Gotowe bibliografie tematyczne / Tidal dynamics

Gotowa bibliografia na temat „Tidal dynamics”

Autor: Grafiati
Data publikacji: 4 czerwca 2021
Data aktualizacji: 20 lutego 2023

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Artykuły w czasopismach na temat "Tidal dynamics"

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Charlier, Roger H. "Tidal Dynamics". International Journal of Environmental Studies 67, nr 3 (czerwiec 2010): 466–67. http://dx.doi.org/10.1080/00207230601124740.

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Вольцингер, Наум Евсеевич, i Алексей Анатольевич Андросов. "Extreme nonhydrostatic tidal dynamics". Вычислительные технологии, nr 2(24) (17.04.2019): 37–51. http://dx.doi.org/10.25743/ict.2019.24.2.004.

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Моделирование длинноволновых океанологических процессов традиционно выполняется в гидростатическом (Гс) приближении, обеспечивающем высокую точность расчета гидрофизических полей, когда вертикальным ускорением движения можно пренебречь. На горном рельефе это не так, и учет динамической компоненты давления становится необходимым. Негидростатическое (Нг) моделирование крупномасштабных океанологических явлений реализуется решением 3D краевой гидродинамической задачи. Структуру метода составляют этапы решения Гс-задачи, краевой задачи для уравнения Пуассона (Нг) и коррекции полей гидрофизических характеристик. Значимость Нг-фактора выявляется при рассмотрении безразмерного вида уравнений, когда безразмерные параметры характеризуют горный рельеф области. Случай резких изменений рельефа, требующий решения Нг-задачи, - пролив Ломбок. Приводятся оценки Нг-фактора в водообмене между океанами, результаты сравнения спектров вертикальной скорости в Гс- и Нг-постановках. Modelling of long-wave oceanological processes is traditionally performed in a hydrostatic (Hs) approximation, which ensures high accuracy of the calculation of hydrophysical fields, when the vertical acceleration of vertical motion can be neglected. In mountainous terrain, this is not the case, and consideration of the dynamic pressure component becomes necessary. Non-hydrostatic (Nh) modelling of large-scale oceanological phenomena is implemented by solving hydrodynamic boundary value problem in an arbitrary 3D domain. The structure of the method consists of the stages of solving the Hs problem, the boundary value problem for the Poisson equation (Nh), and the correction of the fields of hydrophysical characteristics. That is the pressure is presented as a sum of its hydrostatic and dynamical components. Significance of Nh is revealed when considering the dimensionless type of equations, when dimensionless parameters characterize the mountain relief of the region. The Lombok Strait having a complex morphometric structure is an important link in the water exchange between the Pacific and Indian Oceans, it has been chosen as the object for modelling. Estimates of the role of Nh in water exchange between the oceans are given using the comparison of the solution for problems in Hs and Nh sets. It indicates the need to take into account Nh in conditions of pronounced sea mountain relief.
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Chicone, C., i B. Mashhoon. "Tidal dynamics in Kerr spacetime". Classical and Quantum Gravity 23, nr 12 (17.05.2006): 4021–33. http://dx.doi.org/10.1088/0264-9381/23/12/002.

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Mashhoon, Bahram, Nader Mobed i Dinesh Singh. "Tidal dynamics in cosmological spacetimes". Classical and Quantum Gravity 24, nr 20 (2.10.2007): 5031–46. http://dx.doi.org/10.1088/0264-9381/24/20/008.

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Fabrycky, Daniel C. "Tidal dynamics of transiting exoplanets". Proceedings of the International Astronomical Union 6, S276 (październik 2010): 252–57. http://dx.doi.org/10.1017/s1743921311020278.

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AbstractTransits give us the mass, radius, and orbital properties of the planet, all of which inform dynamical theories. Two properties of the hot Jupiters suggest they had a dramatic origin via tidal damping from high eccentricity. First, the tidally circularized planets (in the 1-4 day pile-up) lie along a relation or boundary in the mass-period plane. This observation may implicate a tidal damping process regulated by planetary radius inflation and Roche lobe overflow, early in the planets' lives. Second, the host stars of many planets have spins misaligned from the planets' orbits. This observation was not expected a priori from the conventional disk migration theory, and it was a boon for the alternative theories of planet-planet scattering and Kozai cycles, accompanied by tidal friction, which predicted it. Now we are faced with a curious observation that the misalignment angle depends on the stellar temperature. It may mean that the tide raised on the stars realigns them, the final result being the tidal consumption of hot Jupiters.
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Bakker, C. "Tidal mixing and plankton dynamics". Aquatic Botany 31, nr 3-4 (sierpień 1988): 380–82. http://dx.doi.org/10.1016/0304-3770(88)90031-9.

