod) and calanoid copepods were not concentrated in the convergence, and when the front and foam line were absent, no taxa were concentrated. Plankton tows taken within the foam line as it dissipated shoreward during a wind-reversal event found that concentrations of cyprids, megalopae, and gastropod veligers remained high as the foam line moved, suggesting that it acts as a moving convergence propagating competent larvae shoreward. I measured settlement of two taxa at Sunset Bay and Shore Acres, an open-coast site <2 km away. Barnacle settlement measured every other day from June-September 2013 was significantly cross-correlated with the maximum daily tidal height at lags of -2 days at Sunset Bay and +2 and +4 days at Shore Acres. Settlement was also significantly negatively cross-correlated with wave height at a lag of -4 days at Sunset Bay. Coralline algae settlement measured during eight 48-hr periods in July-August 2013 was significantly negatively correlated with wave height (n = 8, R2 = 0.76, P = 0.0049) at Shore Acres but not at Sunset Bay. Despite the close proximity of the Sunset Bay and Shore Acres sites, settlement patterns differed between taxa, suggesting that differences in nearshore hydrodynamics might affect the supply of water and larvae to shore. This dissertation includes unpublished co-authored material.
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Bâcle, Julie. "The physical oceanography of waters under the North Water Polynya /". Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp03/MQ64314.pdf.

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Le, Quéré Corinne. "Physical oceanography of the Baie des Chaleurs, Gulf of St. Lawrence". Thesis, McGill University, 1992. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=56761.

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Time series of temperature and salinity from current meters moored in 1988 and 1990 along the north shore of Baie des Chaleurs were analyzed to characterize the frequency of upwelling events. Upwelling was found to propagate cyclonically with speeds of 40 to 85 km per day. Moderate correlations between $ sigma sb{ rm t}$ and zonal wind stress were found. The interaction of buoyancy, topography, and oscillating wind stress simulated the upwelling in a reduced gravity model. The dominant frequencies of the upwelling events were approximately 4.5 to 10 days.
Three water masses, one between the surface and the thermocline, one straddling the thermocline, and one at the bottom, were found to describe nicely the TS properties of the water column, as observed from the 1991 CTD data.
The observed circulation, from August to October 1990, was cyclonic, with baroclinicity observed in the bottom two layers, and at two stations in the top layers.
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7

Bain, Cairns Alexander Robertson. "Empirical dynamics of a small scale coastal upwelling region". Doctoral thesis, University of Cape Town, 1991. http://hdl.handle.net/11427/21855.

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The study investigates the dynamics of a small space scale (less than 10 km) coastal upwelling region at the temporal scales spanning hours to years. Three to four year time series data sets of, sea temperatures at different depths (2m, 5 m and 8,5 m) one kilometer offshore, of wind and of waves, obtained from Eskom for the Koeberg nuclear power station site study near Melkbosstrand (33° 41'S, 18° 26'E) were digitized on an hourly basis. An emphasis is placed on the study of the wind and sea temperature data, the latter being an unique data set in the South African context. The data were filtered into different frequency bands (<12,0 <0,5 <0,025 cpd). Simple statistics, linear correlation and spectral analysis were used to characterize these bands. Dominant temporal scales were identified as the seasonal, event (synoptic) and diurnal time scales. The characterization of the latter two time scales were supplemented with field work which inter alia measured: sea temperature profiles and transects; sea surface temperature distribution with the airborne radiation thermometry technique and Lagrangian currents.
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Addison, Victor G. "The physical oceanography of the northern Baffin Bay-Nares Strait region". Thesis, Monterey, California. Naval Postgraduate School, 1987. http://hdl.handle.net/10945/22417.

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Approved for public release; distribution is unlimited
A dense network of conductivity-temperature-depth measurements was conducted from Baffin Bay northward to 82 deg 09 min N at the entrance to the Lincoln Sea, in the most comprehensive physical oceanographic survey ever performed in the northern Baffin Bay-Nares Strait region. These data indicate Nares Strait Atlantic Intermediate Water and Arctic Basin Polar Water to be derived from Arctic Basin waters via the Canadian Archipelago, whereas the West Greenland Current (WGC) is the source of the comparatively dilute West Greenland Current Atlantic Intermediate Water and West Greenland Current Polar Water fractions. Baffin Bay Surface Water is found seasonally throughout northern Baffin Bay. Recurvature of component branches of the WGC, which attains a maximum baroclinic transport of 0.7 Sv, occurs primarily in Melville Bay (0.2 Sv), south of the Carey Islands (0.1 Sv) and ultimately in Smith Sound (0.2 Sv). The Baffin Current originates as an ice-edge jet in Smith Sound and is augmented by net outflow from Smith, Jones and Lancaster Sounds at rates of 0.3 Sv, 0.3 Sv and 1.1 Sv, respectively. Circulation in Smith, Jones and Lancaster Sounds can be described in terms of the Geostrophic Estuarine Circulation Model. The North Water is caused by the combined influences of near-surface layer enthalpy and mechanical ice removal. KeywordsL Sea water temperature; Oceanographic data; Straits; Sounds(Waterways); Ocean currents
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Collins, Charine. "The dynamics and physical processes of the Comoros Basin". Doctoral thesis, University of Cape Town, 2013. http://hdl.handle.net/11427/6467.

