Relevant bibliographies by topics / Surface marine

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Surface marine'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Surface marine"

1

Jibiki, Tatsuhiro. "Surface Modification in Marine Engineering." Journal of The Japan Institute of Marine Engineering 46, no. 5 (2011): 663–68. http://dx.doi.org/10.5988/jime.46.663.

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Thom, Bruce G., Jock B. Keene, Peter J. Cowell, and Marc Daley. "East Australian marine abrasion surface." Geological Society, London, Special Publications 346, no. 1 (2010): 57–69. http://dx.doi.org/10.1144/sp346.5.

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Kent, Elizabeth C., and John J. Kennedy. "Historical Estimates of Surface Marine Temperatures." Annual Review of Marine Science 13, no. 1 (January 3, 2021): 283–311. http://dx.doi.org/10.1146/annurev-marine-042120-111807.

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Surface temperature documents our changing climate, and the marine record represents one of the longest widely distributed, observation-based estimates. Measurements of near-surface marine air temperature and sea-surface temperature have been recorded on platforms ranging from sailing ships to autonomous drifting buoys. The raw observations show an imprint of differing measurement methods and are sparse in certain periods and regions. This review describes how the real signal of global climate change can be determined from these sparse and noisy observations, including the quantification of measurement method–dependent biases and the reduction of spurious signals. Recent progress has come from analysis of the observations at increasing levels of granularity and from accounting for artifacts in the data that depend on platform types, measurement methods, and environmental conditions. Cutting across these effects are others caused by how the data were recorded, transcribed, and archived. These insights will be integrated into the next generation of global products quantified with validated estimates of uncertainty and the dependencies of its correlation structure. Further analysis of these records using improved data, metadata, and methods will certainly uncover more idiosyncrasies and new ways to improve the record.
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Ista, Linnea K., Maureen E. Callow, John A. Finlay, Sarah E. Coleman, Aleece C. Nolasco, Robin H. Simons, James A. Callow, and Gabriel P. Lopez. "Effect of Substratum Surface Chemistry and Surface Energy on Attachment of Marine Bacteria and Algal Spores." Applied and Environmental Microbiology 70, no. 7 (July 2004): 4151–57. http://dx.doi.org/10.1128/aem.70.7.4151-4157.2004.

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ABSTRACT Two series of self-assembled monolayers (SAMs) of ω-substituted alkanethiolates on gold were used to systematically examine the effects of varying substratum surface chemistry and energy on the attachment of two model organisms of interest to the study of marine biofouling, the bacterium Cobetia marina (formerly Halomonas marina) and zoospores of the alga Ulva linza (formerly Enteromorpha linza). SAMs were formed on gold-coated glass slides from solutions containing mixtures of methyl- and carboxylic acid-terminated alkanethiols and mixtures of methyl- and hydroxyl-terminated alkanethiols. C. marina attached in increasing numbers to SAMs with decreasing advancing water contact angles (θAW), in accordance with equation-of-state models of colloidal attachment. Previous studies of Ulva zoospore attachment to a series of mixed methyl- and hydroxyl-terminated SAMs showed a similar correlation between substratum θAW and zoospore attachment. When the hydrophilic component of the SAMs was changed to carboxylate, however, the profile of attachment of Ulva was significantly different, suggesting that a more complex model of interfacial energetics is required.
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Hayek, Mahmoud, Marie Salgues, Frédéric Habouzit, Sandrine Bayle, Jean-Claude Souche, Klartjee De Weerdt, and Sylvain Pioch. "L’influence de la carbonatation sur la biocolonisation de matériaux cimentaires dans le milieu marin." Matériaux & Techniques 108, no. 2 (2020): 202. http://dx.doi.org/10.1051/mattech/2020020.