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Anderson, Christopher J., i B. Graeme Lockaby. "Foliar nutrient dynamics in tidal and non-tidal freshwater forested wetlands". Aquatic Botany 95, nr 2 (sierpień 2011): 153–60. http://dx.doi.org/10.1016/j.aquabot.2011.05.010.

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Cardone, G., A. Fouetio, S. Talla Lando i J. L. Woukeng. "Global dynamics of stochastic tidal equations". Nonlinear Analysis 225 (grudzień 2022): 113137. http://dx.doi.org/10.1016/j.na.2022.113137.

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Hoitink, A. J. F., i D. A. Jay. "Tidal river dynamics: Implications for deltas". Reviews of Geophysics 54, nr 1 (marzec 2016): 240–72. http://dx.doi.org/10.1002/2015rg000507.

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Battiston, L., i D. Zambella. "Noise-driven intermittency in tidal dynamics". Il Nuovo Cimento D 14, nr 12 (grudzień 1992): 1255–71. http://dx.doi.org/10.1007/bf02456782.

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Rozprawy doktorskie na temat "Tidal dynamics"

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Teo, Hhih-Ting, i h. teo@griffith edu au. "Tidal Dynamics in Coastal Aquifers". Griffith University. School of Engineering, 2003. http://www4.gu.edu.au:8080/adt-root/public/adt-QGU20030729.155028.

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The prediction of coastal groundwater movement is necessary in coastal management. However, the study in this field is still a great challenge due to the involvement of tidal-groundwater interactions and the phenomena of hydrodynamic dispersion between salt-fresh water in the coastal region. To date, numerous theories for groundwater dynamic have been made available in analytical, numerical and also experimental forms. Nevertheless, most of them are based on the zeroth-order shallow flow, i.e. Boussinesq approximation. Two main components for coastal unconfined aquifer have been completed in this Thesis: the vertical beach model and the sloping beach model. Both solutions are solved in closed-form up to higher order with shallow water parameter ([epsilon]) and tidal amplitude parameter ([alpha]). The vertical beach solution contributes to the higher-order tidal fluctuations while the sloping beach model overcomes the shortcomings in the existing solutions. From this study, higher-order components are found to be significant especially for larger value of [alpha] and [epsilon]. Other parameters such as hydraulic conductivity (K) and the thickness of aquifer (D) also affect the water table fluctuations. The new sloping solution demonstrated the significant influence of beach slope ([beta]) on the water table fluctuations. A comprehensive comparison between previous solution and the present sloping solution have been performed mathematically and numerically and the present solution has been demonstrated to provide a better prediction
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Teo, Hhih-Ting. "Tidal Dynamics in Coastal Aquifers". Thesis, Griffith University, 2003. http://hdl.handle.net/10072/365678.

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The prediction of coastal groundwater movement is necessary in coastal management. However, the study in this field is still a great challenge due to the involvement of tidal-groundwater interactions and the phenomena of hydrodynamic dispersion between salt-fresh water in the coastal region. To date, numerous theories for groundwater dynamic have been made available in analytical, numerical and also experimental forms. Nevertheless, most of them are based on the zeroth-order shallow flow, i.e. Boussinesq approximation. Two main components for coastal unconfined aquifer have been completed in this Thesis: the vertical beach model and the sloping beach model. Both solutions are solved in closed-form up to higher order with shallow water parameter ([epsilon]) and tidal amplitude parameter ([alpha]). The vertical beach solution contributes to the higher-order tidal fluctuations while the sloping beach model overcomes the shortcomings in the existing solutions. From this study, higher-order components are found to be significant especially for larger value of [alpha] and [epsilon]. Other parameters such as hydraulic conductivity (K) and the thickness of aquifer (D) also affect the water table fluctuations. The new sloping solution demonstrated the significant influence of beach slope ([beta]) on the water table fluctuations. A comprehensive comparison between previous solution and the present sloping solution have been performed mathematically and numerically and the present solution has been demonstrated to provide a better prediction
Thesis (Masters)
Master of Philosophy (MPhil)
School of Engineering
Full Text
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O'Callaghan, Joanne M. "Tidal and sediment dynamics of a partially mixed, micro-tidal estuary". University of Western Australia. Centre for Water Research, 2005. http://theses.library.uwa.edu.au/adt-WU2005.0088.