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Includes abstract.
Includes bibliographical references.
The main objective of this thesis was to investigate the circulation in the ComorosBasin using observed and model datasets. These data were used to establish whether or not a Comoros Gyre exists and to investigate the nature of the eddy variability in the basin.The water masses in the Comoros Basin emulate those found further south in the Mozambique Channel. The presence of AAIW north of Madagascar confirmed that this water mass enters the Comoros Basin from the east while the presence of North Atlantic Deep Water showed that this water mass is capable of spreading northward over the Davie Ridge. The main currents in the Comoros Basin, the westward flowing NEMC and a poleward current along the western boundary, are under the influence of the monsoon winds. The NEMC intensifies during the Southwest monsoon in response to a strong wind jet which develops off the northern tip of Madagascar, whereas the poleward current weakens due to the opposing force imposed by the southwesterlies. Additionally, the circulation in the basin consist of meso-scale eddies of both polarities. Anti-cyclonic eddies, with lifespans of
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Vianello, Patrick Angus. "A qualitative and physical analysis of processes around the Mascarene plateau". Doctoral thesis, University of Cape Town, 2015. http://hdl.handle.net/11427/16940.

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Includes bibliographical references
The Mascarene Plateau is a submerged volcanic plateau to the east of Madagascar which extends over 2200 km between the Seychelles and Mauritius. It is a complex feature, which is composed of 4 banks separated by 3 channels - namely the Seychelles, Saya de Malha, Nazareth and Cargados-Carajos Banks. The main objective of this thesis is to analyze cruise data obtained during the October/November 2008 ASCLME (Agulhas Somali Current Large Marine Ecosystem) cruise on board the Dr Fridtjof Nansen which surveyed the region around the Mascarene Plateau. Due to the paucity of data in the region, the cruise was a routine cruise with no specific scientific questions to be answered. A comparison is also made between sea surface temperature (SST) and Acoustic Doppler Current Profiler (ADCP) derived currents on board to satellite estimate to possibly extend cruise results in space and time. Although the resolution of satellite estimate is low compared to cruise measurements, satellite estimate of geostrophic velocities and sea surface temperatures compare well with cruise data and can therefore be used in the region with confidence. This is invaluable since the Mascarene Plateau is relatively poorly understood and it allows us to link cruise data with Rossby waves and currents impacting the region. This is the second cruise in the region as there was a research cruise on board the RRS Charles Darwin during June/July 2002. However, the June/July 2002 cruise did not sample the banks of the Mascarene Plateau.
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Libri sul tema "Physical oceanography"

1

Jochum, Markus, e Raghu Murtugudde, a cura di. Physical Oceanography. New York, NY: Springer New York, 2006. http://dx.doi.org/10.1007/0-387-33152-2.

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Reddy, M. P. M. Descriptive physical oceanography. Lisse [Netherlands]: A. A. Balkema Publishers, 2001.

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3

Dijkstra, Henk A. Nonlinear Physical Oceanography. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-015-9450-9.

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H, Stewart Robert. Introduction to physical oceanography. 2a ed. [College Station, Tex: Texas A & M University], 2008.

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5

Knauss, John A. Introduction to physical oceanography. 2a ed. Upper Saddle River, N.J: Prentice Hall, 1997.

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6

Pickard, George L. Descriptive physical oceanography: An introduction. 4a ed. Oxford, [Oxfordshire]: Pergamon Press, 1988.

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7

Bruner de Miranda, Luiz, Fernando Pinheiro Andutta, Björn Kjerfve e Belmiro Mendes de Castro Filho. Fundamentals of Estuarine Physical Oceanography. Singapore: Springer Singapore, 2017. http://dx.doi.org/10.1007/978-981-10-3041-3.