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Les ingénieurs spécialisés en génie civil doivent intégrer dans leur design des mesures de protection de la biodiversité marine de qui autorise le concept d’écoconception d’infrastructures marines respectueuses de l’environnement. Les matériaux cimentaires sont privilégiés pour concevoir les infrastructures marines et interagissent avec le milieu marin. Ces structures seront colonisées par des micro-organismes et macroorganismes marins. Dans un premier temps, les organismes forment un biofilm à la surface du béton en fonction des facteurs environnementaux et des propriétés physico-chimiques du matériau. Dans cette étude, il a été démontré que la pré-carbonatation des matériaux cimentaires accélère la croissance des micro-organismes formant le biofilm à leur surface en abaissant le pH de la surface. Il a été démontré en laboratoire que la colonisation de la surface par des micro-organismes augmente également l’hydrophobicité de la surface et pourrait ainsi améliorer la durabilité du matériau en diminuant l’absorption d’eau de mer contenant des agents agressifs.
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Taylor, David B. "Fast modelling of marine surface multiples." Geophysical Prospecting 50, no. 3 (May 2002): 329–40. http://dx.doi.org/10.1046/j.1365-2478.2002.00321.x.

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Wang, Liping, Wenjie Zhao, and Haichao Zhao. "Surface and Interface of Marine Materials." Surface Topography: Metrology and Properties 8, no. 1 (February 4, 2020): 010401. http://dx.doi.org/10.1088/2051-672x/ab6dba.

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Petrone, Luigi. "Molecular surface chemistry in marine bioadhesion." Advances in Colloid and Interface Science 195-196 (July 2013): 1–18. http://dx.doi.org/10.1016/j.cis.2013.03.006.

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Das, Swarup, and S. E. Talole. "Nonlinear Control of Marine Surface Vessels." Journal of The Institution of Engineers (India): Series C 100, no. 2 (March 19, 2018): 385–400. http://dx.doi.org/10.1007/s40032-018-0449-3.

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Colitz, Carmen Maria Helena. "Ocular Surface Diseases in Marine Mammals." Veterinary Clinics of North America: Exotic Animal Practice 22, no. 1 (January 2019): 35–51. http://dx.doi.org/10.1016/j.cvex.2018.08.007.

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Dissertations / Theses on the topic "Surface marine"

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Alme, Jon. "Autotuned Dynamic Positioning for Marine Surface Vessels." Thesis, Norwegian University of Science and Technology, Department of Engineering Cybernetics, 2008. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-8861.

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Dynamic positioning of surface vessels involves control of vessels with changing dynamics, shifting conditions, for different operational tasks. A controller with fixed controller parameters cannot have an optimal performance for all these different cases, and autotuning of the controller would be very valuable. However, dynamic positioning is a complex task, and thus automatic tuning of a dynamic positioning controller is not less so. This thesis does not solve all problems that comes with autotuning of dynamic positioning systems, but it gives an overview of the problem and presents a novel performance index for station keeping. Furthermore, a hybrid controller that can function as a first step in solving the autotuning problem is suggested. The hybrid controller has a fixed controller structure and is a combination of a gain-scheduling controller and an adaptive controller. The adaptive controller is used in an idle (training/learning) mode to populate a look-up table with controller parameters, while the gain-scheduling controller work as a fast-changing dynamical controller, using the controller parameters stored in the look-up table. Each controller parameter set in the look-up table is optimized according to a vessel operational condition, which is defined as a function of environmental conditions (wind, waves, ocean current), vessel draught, and water depth. Optimization of the controller parameters for the different vessel operational conditions is carried out by two different autotuning methods; a genetic algorithm and a rule-based algorithm. Both of these autotuning methods are optimizing the controller gains in a nonlinear PID-controller. The performance index and the two autotuning methods are implemented in Matlab/Simulink, where simulation tests are performed for a 3 DOF mathematical model of a supply vessel. The test scenario includes two different vessel operational conditions, where the controller has been automatically tuned both for minimal position and heading deviation as well as weighting on the use of forces. A comparison of the two autotuning methods is also performed and finally a discussion of the behaviour and tuning of the suggested performance index is carried out.

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Angelopoulos, Christos K. "String stability of multiple surface marine vessels." Thesis, Monterey, California. Naval Postgraduate School, 2011. http://hdl.handle.net/10945/5676.