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[Truncated abstract] The expansion of human populations in coastal land margins has resulted in major modifcations to estuarine ecosystems. The use of numerical models as predictive tools for assessing remediation strategies is increasing. However, parameterisation of physical processes, developed mainly through field investigations, is necessary for these models to be reliable and effective management tools. The physical processes in micro–tidal diurnal tidal systems are relatively unknown and the current study examines field measurements obtained from the upper Swan River estuary (Western Australia), a diurnal, partially mixed system during the summer when the freshwater discharge is negligible. The aims of the study were to characterise, temporally and spatially, the dominant physical processes and associated sediment resuspension. Variability at three dominant time-scales were examined: 1) sub–tidal oscillations (∼5 to 10 days) resulting from local and remote forcing; 2) tidal (∼ 24 hours) due to astronomical forcing; and 3) intra-tidal (∼2 to 3 hours) resulting from the interaction between tidal constituents. Circulation in estuaries is widely accepted in the literature to be dominated, in varying proportions, by tidal range, freshwater discharge and gravitational circulation. In the upper Swan River estuary sub–tidal oscillations were responsible for the largest upstream displacement of the salt wedge in the absence of freshwater discharge. Moreover, these sub–tidal fluctuations in water level modified the ‘classic’ estuarine circulation. The dynamics of diurnal tides are largely controlled by the tropic month, which oscillates at a slightly different period to the lunar month, resulting in the spring–neap tidal cycle to be sometimes different from syzygy. The phase lag between the diurnal (O1 + K1) and semi-diurnal (M2 + S2) constituents, at the seasonal time scale cause the maximum tidal range to be near the solstice. Over a 24–hour tidal cycle this phase lag is manifested as an intra–tidal oscillation that occurs on the flood tide. Turbidity events that last ∼1 to 2 hours occur during the intra–tidal oscillation, but are not related to maximum shear stress predicted from the mean flow characteristics. The increases in turbidity during the intra–tidal oscillation is, however, correlated with the near–bed Reynolds fluxes. During the intra–tidal oscillation advection opposes the estuarine circulation in the near–bed region, promoting vertical shear that results in destratifcation of the water column. The turbulent mixing generated at the interface and in the near–bed region coincide with resuspension events. Similar turbidity data have often been disregarded and documented as being ‘spikes’ based on the premise that the mean flow was below a critical level to resuspend sediment. Resuspension events were not simply related to mean processes and may be controlled by turbulent instabilities generated when tidal currents reverse during an intra-tidal oscillation
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Coelho, Emanuel Ferreira. "Tidal dynamics and mixing over steep topography". Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 1994. http://handle.dtic.mil/100.2/ADA283535.

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Herman, W. M. "Wave dynamics in a macro-tidal estuary". Thesis, University of Cambridge, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.603976.