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Adler, Robert J., Peter Müller e Boris L. Rozovskii, a cura di. Stochastic Modelling in Physical Oceanography. Boston, MA: Birkhäuser Boston, 1996. http://dx.doi.org/10.1007/978-1-4612-2430-3.

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Godin, Gabriel. Bad science in physical oceanography. Ottawa, ON: Anadyomene Edition, 2003.

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J, Emery William, a cura di. Descriptive physical oceanography: An introduction. 5a ed. Oxford: Pergamon Press, 1990.

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Capitoli di libri sul tema "Physical oceanography"

1

Dobson, Fred. "Introductory Physical Oceanography". In Introductory Physics of the Atmosphere and Ocean, 53–119. Dordrecht: Springer Netherlands, 1986. http://dx.doi.org/10.1007/978-94-009-5484-7_2.

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2

Warren, Bruce A. "Historical Introduction". In Physical Oceanography, 1–14. New York, NY: Springer New York, 2006. http://dx.doi.org/10.1007/0-387-33152-2_1.

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3

Philander, S. George. "Sextant to Satellite". In Physical Oceanography, 153–63. New York, NY: Springer New York, 2006. http://dx.doi.org/10.1007/0-387-33152-2_10.

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Von Storch, Hans, Jürgen Sündermann e Lorenz Magaard. "Interview with Klaus Wyrtki, 25 February 1999". In Physical Oceanography, 203–37. New York, NY: Springer New York, 2006. http://dx.doi.org/10.1007/0-387-33152-2_13.

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Bryan, Kirk. "Modeling Ocean Circulation". In Physical Oceanography, 29–44. New York, NY: Springer New York, 2006. http://dx.doi.org/10.1007/0-387-33152-2_3.

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McPhaden, Michael J. "El Niño and Ocean Observations". In Physical Oceanography, 79–99. New York, NY: Springer New York, 2006. http://dx.doi.org/10.1007/0-387-33152-2_6.

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Munk, Walter. "Ocean Acoustic Tomography". In Physical Oceanography, 119–38. New York, NY: Springer New York, 2006. http://dx.doi.org/10.1007/0-387-33152-2_8.

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Brown, Wendell S. "Elements of Physical Oceanography". In Springer Handbook of Ocean Engineering, 15–46. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-16649-0_2.

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Schumann, Eckart H. "Physical Oceanography off Natal". In Lecture Notes on Coastal and Estuarine Studies, 101–30. New York, NY: Springer New York, 1988. http://dx.doi.org/10.1007/978-1-4757-3908-4_5.

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Schumann, Eckart H. "Physical oceanography off Natal". In Lecture Notes on Coastal and Estuarine Studies, 101–30. Washington, D. C.: American Geophysical Union, 1988. http://dx.doi.org/10.1029/ln026p0101.

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Atti di convegni sul tema "Physical oceanography"

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Arasakumar, Ganesa Murthy, Kannan Kattari, Arulselvi Velu, Vijayakumar Shanmugam, Uma Pichandi e Perumalsamy Esakkimuthu. "Research on scientometric analysis of physical oceanography". In ADVANCES IN SUSTAINABLE CONSTRUCTION MATERIALS. AIP Publishing, 2023. http://dx.doi.org/10.1063/5.0133549.

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Bolado-Penagos, Marina, Ana Aldarias, Theocharis A. Plomaritis e Irene Laiz. "INTRODUCTION TO PHYSICAL OCEANOGRAPHY FOR HIGH-ABILITY STUDENTS". In 15th International Technology, Education and Development Conference. IATED, 2021. http://dx.doi.org/10.21125/inted.2021.0386.

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Luther, D. S. "Physical oceanography from deep ocean submarine cable observations". In 3rd International Workshop on Scientific Use of Submarine Cables and Related Technologies. IEEE, 2003. http://dx.doi.org/10.1109/ssc.2003.1224154.

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Huntley, D. A. "Nearshore Physical Oceanography: Recent Trends and Future Prospects". In NCK-days 2012 : Crossing borders in coastal research. Enschede, the Netherlands: University of Twente, Department of Water Engineering & Management, 2012. http://dx.doi.org/10.3990/2.169.

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Norman, Noorafiza, e Nurul Hawani Idris. "Exploring a linked data approach in accessing physical oceanography archive". In 2017 IEEE 15th Student Conference on Research and Development (SCOReD). IEEE, 2017. http://dx.doi.org/10.1109/scored.2017.8305420.