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The phenomenon of string instability is well known in a platoon of cars moving forward in an Automated Highway System (AHS). It is also known that ships can experience a similar instability phenomenon from mis-coordination of guidance and control laws. The proposed research studies the latter phenomenon, generalized in the case of multiple marine surface vessels moving in a platoon. The question of how it is possible for ships raveling in formation to exhibit the phenomenon of string instability is answered. Moreover, we examine under what conditions this phenomenon can be exhibited, as well as how it can be prevented.
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Zúñiga, Carlos A. "Small flux buoy for characterizing marine surface layers." Monterey, California: Naval Postgraduate School, 2013. http://hdl.handle.net/10945/34767.

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A small easily deployable buoy, Marine-Air-Sea-Flux System (MASFlux), has been developed by the Meteorology Department of the Naval Postgraduate School. This system measures turbulence perturbations, mean wind and thermodynamic profiles, surface wave, and upper ocean temperature simultaneously. This research focuses on testing, documenting, and evaluating the MASFlux performance. The buoy system was tested in the Monterey Bay since August 2012 using small vessels, with the first three deployments focusing on sensor and buoy performance improvements. Concurrent measurements of wave and turbulence fluxes in the lower part of the atmospheric boundary layer during the last three deployments were not subject to apparent sensor errors or excessive mast rotations. Data from these deployments are analyzed here. The two-dimensional wave measurements were compared with those from the Datawell DWR-G4 wave buoys and showed consistent results in all deployments. Turbulent spectra analyses for data before and after buoy motion correction demonstrate the effectiveness in motion correction for the MASFlux. The spectra revealed a significant amount of energy in the atmospheric turbulence at frequencies of the dominant swell. The mean vertical wind profiles also indicated the effects of swell. These initial measurements and results point to great potential for the MASFlux for future air-sea-wave study.
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Qi, Yusheng Ph D. Massachusetts Institute of Technology. "Sea surface wave reconstruction from marine radar images." Thesis, Massachusetts Institute of Technology, 2012. http://hdl.handle.net/1721.1/74939.

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Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Mechanical Engineering, 2012.
Cataloged from PDF version of thesis.
Includes bibliographical references (p. 103-105).
The X-band marine radar is one type of remote sensing technology which is being increasingly used to measure sea surface waves nowadays. In this thesis, how to reconstruct sea surface wave elevation maps from X-band marine radar images and do wave field prediction over short term in real time are discussed. The key idea of reconstruction is using dispersion relation based on the linear wave theory to separate the wave-related signal from non-wave signal in radar images. The reconstruction process involves three-dimensional Fourier analysis and some radar imaging mechanism. In this thesis, an improved shadowing simulation model combined with wave field simulation models for the study of the correction function in the reconstruction process and an improved wave scale estimation model using non-coherent radar data are proposed, which are of great importance in the reconstruction process. A radar image calibration method based on wave field simulation is put forward in order to improve the quality of reconstructed sea surface wave. Besides, a theoretical wave scale estimation model using Doppler spectra of the coherent radar is put forward, which is proposed to be a good alternative to the current wave scale estimation model. The reconstructed sea surface wave can be used for wave field simulation in order to predict the wave field, which is not only an application of this reconstruction process, but also a parameter optimizing tool for the reconstruction process.
by Yusheng Qi.
S.M.
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Lidbury, Ian. "Microbial methylated amine metabolism in marine surface waters." Thesis, University of Warwick, 2015. http://wrap.warwick.ac.uk/68959/.