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This study explores field and numerically modelled datasets on wave and wave-driven processes within the macro-tidal Blackwater Estuary in Essex, U.K. The wave climate of the Blackwater Estuary was characterised from wave records collected from 1994 to 1996 at 5 monitoring stations within the estuary. From these records and hindcasted offshore wave records over this period, locally-generated wind waves, wind-sea, and swell waves were identified and their significance assessed in terms of probability of occurrence and variability in different sections of the estuary. The Blackwater Estuary is found to be subject to waves from both offshore and from within the estuary, with evidence of seasonality within these wave climates. Longer-term wave and tidal height distributions were predicted through a Weibull probability model and their joint probability established for different return intervals. A numerical wave model (MWAVE_REG) was used to quantify the temporal and spatial impact of a variety of hydrodynamic scenarios (including 'worst case') within the Blackwater Estuary. The effects of wave diffraction, reflection and refraction were evaluated and areas of wave focusing within the estuary identified. The model was subsequently used to predict morphological changes per 1km shoreline, linking modelled hydrodynamics to observed morphological changes. The significance of the distribution of wave energy within the estuary for sediment entrainment, transport and deposition is discussed. In order to modify the highly artificial estuarine system of the Blackwater, a number of potential managed realignment sites were identified. From the hydrodynamic and morphodynamic findings of this study; these may aid in the reaction of a more natural estuarine system, better able to absorb extreme water local events.
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Pritchard, Mark. "Dynamics of a small tidal estuarine plume". Thesis, University of Plymouth, 2000. http://hdl.handle.net/10026.1/844.

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Small-scale estuarine plume discharges into adjacent seas are common inshore features responsible for the transportation and dispersion of brackish water in the coastal zone. However, the physics that govern small-scale mixing in the frontal regions of river plumes are still poorly understood. The current study quantified and compared the observed hydrodynamic properties present inside a radially spreading river plume discharge from the River Teign, Teignmouth, Devon, UK, to those predicted by a generic plume model. Numerical simulations designed to replicate time dependent radial plume spreading from a constant source predicted the development of an internal interfacial bore that lagged the surface plume front through radial distance and time from initial plume release. The model was scaled from time lapse X-band radar imagery that recorded several plume discharge events. Scaled model output predicted the internal bore to form approximately 180 m behind the leading surface front. Subsequent field studies employed instrumentation capable of recording high-resolution measurements of temperature, salinity and velocity, spatially and vertically throughout the plume's buoyant layer over two ebb tidal cycles. Results suggested the plume advanced at a rate dependent on a super-critical interfacial Froude number of O(1.3) and was a region of intense mixing and downward mass entrainment. Temperature contours recorded through the stratified plume gave no indication of an internal bore in its predicted position but did show an abrupt shallowing of the interfacial region some 40 to 60 m behind the surface plume front. Super-critical interfacial Froude and critical Gradient Richardson numbers present in this region of the plume implied that this was the position of the predicted bore. The form of the bore often appeared as an ensemble of undular internal hydraulic jumps rather than a singular discontinuity as predicted by the model. Bulk mixing analysis inside the leading front based on established gravity current theory suggested that the extent of turbulent exchange in the model frontal boundary condition P, was underestimated by about a factor of 2. With the required increase in P, model simulations showed a decrease in the lag distance of internal bore formation to one where critical Froude numbers were detected inside the actual plume. Throughout both surveys, the gravity head remained a reasonably constant size due to any increase in across frontal velocity over the ebb tidal cycle being matched by an increase in entrainment and mixing. The subsequent conclusions from the study show the outflow and mixing dynamics are controlled by the estuary's tidal modulation of estuarine brackish water outflow / plume inflow rate behind the leading plume frontal discontinuity.
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Gao, Shu. "Sediment dynamics and stability of tidal inlets". Thesis, University of Southampton, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.387108.

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Signell, Richard P. "Tidal dynamics and dispersion around coastal headlands". Thesis, Massachusetts Institute of Technology, 1989. http://hdl.handle.net/1721.1/57928.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 1989.
Includes bibliographical references (leaves 160-162).
by Richard Peter Signell.
Ph.D.
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Neubauer, Scott C. "Carbon dynamics in a tidal freshwater marsh". W&M ScholarWorks, 2000. https://scholarworks.wm.edu/etd/1539616793.