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Lugo-Fernández, Alexis. "MMS Physical Oceanography of Slope and Rise (POSAR) Workshop Results". In Offshore Technology Conference. Offshore Technology Conference, 2001. http://dx.doi.org/10.4043/12997-ms.

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Lubis, Muhammad Zainuddin, Budiana, Oktavianto Gustin, Widya Rika Puspita, Amandangi Wahyuning Hastuti, Satria Antoni, Insaniah Rahimah, Husnul Kausarian e Budhi Agung Prasetyo. "Physical Oceanography and Hydrodynamic Modelling in Tembesi Reservoir Waters, Batam". In 2020 3rd International Conference on Applied Engineering (ICAE). IEEE, 2020. http://dx.doi.org/10.1109/icae50557.2020.9350549.

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Foote, K. G. "Measurement of morphology and physical properties of zooplankton". In IEE Colloquium on Recent Advances in Sonar Applied to Biological Oceanography. IEE, 1998. http://dx.doi.org/10.1049/ic:19980183.

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Chen, Chi-Fang, Hsiang-Chih Chan, Ray-I. Chang, Tswen-Yung Tang, Sen Jan, Chau-Chang Wang, Ruey-Chang Wei et al. "Data demonstrations on physical oceanography and underwater acoustics from the MArine Cable Hosted Observatory (MACHO)". In OCEANS 2012 - YEOSU. IEEE, 2012. http://dx.doi.org/10.1109/oceans-yeosu.2012.6263639.

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Wood, Stephen, Todd Allen, Sean Kuhn e Joseph Caldwell. "The Development of an Autonomous Underwater Powered Glider for Deep-Sea Biological, Chemical and Physical Oceanography". In OCEANS 2007 - Europe. IEEE, 2007. http://dx.doi.org/10.1109/oceanse.2007.4302217.

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Rapporti di organizzazioni sul tema "Physical oceanography"

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Eert, J. Physical oceanography. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2012. http://dx.doi.org/10.4095/290247.

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NATIONAL RESEARCH COUNCIL WASHINGTON DC. Statistics and Physical Oceanography. Fort Belvoir, VA: Defense Technical Information Center, gennaio 1993. http://dx.doi.org/10.21236/ada268565.

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Pounder, E. R. Physical oceanography near the North Pole. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/126775.

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Bennett, Andrew F. Applications of Parallel Computing in Physical Oceanography. Fort Belvoir, VA: Defense Technical Information Center, settembre 1997. http://dx.doi.org/10.21236/ada627882.

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Geer, Ira W. The Maury Project: Exploring the Physical Foundations of Oceanography,. Fort Belvoir, VA: Defense Technical Information Center, ottobre 1997. http://dx.doi.org/10.21236/ada329566.

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Piper, D. J. W. Surficial geology and physical properties 7: paleo-oceanography and paleo-glaciology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/210699.

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Lozier, M. S. Implementation of a Mentoring Program for Junior Women in Physical Oceanography. Fort Belvoir, VA: Defense Technical Information Center, settembre 2007. http://dx.doi.org/10.21236/ada605659.

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Westbrook, Elizabeth, Frederick M. Bingham, Susannah Brodnitz, J. Thomas Farrar, Ernesto Rodriguez e Christopher Zappa. Submesoscale Ocean Dynamis Experiment (S-MODE) Data Submission Report. Woods Hole Oceanographic Institution, aprile 2024. http://dx.doi.org/10.1575/1912/69362.

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Abstract (sommario):
This document reviews the sampling details of the S-MODE (Submesoscale Ocean Dynamics Experiment), a NASA-funded, EVS-3 (Earth Venture Suborbital-3), oceanographic field program. It describes what measurements were collected, when and with what instruments and platforms. For each measurement platform it gives simple plots showing the basic dataset, and describes the sampling in detail. S-MODE in situ and aircraft data are available from the PO.DAAC (Physical Oceanography Distributed Active Archive Center) landing page, and individual datasets are also available at the DOIs listed in the “Data Availability” section of this report.
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Lozier, M. S. A Focus on the Scientific Contributions by Women to the Field of Physical Oceanography. Fort Belvoir, VA: Defense Technical Information Center, settembre 2006. http://dx.doi.org/10.21236/ada613110.

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Boyd, Janice D. Descriptive Physical Oceanography of the North Pacific, Sea of Japan (East Sea) and Sea of Okhotsk. Fort Belvoir, VA: Defense Technical Information Center, gennaio 1995. http://dx.doi.org/10.21236/ada311009.

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