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Methylated amines, such as trimethylamine (TMA) and trimethylamine N-oxide, are nitrogenous compounds that are thought to be ubiquitous in the marine environment. TMA is a product of the anaerobic degradation of quaternary amines, such as glycine betaine and choline. Through a set of complex chemical and biological interactions, methylated amines play a role in regulating the planet’s climate. Microbial degradation of methylated amines is thought to be a sink for these compounds in the marine environment, however some of the key genes and enzymes responsible for the degradation of methylated amines are unknown. Using Ruegeria pomeroyi DSS-3 as the model organism, the key enzymes for the uptake and catabolism of trimethylamine N-oxide were identified and it was discovered that these genes and enzymes are highly expressed in the seawater, as revealed by the re-analysis of a number of recent metatranscriptomic and metaproteomic datasets. Again using R. pomeroyi as the model organism, it was shown that trimethylamine and trimethylamine N-oxide can be oxidised to CO2 to generate reducing equivalents and ATP. The generation of this reducing power results in a number of physiological benefits which are further discussed in detail. It was determined that bacteria possessing trimethylamine monooxygenase, the key enzyme required for the oxidation of TMA could also oxidise the reduced sulfur compound, dimethylsulfide, when supplemented with methylated amines. The ecology of methylated amine-utilising bacteria was investigated using a newly designed primer set targeting the trimethylamine N-oxide demethylase. The results are presented in detail within. The key genes and enzymes essential for the catabolism of the quaternary amine, choline were also discovered, again using R. pomeroyi as the model organism. The occurrence of genes required for the catabolism of choline are widespread among certain groups of marine bacteria known to interaction with eukaryotic biota, suggesting that this compound may be an essential nutrient for these organisms.
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Boppe, Ravi Shankar. "Structure of turbulence in the marine atmospheric surface layer." Diss., Virginia Tech, 1995. http://hdl.handle.net/10919/37461.

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Turbulence research in the laboratory has confirmed the existence of quasi-coherent structures amidst the chaos of a turbulent boundary layer. It has been observed that a quasi-periodic phenomena called “bursting” accounts for a major contribution to the turbulent Reynolds stress and the production of turbulent kinetic energy. Bursting is the term used for a sequence of events, where a low-speed streak of fluid from the near wall region lifts away from the wall, slowly at first, and then rapidly moves away from the wall as it convects downstream where it becomes unstable and breaks up violently upon interaction with the outer flow. This ejection of low speed fluid into the mean flow is responsible for locally high values of turbulent kinetic energy. Although a great deal is known about these structures in laboratory flows, little has been done to investigate if such structures are universal in turbulent flows, i.e., their existence in large Reynolds number flows such as the turbulent air flow over the ocean. It would seem, intuitively, that such structures, if present in the marine atmospheric boundary layer, would play a major role in the transfer of momentum, mass and heat across the air-sea interface. It is speculated that these motions may also be associated with large scale organized motions in wall bounded turbulent shear flows. The effort aimed at elucidating the physics underlying such structures would be invaluable in contributing to our understanding of the air-sea flux mechanism. In this dissertation, standard ejection detection schemes like the quadrant, the VITA and the modified u-level techniques have been applied to turbulent wind data measured over the ocean to confirm the existence of burst like structures. The proportions of contributions to the Reynolds stress from the four quadrants of the u’w’ plane are in close agreement with the corresponding contributions for a laboratory flow. Ejection detection followed by the grouping of ejections into bursts yielded a mean burst period of 47 s, at a height of 8.2 m above the water surface, where the mean wind velocity was 6.74 m/s. This burst period corresponds well with the peaks obtained from the autocorrelation of the streamwise velocity signal and the first moment of the stress spectrum, confirming the quasi-periodic nature of this phenomena. Furthermore, phase averages of these events show a structure which is similar to the structure of events detected in laboratory flows. The ejection periods are seen to decrease with increasing wind speed. The burst periods decrease at first with increasing wind speed and then appear to attain a constant value after a wind speed of 6-7 m/s. This has been attributed to the breakdown of the grouping algorithm at higher wind speeds. Ejection and burst frequencies exhibit no discernible dependence on the surface wave field. Ejection and sweep motions have been studied at various length scales. The original velocity signal is bandpass filtered for various frequency bands. For each band, the percentage contributions to the Reynolds stress from the quadrants of the u'w’ plane are close to the corresponding quadrant contributions of the other bands. This indicates similar turbulence structure at different scales. The velocity signals for each band have been normalized by their root mean square (RMS) value. Visualizing the signals on nondimensional time shows the signals from each band to be very similar. These results can also be interpreted as evidence for the ejection and sweep motions existing simultaneously at different scales, indicating the fractal nature of these events. Large scale motions, which appear to be associated with ejection and sweep motions, have been identified in the marine atmospheric surface layer using velocity probe measurements at multiple heights. Visualizing these velocity signals suggests that the organized features extend across the depth of the surface layer. Converting the temporal signals to spatial fluctuations suggests that these structures are inclined at an angle while convecting downstream. The inclination angle near the surface (z < 18 m) is approximately 15° and it increases with increasing height to about 45° when z = 45 m. The spatial velocity fluctuations also indicate that these organized features may be large transverse vortical arches.
Ph. D.
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Battista, Thomas Andrew. "Lagrangian Mechanics Modeling of Free Surface-Affected Marine Craft." Diss., Virginia Tech, 2018. http://hdl.handle.net/10919/82928.

