Relevant bibliographies by topics / Macrotidal

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

Academic literature on the topic 'Macrotidal'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 June 2024

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Journal articles on the topic "Macrotidal"

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Mitchell, S. B. "Turbidity maxima in four macrotidal estuaries." Ocean & Coastal Management 79 (July 2013): 62–69. http://dx.doi.org/10.1016/j.ocecoaman.2012.05.030.

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Araújo, Wilton Pires, and Nils E. Asp. "Hydrodynamic connectivity between two macrotidal Amazonian estuaries." Journal of Coastal Research 165 (January 3, 2013): 1086–91. http://dx.doi.org/10.2112/si65-184.1.

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Lessa, Guilherme, and Gerhard Masselink. "Morphodynamic evolution of a macrotidal barrier estuary." Marine Geology 129, no. 1-2 (1995): 25–46. http://dx.doi.org/10.1016/0025-3227(95)00103-4.

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Cariolet, J. M., and S. Suanez. "Runup estimations on a macrotidal sandy beach." Coastal Engineering 74 (April 2013): 11–18. http://dx.doi.org/10.1016/j.coastaleng.2012.11.008.

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Yang, Mengmeng, Joaquim I. Goes, Hongzhen Tian, Elígio de R. Maúre, and Joji Ishizaka. "Effects of Spring–Neap Tidal Cycle on Spatial and Temporal Variability of Satellite Chlorophyll-A in a Macrotidal Embayment, Ariake Sea, Japan." Remote Sensing 12, no. 11 (2020): 1859. http://dx.doi.org/10.3390/rs12111859.

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We investigated the spatio-temporal variability of chlorophyll-a (Chl-a) and total suspended matter (TSM) associated with spring–neap tidal cycles in the Ariake Sea, Japan. Our study relied on significantly improved, regionally-tuned datasets derived from the ocean color sensor Moderate Resolution Imaging Spectroradiometer (MODIS) Aqua over a 16-year period (2002–2017). The results revealed that spring–neap tidal variations in Chl-a and TSM within this macrotidal embayment (the Ariake Sea) are clearly different regionally and seasonally. Generally, the spring–neap tidal variability of Chl-a in the inner part of the Ariake Sea was controlled by TSM for seasons other than summer, whereas it was controlled by river discharge for summer. On the other hand, the contribution of TSM to the variability of Chl-a was not large for two areas in the middle of Ariake Sea where TSM was not abundant. This study demonstrates that ocean color satellite observations of Chl-a and TSM in the macrotidal embayment offer strong advantages for understanding the variations during the spring–neap tidal cycle.
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Moskalski, Susanne, France Floc'h, and Romaric Verney. "Suspended sediment fluxes in a shallow macrotidal estuary." Marine Geology 419 (January 2020): 106050. http://dx.doi.org/10.1016/j.margeo.2019.106050.

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Scott, Tim, Gerd Masselink, Martin J. Austin, and Paul Russell. "Controls on macrotidal rip current circulation and hazard." Geomorphology 214 (June 2014): 198–215. http://dx.doi.org/10.1016/j.geomorph.2014.02.005.

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Thomas, T., M. R. Phillips, A. T. Williams, and R. E. Jenkins. "Rotation on two adjacent open coast macrotidal beaches." Applied Geography 35, no. 1-2 (2012): 363–76. http://dx.doi.org/10.1016/j.apgeog.2012.08.010.

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Miles, Jon, Antony Thorpe, Paul Russell, and Gerd Masselink. "Observations of bedforms on a dissipative macrotidal beach." Ocean Dynamics 64, no. 2 (2014): 225–39. http://dx.doi.org/10.1007/s10236-013-0677-2.

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Bonte, Yoann, and Franck Levoy. "MORPHODYNAMIC OF BEACH SCARPS ON A MACROTIDAL COAST DURING EXCEPTIONAL WATER LEVEL EVENTS (NORMANDY, FRANCE)." Coastal Engineering Proceedings 1, no. 33 (2012): 11. http://dx.doi.org/10.9753/icce.v33.posters.11.

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Although there are numerous studies on the morphology and physical processes affecting the dune's scarp and many conceptual models describing beach scarps on microtidal and mesotidal environments (Sunamura, 1985a ; Short,1999), really quantitative informations about the beach scarp formation is lacking, especially along tidal environments where the tide controls the level of wave attack. However, Sherman and Nordstrom(1985) give a qualitative description of beach scarp formations and evolution based on field observations but without data set. The coast of Calvados (Normandy, France) is a fine example of a macrotidal coast, where beach scarps have been often observed. Along macrotidal beaches, the formation of a berm is classically observed during fair weather conditions which contribute to stabilize the coastline. During stormy conditions, the low atmosphere pressure, short waves and onshore winds cause an increase of the water level, which during spring tides, increases the high tide water level time action. Consequently, the natural berm protecting the dune foot, or sometimes a seawall foot, is threatened by erosion and often destroyed. The goal of this study is to quantify the beach scarp destruction (foot and crest scarp retreat speed, eroded volume...) in relation with the hydraulic and morphologic local conditions.
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Dissertations / Theses on the topic "Macrotidal"

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Poate, Timothy George. "Morphological response of high-energy macrotidal beaches." Thesis, University of Plymouth, 2012. http://hdl.handle.net/10026.1/1094.