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The sources and fates of carbon in a tidal freshwater marsh (Sweet Hall marsh; Pamunkey River, Virginia) were determined to understand the role that these marshes play with respect to estuarine carbon cycling. A carbon gas flux model, based on measured carbon dioxide and methane fluxes, was developed to calculate annual rates of macrophyte and microalgal photosynthesis and community and belowground respiration. Because carbon fluxes out of marsh sediments may underestimate true belowground respiration if sediment-produced gases are transported through plant tissues, gross nitrogen mineralization was used as a proxy for belowground carbon respiration. Annual community respiration exceeded gross photosynthesis, suggesting an allochthonous input of organic carbon to the marsh. Sediment deposition during tidal flooding was measured as a potential exogenous carbon source. Short term deposition rates (biweekly to monthly) were spatially and temporally variable, with highest rates measured near a tidal creek during summer. Annual deposition on the marsh was sufficient to balance relative sea level rise and measured respiration rates. Sediment inventories of 7Be indicated that spatial patterns of sedimentation were not due to sediment redistribution within the marsh. Accretion rates calculated from 137Cs (decadal scale) and 14C (centuries to millennia) were substantially less than annual deposition rates. The concentration and isotopic composition of dissolved and particulate inorganic and organic carbon (DIC, DOC, POC) were measured in a marsh creek which drained the study site. Seasonal isotopic variations in DIC were explained by marsh porewater drainage and decomposition of marsh-derived carbon. A model linking DIC concentrations and water transport showed that DIC export from tidal marshes could explain a significant portion of excess DIC production in the adjacent estuary. Isotopic mixing models indicated seasonal variability in the importance of phytoplankton as a source of DOC and POC although there was no evidence for a net flux of these materials between the marsh and estuary. Annually, the marsh carbon budget was closely balanced, with sources exceeding sinks by approximately 5 percent. This similarity suggests that those processes which were not quantified (e.g. consumption by marsh and riverine fauna) were quantitatively unimportant with respect to the entire marsh carbon budget.
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Schostak, Laura Elizabeth. "Dynamics of a high-macrotidal saltmarsh tidal creek". Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk2/tape15/PQDD_0026/MQ33270.pdf.

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Książki na temat "Tidal dynamics"

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Wood, Fergus J. Tidal dynamics. Wyd. 3. West Palm Beach: Coastal Education & research Foundation, 2001.

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International Conference on Tidal Dynamics and Environment (2002 Hangzhou, China). Tidal dynamics and environment. Lawrence, Kansas: Coastal Education and Research Foundation, 2004.

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Bowman, Malcolm J., Clarice M. Yentsch i William T. Peterson, red. Tidal Mixing and Plankton Dynamics. New York, NY: Springer New York, 1986. http://dx.doi.org/10.1007/978-1-4612-4966-5.

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1926-, Bowman Malcolm J., Yentsch Clarice M i Peterson William Thornton, red. Tidal mixing and plankton dynamics. Berlin: Springer-Verlag, 1986.

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Signell, Richard Peter. Tidal dynamics and dispersion around coastal headlands: Doctoral dissertation. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1989.

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Aubrey, David G., i Lee Weishar, red. Hydrodynamics and Sediment Dynamics of Tidal Inlets. Washington, D. C.: American Geophysical Union, 1988. http://dx.doi.org/10.1029/ln029.

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Aubrey, David G., i Lee Weishar, red. Hydrodynamics and Sediment Dynamics of Tidal Inlets. New York, NY: Springer New York, 1988. http://dx.doi.org/10.1007/978-1-4757-4057-8.

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G, Aubrey David, Weishar Lee i International Symposium on Hydrodynamics and Sediment Dynamics of Tidal Inlets (1986 : Woods Hole, Mass.), red. Hydrodynamics and sediment dynamics of tidal inlets. New York: Springer-Verlag, 1988.

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Friedrichs, Carl T. Pressure/Temperature Logger (PTL), development and field deployment for the Great Bay, NH, tidal dynamics experiment. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1998.

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Ballegooyen, R. C. Van. Dynamics relevant to modelling tidal and subtidal circulation in False Bay. Stellenbosch, South Africa: Marine Pollution Programme, Division of Earth, Marine and Atmospheric Science and Technology, CSIR, 1990.

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Części książek na temat "Tidal dynamics"

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Rimrott, Fred P. J. "Tidal Forces". W Introductory Orbit Dynamics, 160–64. Wiesbaden: Vieweg+Teubner Verlag, 1989. http://dx.doi.org/10.1007/978-3-322-90338-9_13.

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Sharma, Ishan. "Tidal Flybys". W Shapes and Dynamics of Granular Minor Planets, 307–35. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-40490-5_12.

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Stockton, A. "The QSO-Tidal Connection". W Dynamics and Interactions of Galaxies, 440–49. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-75273-5_113.