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Although ships have been used for thousands of years, modeling the dynamics of marine craft has historically been restricted by the complex nature of the hydrodynamics. The principal challenge is that the vehicle motion is coupled to the ambient fluid motion, effectively requiring one to solve an infinite dimensional set of equations to predict the hydrodynamic forces and moments acting on a marine vehicle. Additional challenges arise in parametric modeling, where one approximates the fluid behavior using reduced-order ordinary differential equations. Parametric models are typically required for model-based state estimation and feedback control design, while also supporting other applications including vehicle design and submarine operator training. In this dissertation, Lagrangian mechanics is used to derive nonlinear, parametric motion models for marine craft operating in the presence of a free surface. In Lagrangian mechanics, one constructs the equations of motion for a dynamic system using a system Lagrangian, a scalar energy-like function canonically defined as the system kinetic energy minus the system potential energies. The Lagrangian functions are identified under ideal flow assumptions and are used to derive two sets of equations. The first set of equations neglects hydrodynamic forces due to exogenous fluid motions and may be interpreted as a nonlinear calm water maneuvering model. The second set of equations incorporates effects due to exogenous fluid motion, and may be interpreted as a nonlinear, unified maneuvering and seakeeping model. Having identified the state- and time-dependent model parameters, one may use these models to rapidly simulate surface-affected marine craft maneuvers, enabling model-based control design and state estimation algorithms.
Ph. D.
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Shuai, Hua. "Characteristics of Coherent Structures in Marine Atmospheric Surface Layer." Thesis, Virginia Tech, 1997. http://hdl.handle.net/10919/36931.

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Wind speed data of multi-heights have been examined to investigate the spatial and temporal characteristics of coherent structures in the near neutral marine atmospheric surface layer. With Taylor's hypothesis, the temporal velocity signals have been transformed to spatial fluctuations and then visualize these spatial velocity fluctuations to identify the coherent structures. It has been confirmed that there exist similar coherent structures in the marine atmospheric surface layer to those in laboratory turbulent boundary layer. These similar coherent structures include ejections, sweeps, shear layers, transverse vortices, and combined events of the shear layers and transverse vortices. Besides these similar coherent structures, there exist the plume and downdraft motions in the unstable marine atmospheric surface layer.

It has been observed that the streamwise spatial length of the ejections and sweeps is 20-250 m and their mean frequency is of order of 0.01-0.001 /s at mean wind speed of 5-12.6 m/s. Between the region of the upstream ejection and downstream sweep motions an inclined shear layer is often seen. The inclined angle of the shear layer has been observed to vary from 30 to 70 degree with the height and length of the the shear layer. The transverse vortices are seen to exist in every region from the wall up to a height of 45 m and their diameter is up to 40 m. The mean frequency of the shear layers and the transverse vortices is of order of 0.001 /s. In the fully developed stage of the combined event of the shear layer and transverse vortex, the shear layer is generally longer and the diameter of the transverse vortex is larger. The mean frequency of the combined event of the shear layers and the transverse vortices is of order of 0.001 /s. The streamwise spatial length of the plume and downdraft motions is generally from 20 m to 50 m.

Analysis indicates that the mean wind speed is a dominant factor in affecting the spatial and temporal characteristics of the coherent structures in the near neutral marine atmospheric surface layer. As the mean wind speed increases, the frequency of the shear related coherent events will increase, while the frequency of the buoyancy related coherent events (plumes and downdrafts) will decrease. The temperature difference between higher level of the surface layer and sea surface is the second main factor in affecting the spatial and temporal characteristics of the coherent structures. As the marine atmospheric surface layer becomes more stable the coherent motions will be suppressed. The effect of the temperature difference on the buoyancy related plume and downdraft motions is more evident than on the other shear related coherent motions.
Master of Science

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Johnston, Rodney G. K. "Deterministic free surface multiple removal of marine seismic data." Thesis, University of Edinburgh, 2000. http://hdl.handle.net/1842/12311.

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This thesis presents a new method for sea surface multiple removal which includes in its solution the information at the source from the oscillating bubbles which generate the propagating wavefield. Arrays of interacting oscillating bubbles excite the earth with sound energy which is recorded as marine seismic reflection data. In the manipulation of the data to produce a detailed image of the earth's subsurface, the first task is the removal of multiple reflections related to the sea surface. The new formulation, in common with other wave-theoretical methods, requires a two-dimensional grid of receivers to record a two-dimensional grid of shots. Using the data themselves, and no information about the subsurface, all multiples are removed in a three-dimensional earth by calculating the plane wave reflection response in the frequency-wavenumber domain. Applying the plane wave concept to waves in three dimensions permits a complicated reflected wave to be decomposed into plane wave components. Each of these scattered upgoing plane wave components comprises primary and multiple reflections. The primaries result from a multiplication of an incident downgoing plane wave component with a plane wave reflection response, unique for the particular downgoing and upgoing plane wave components chosen. The multiples represent a sum of products of scattered downgoing plane wave components with plane wave reflection responses, related to the chosen downgoing and upgoing plane wave components. The result is a set of simultaneous equations whose unknowns form the three-dimensional reflection response. The wavefield from the oscillating bubbles produces the downgoing incident plane wave. There are various methods of measuring this input energy. They depend on the acquisition configuration being used, and the feasibility of placing hydrophones at certain distances from the sources of the oscillating bubbles. Consideration of the fluid dynamics of these oscillating bubbles, in isolation and together, and the wave propagation produced by them, reveals the requisite measurements to describe fully the acoustic output of the source.
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Johnson, Stuart. "Surface microtopography and the fate of seaweed propagules." Thesis, University of Liverpool, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.333579.

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Books on the topic "Surface marine"

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Gade, Martin, Heinrich Hühnerfuss, and Gerald M. Korenowski, eds. Marine Surface Films. Berlin, Heidelberg: Springer Berlin Heidelberg, 2006. http://dx.doi.org/10.1007/3-540-33271-5.

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United States. National Environmental Satellite, Data, and Information Service. Atlas of surface marine data 1994. Washington, D.C: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Environmental Satellite, Data, and Information Service, 1994.

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Uścinowicz, Szymon, and Magdalena Bełdowska. Geochemistry of Baltic Sea surface sediments. Warsaw: Polish Geological Institute-National Research Institute, 2011.

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Hess, Kurt W. Assessment models for surface dispersion of marine pollutants. Washington, DC: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Environmental Satellite, Data, and Information Service, 1985.

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Dean, Walter E. Geochemistry of surface sediments in the Gulf of the Farallones. [Reston, Va.]: U.S. Dept. of the Interior, U.S. Geological Survey, 1995.

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Dean, Walter E. Geochemistry of surface sediments in the Gulf of the Farallones. [Reston, Va.]: U.S. Dept. of the Interior, U.S. Geological Survey, 1995.

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Gardiner, William Wood. Sea surface films: Deposition and toxicity in intertidal habitats. Mount Vernon, Wash: Padilla Bay National Estuarine Research Reserve, 1992.

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IMO/FAO/UNESCO-IOC/WMO/WHO/IAEA/UN/UNEP Joint Group of Experts on the Scientific Aspects of Marine Environmental Protection. The Sea-surface microlayer and its role in global change. Geneva: World Meteorological Organization, 1995.

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Taylor, Scott L., Wanda L. Davis, and Cailin Clarke. Trip under the surface. Toronto: GTK Press, 2004.

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Grange, K. R. Monitoring of littoral macrobenthos and surface sediments in Manukau Harbour, New Zealand. Wellington, N.Z: New Zealand Oceanographic Institute, Division of Water Sciences, 1989.