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Seitzer, P. "Tidal Effects on Globular Clusters". W Dynamics of Star Clusters, 343–46. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5335-2_42.

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Baba, Eiichi, Hideo Kawarada, Wataru Nishijima, Mitsumasa Okada i Hiroshi Suito. "Breaking waves and ecosystem dynamics". W Waves and Tidal Flat Ecosystems, 117–26. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-642-55534-3_8.

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Borne, K. D. "Tidal Phenomena in Interacting Galaxies". W Dynamics and Interactions of Galaxies, 196–99. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-75273-5_45.

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McGlynn, T. A. "Remnants of Strong Tidal Interactions". W Dynamics and Interactions of Galaxies, 225–26. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-75273-5_54.

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van de Kreeke, J. "Hydrodynamics of Tidal Inlets". W Hydrodynamics and Sediment Dynamics of Tidal Inlets, 1–23. New York, NY: Springer New York, 1988. http://dx.doi.org/10.1007/978-1-4757-4057-8_1.

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van de Kreeke, J. "Hydrodynamics of tidal inlets". W Hydrodynamics and Sediment Dynamics of Tidal Inlets, 1–23. Washington, D. C.: American Geophysical Union, 1988. http://dx.doi.org/10.1029/ln029p0001.

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Mann, K. H., i J. R. N. Lazier. "Tides, Tidal Mixing, and Internal Waves". W Dynamics of Marine Ecosystems, 254–84. Malden, MA USA: Blackwell Publishing Ltd., 2013. http://dx.doi.org/10.1002/9781118687901.ch7.

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Streszczenia konferencji na temat "Tidal dynamics"

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Hibma, Anneke, i Jacobus van de Kreeke. "Tidal Variations in Sand Concentrations in the Frisian Inlet". W Fourth Conference on Coastal Dynamics. Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40566(260)46.

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Sherwood, Christopher R., Guy Gelfenbaum, Peter A. Howd i Margaret L. Palmsten. "Sediment Transport on a High-Energy Ebb-Tidal Delta". W Fourth Conference on Coastal Dynamics. Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40566(260)48.

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Yang, Zizang, i Richard Patchen. "Nonlinear Tidal Dynamics in Florida Coastal Waters". W International Conference on Estuarine and Coastal Modeling 2012. Reston, VA: American Society of Civil Engineers, 2012. http://dx.doi.org/10.1061/9780784412411.00001.

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Ladage, Florian, Hans-Joachim Stephan i Hanz Dieter Niemeyer. "Interactions of Large-Scale Groyne and Tidal Inlet Migration". W Fifth International Conference on Coastal Dynamics. Reston, VA: American Society of Civil Engineers, 2006. http://dx.doi.org/10.1061/40855(214)111.

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Uchiyama, Yusuke, Yoshiaki Kuriyama i Kazumasa Katoh. "Suspended Sediment and Morphological Response on Banzu Tidal Flat, Japan". W Fourth Conference on Coastal Dynamics. Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40566(260)106.

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Eelkema, M., Z. B. Wang i M. J. F. Stive. "85. Historical morphological development of the Eastern Scheldt tidal basin (The Netherlands)". W Coastal Dynamics 2009 - Impacts of Human Activities on Dynamic Coastal Processes. WORLD SCIENTIFIC, 2009. http://dx.doi.org/10.1142/9789814282475_0087.

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Stive, Marcel J. F., J. van de Kreeke, Nghiem T. Lam, Tran T. Tung i Roshanka Ranasinghe. "96. EMPIRICAL RELATIONSHIPS BETWEEN INLET CROSS-SECTION AND TIDAL PRISM: A REVIEW". W Coastal Dynamics 2009 - Impacts of Human Activities on Dynamic Coastal Processes. WORLD SCIENTIFIC, 2009. http://dx.doi.org/10.1142/9789814282475_0098.

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Xu, Jiangtao, i Edward Myers. "Modeling Tidal Dynamics and Tidal Datums along the Coasts of Texas and Western Louisiana". W 11th International Conference on Estuarine and Coastal Modeling. Reston, VA: American Society of Civil Engineers, 2010. http://dx.doi.org/10.1061/41121(388)30.