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Book chapters on the topic "Surface marine"

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Berendsen, A. M. "Surface Preparation." In Marine Painting Manual, 77–105. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-017-2186-8_3.

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Saltzman, Eric S. "Marine aerosols." In Surface Ocean—Lower Atmosphere Processes, 17–35. Washington, D. C.: American Geophysical Union, 2009. http://dx.doi.org/10.1029/2008gm000769.

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Korenowski, Gerald M., Elizabeth A. van Wagenen, and Amir Hirsa. "Imaging surfactant concentration distribution at the air/water interface." In Marine Surface Films, 157–64. Berlin, Heidelberg: Springer Berlin Heidelberg, 2006. http://dx.doi.org/10.1007/3-540-33271-5_15.

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Korenowski, Gerald M., John R. Saylor, Elizabeth A. van Wagenen, Joseph S. Kelley, Mark E. Anderson, and Elizabeth J. Edwards. "Imaging surfactant concentration distributions at the air/water interface." In Marine Surface Films, 165–73. Berlin, Heidelberg: Springer Berlin Heidelberg, 2006. http://dx.doi.org/10.1007/3-540-33271-5_16.

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Ulloa, Osvaldo, and Carolina Grob. "Marine pelagic ecosystems." In Surface Ocean—Lower Atmosphere Processes, 119–37. Washington, D. C.: American Geophysical Union, 2009. http://dx.doi.org/10.1029/2008gm000867.

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Takagi, Toshiyuki. "Energy Production: Biomass – Marine." In Yeast Cell Surface Engineering, 29–41. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-5868-5_3.

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Lohmann, Ulrike. "Marine boundary layer clouds." In Surface Ocean—Lower Atmosphere Processes, 57–68. Washington, D. C.: American Geophysical Union, 2009. http://dx.doi.org/10.1029/2008gm000761.

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Biscaye, Pierre E., David J. Demaster, and Ursula Ginster. "Mineralogy and Surface Properties." In Marine Particles: Analysis and Characterization, 325–42. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm063p0325.

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Zehr, Jonathan P., and Douglas G. Capone. "Biogeography of N2 Fixation in the Surface Ocean." In Marine Nitrogen Fixation, 117–41. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-67746-6_7.

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Massel, Stanisław Ryszard. "An Introduction to Surface Waves." In Fluid Mechanics for Marine Ecologists, 79–106. Berlin, Heidelberg: Springer Berlin Heidelberg, 1999. http://dx.doi.org/10.1007/978-3-642-60209-2_3.

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Conference papers on the topic "Surface marine"

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FORD, ALLEN, ROY TREESE, and STEPHEN CHORNEY. "Surface effect ship seakeeping assessment." In Advanced Marine Vehicles Conference. Reston, Virigina: American Institute of Aeronautics and Astronautics, 1989. http://dx.doi.org/10.2514/6.1989-1470.

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Candries, M. "Drag Reduction by Conditioning of Surface Treated Coatings." In Marine & Offshore Coatings. RINA, 2010. http://dx.doi.org/10.3940/rina.coat.2010.03.

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Mouton, E., and D. Robert. "Combination of Seismic Refraction and Marine Surface Wave to Characterize Near Surface Marine Sediments." In Near Surface Geoscience 2014 - First Applied Shallow Marine Geophysics Conference. Netherlands: EAGE Publications BV, 2014. http://dx.doi.org/10.3997/2214-4609.20142135.

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Tsourlos, P. I., G. A. Tassis, and J. S. Rønning. "Marine ERT Modelling for the Detection of Fracture Zones." In Near Surface Geoscience 2013. Netherlands: EAGE Publications BV, 2013. http://dx.doi.org/10.3997/2214-4609.20131398.

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Biriukov, E. A., M. U. Tokarev, and V. V. Ivanova. "The Latest Trends in Near-Surface Marine Seismic Survey (2D, 3D)." In Marine Technologies 2019. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201901823.

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Ruman, Md Raseduzzaman, Mukta Das, S. M. Istiaque Mahmud, and Shantanu Kumar Nath. "Automated Marine Surface Trash Cleaner." In 2019 IEEE 5th International Conference for Convergence in Technology (I2CT). IEEE, 2019. http://dx.doi.org/10.1109/i2ct45611.2019.9033828.

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Nelson, T. "The Potential for Surface Disruption Techniques in the Aesthetic Evolution of Superyachts." In Marine Design 2014. RINA, 2014. http://dx.doi.org/10.3940/rina.md.2014.19.

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Ingerov, I. "Shallow marine EM surveys." In Near-Surface Asia Pacific Conference, Waikoloa, Hawaii, 7-10 July 2015. Society of Exploration Geophysicists, Australian Society of Exploration Geophysicists, Chinese Geophysical Society, Korean Society of Earth and Exploration Geophysicists, and Society of Exploration Geophysicists of Japan, 2015. http://dx.doi.org/10.1190/nsapc2015-100.

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Pageot, D., D. Leparoux, Y. Capdeville, and P. Côte. "Alternative Surface Wave Analysis Method for 2D Near-Surface maging Using Particle Swarm Optimization." In 3rd Applied Shallow Marine Geophysics Conference. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201802679.

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DURKIN, J., and N. PARASKEVAS. "Progress in the development of the surface effect catamaran (SECAT)." In Advanced Marine Systems Conference. Reston, Virigina: American Institute of Aeronautics and Astronautics, 1986. http://dx.doi.org/10.2514/6.1986-2364.

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Reports on the topic "Surface marine"

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Edson, James B. Spectral Characteristics of the Marine Surface Layer. Fort Belvoir, VA: Defense Technical Information Center, April 2000. http://dx.doi.org/10.21236/ada376029.

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Edson, James B. Spectral Characteristics of the Marine Surface Layer. Fort Belvoir, VA: Defense Technical Information Center, September 1997. http://dx.doi.org/10.21236/ada634715.

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Sullivan, Peter P., James C. McWilliams, and Chin-Hoh Moeng. Surface Gravity Waves and Coupled Marine Boundary Layers. Fort Belvoir, VA: Defense Technical Information Center, September 2001. http://dx.doi.org/10.21236/ada625363.

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Sullivan, Peter P., and James C. McWilliams. Turbulent Flow and Large Surface Wave Events in the Marine Boundary Layers. Fort Belvoir, VA: Defense Technical Information Center, September 2008. http://dx.doi.org/10.21236/ada495358.

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Sullivan, Peter P., and James C. McWilliams. Turbulent Flow and Large Surface Wave Events in the Marine Boundary Layers. Fort Belvoir, VA: Defense Technical Information Center, September 2012. http://dx.doi.org/10.21236/ada590522.

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Sullivan, Peter P., and James C. McWilliams. Turbulent Flow and Large Surface Wave Events in the Marine Boundary Layers. Fort Belvoir, VA: Defense Technical Information Center, September 2007. http://dx.doi.org/10.21236/ada573094.

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Lewis, Marlon R., and John J. Cullen. Variability in Surface Reflectance and the Attenuation of Solar Radiation in Coastal Marine Waters. Fort Belvoir, VA: Defense Technical Information Center, August 2002. http://dx.doi.org/10.21236/ada626519.

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Blough, Neil V. In Situ and Laboratory Measurements of the Optical and Photochemical Properties of Surface Marine Waters. Fort Belvoir, VA: Defense Technical Information Center, August 2001. http://dx.doi.org/10.21236/ada626252.

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Fairall, C. W., and R. J. Hill. Similarity in the Marine Atmospheric Surface Layer: The Role of Intermittency and Boundary-Layer Structures. Fort Belvoir, VA: Defense Technical Information Center, September 1997. http://dx.doi.org/10.21236/ada629306.

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Reynolds, R. Michael, and Charles N. Long. Marine ARM GPCI Investigation of Clouds Infrared Sea Surface Temperature Autonomous Radiometer (ISAR) Field Campaign Report. Office of Scientific and Technical Information (OSTI), January 2016. http://dx.doi.org/10.2172/1328010.

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