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Militello, Adele, i Nicholas C. Kraus. "Re-Alignment of an Inlet Entrance Channel by Ebb-Tidal Eddies". W Fourth Conference on Coastal Dynamics. Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40566(260)43.

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Mason, Travis, i Michael B. Collins. "Nearshore Currents on a Macro-Tidal, Mixed (Sand and Shingle) Beach". W Fourth Conference on Coastal Dynamics. Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40566(260)55.

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Raporty organizacyjne na temat "Tidal dynamics"

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Fagherazzi, Sergio. Tidal Channel Dynamics and Muddy Substrates: A Comparison between a Wave Dominated and a Tidal Dominated System. Fort Belvoir, VA: Defense Technical Information Center, wrzesień 2012. http://dx.doi.org/10.21236/ada572756.

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Fagherazzi, Sergio. Tidal Channel Dynamics and Muddy Substrates: a Comparison Between a Wave Dominated and a Tidal Dominated System. Fort Belvoir, VA: Defense Technical Information Center, wrzesień 2011. http://dx.doi.org/10.21236/ada557157.

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Fritts, D. C. Gravity Wave Dynamics and Tidal Interactions in the MLT and at the Bottomside F Layer and Their Potential Contributions to Neutral and Plasma Dynamics. Fort Belvoir, VA: Defense Technical Information Center, kwiecień 2012. http://dx.doi.org/10.21236/ada559865.

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Traykovski, Peter A., i W. R. Geyer. Multi-Scale (cm to km) Hydrodynamic and Morphologic Interactions in Tidal Inlets, Dynamics of Sandwaves with Combined Wave - Current Forcing and Mine Burial Processes, and Instrumentation for Measuring Nearshore Morphologic Change and Hydrodynamic Forcing. Fort Belvoir, VA: Defense Technical Information Center, wrzesień 2011. http://dx.doi.org/10.21236/ada557178.

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Brodie, Katherine, Ian Conery, Nicholas Cohn, Nicholas Spore i Margaret Palmsten. Spatial variability of coastal foredune evolution, part A : timescales of months to years. Engineer Research and Development Center (U.S.), lipiec 2021. http://dx.doi.org/10.21079/11681/41322.

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Streszczenie:
Coastal foredunes are topographically high features that can reduce vulnerability to storm-related flooding hazards. While the dominant aeolian, hydrodynamic, and ecological processes leading to dune growth and erosion are fairly well-understood, predictive capabilities of spatial variations in dune evolution on management and engineering timescales (days to years) remain relatively poor. In this work, monthly high-resolution terrestrial lidar scans were used to quantify topographic and vegetation changes over a 2.5 year period along a micro-tidal intermediate beach and dune. Three-dimensional topographic changes to the coastal landscape were used to investigate the relative importance of environmental, ecological, and morphological factors in controlling spatial and temporal variability in foredune growth patterns at two 50 m alongshore stretches of coast. Despite being separated by only 700 m in the alongshore, the two sites evolved differently over the study period. The northern dune retreated landward and lost volume, whereas the southern dune prograded and vertically accreted. The largest differences in dune response between the two sections of dunes occurred during the fall storm season, when each of the systems’ geomorphic and ecological properties modulated dune growth patterns. These findings highlight the complex eco-morphodynamic feedback controlling dune dynamics across a range of spatial scales.
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Candela, Julio. Dynamic Response of a Semi-Enclosed Sea to Atmospheric and Tidal Forcing. Fort Belvoir, VA: Defense Technical Information Center, lipiec 1997. http://dx.doi.org/10.21236/ada327670.

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Wave climate and sediment dynamics in the tidal flats and marshes of Galgeschoor: Synthesis report. Instituut voor Natuur- en Bosonderzoek, 2019. http://dx.doi.org/10.21436/inbor.17169167.

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Nitrogen dynamics in the tidal freshwater Potomac River, Maryland and Virginia, water years 1979-81. US Geological Survey, 1989. http://dx.doi.org/10.3133/wsp2234j.

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Phytoplankton dynamics of the fresh, tidal Potomac River, Maryland, for the summers of 1979 to 1981. US Geological Survey, 1988. http://dx.doi.org/10.3133/wsp2234c.

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