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Spatial data collected over 3 years is presented to assess the extent of morphological variability under seasonal and storm waves at four high-energy macrotidal beaches. A novel approach is adopted to identify and classify the beach response which is used to assess the relative stability of the system to changes in the dominant forcing conditions. Field measurements and modelling simulations using XBeach provide further support for a storm dominated system exhibiting relative stability. Morphologically the beaches range from dissipative to intermediate and are characterised by low tide bar/rip morphology which plays a key role in the nearshore dynamics and beach safety. Located in the north coast of Cornwall the sites are exposed to high-energy waves that dominate the stability and behaviour of beaches in this region. The growing need for marine renewable energy in the UK has led to the deployment of a Wave Hub on the seabed off the north coast of Cornwall, designed to provide grid connection for wave energy devices (WECs). As a unique development much has been done to address concerns over potential impacts cause by arrays of WECs during its construction and operational lifetime; these predicted impacts include changes in the quality of waves for surfing and effects on the beach dynamics which determines beach safety through the presence of bar/rip features. In this thesis three years of monthly topographic surveys were collected from beaches in the proposed Wave Hub shadow zone to assess their morphodynamic variability. Realtime kinematic (RTK) GPS surveys were undertaken using an all-terrain vehicle to measure the three dimensional (3D) morphology at four beaches (Perranporth, Chapel Porth, Porthtowan and Gwithian) situated along a 23 km stretch of the north Cornish coast. In addition nearshore wave data, in-situ hydrodynamic measurements, local tide gauges and Argus video data allowed detailed analysis of process-response mechanisms for long term (yearly); seasonal (monthly); storm (weekly/daily); and tidal (hourly) morphological behaviour. Of particular interest was the degree to which the beaches displayed bar/rip morphology, characterised by the three dimensionality (3D) of beach response, which determines wave breaking and affects beach safety. Using a combination of measured shoreline variability and empirical beach classification schemes, the response to changes in the wave conditions at each beach have been assessed. The sites exhibited net long term accretion derived from the intertidal beach volume. Throughout the survey period intersite similarity in beach response was observed in response to storm waves, yet coupling between the seasonal wave climate and the beach morphology was not evident at any of the sites, due to the dominance of recovery phases following storm events. The role of increased wave conditions (exceeding Hs=4 m) during sustained storm events (> 50 hrs) led to offshore transport from the beach face to the subtidal bar region. Post-storm recovery was characterised by onshore transport and the development of substantial 3D low tide morphology. Under normal wave conditions (Hs=1.6 m) the dominant 3D features smoothed out as channels in-filled and bars reduced over a period of 2-3 months. This cyclicity was observed on ~3 occasions at the northern sites, while Gwithian remained more stable throughout; reflecting the more sheltered position of the beach. Overall the beaches exhibited a significant storm dominated morphological response cycle, unlike the more familiar winter/summer seasonal response. Nearshore bar behaviour at Perranporth and Porthtowan, assessed using ARGUS images, was dominated by offshore migration (ca.20 m/yr) following closely the net intertidal accretion, while bar shape exhibited changes over monthly periods. Intensive field studies of morphological change, nearshore current flows and surf zone wave conditions were undertaken at Porthtowan during small swell dominated waves and large energetic storm conditions in May and October 2010 respectively. The field data highlighted accretionary response under small swell dominated waves, and strong offshore directed undertow flows (0.5 m/s-1) during erosive energetic conditions (>Hs = 4m) which were then related to the monthly surveys. These results were applied to XBeach model simulations which helped further identify the importance of antecedent morphology and the complexities of intertidal geology in controlling beach response. The study provides the longest continuous record of beach morphology dynamics for macrotidal energetic sites and provides a valuable addition to work in this field. The dominance of storm driven morphological response was clear with highly threedimensional morphology developing under post storm conditions and continued beach evolution driven by the seasonal conditions. Antecedent morphology was found to be a key element of beach response with geological control an additional component. The projected reduction in wave conditions due to the Wave Hub and the natural variability observed indicates the sites are unlikely to shift significantly from their current dynamic state in response to the Wave Hub, and as such the potential impact on nearshore and beach dynamics is minimal.
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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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Saulter, Andrew Nicholas. "Analysis of infragravity frequency sediment transport on macrotidal beaches." Thesis, University of Plymouth, 2000. http://hdl.handle.net/10026.1/1751.

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Many cross-shore sediment transport models use simple treatments of infragravity frequency (0.005- 0.05Hz) processes. For example, infragravity waves have been assumed to provide solely a 'drift velocity' for transport of sediment mobilised by incident frequency waves (0.05-0.5Hz) and be 100% reflected at the shoreline. Furthermore, numerous models calculate broken incident wave heights on the basis of water depth only. This work investigates both the processes underlying infragravity frequency variations in the crossshore velocity field, and the resulting effect of such variations on sediment suspension and transport. Data were selected from three beach experiments in order to compare observations from a range of energetic conditions and positions in the nearshore. Experiments conducted on a dissipative beach at Llangennith, and an intermediate beach at Spurn Head, form part of the pre-existing British Beach And Nearshore Dynamics dataset. The third deployment, at a dissipative site at Perranporth (Cornwall), provided new data for analysis. At Llangennith, high swell waves (significant wave height 3m) were observed, and the measurements come from an infragravity wave dominated saturated surf zone. At Perranponh, locally generated wind wave heights were 2m and measurements came from an incident wave dominated saturated surf zone. Conditions at Spurn Head saw swell wave heights of 1.5m, and observations were made in both an incident wave dominated non-saturated surf zone and the incident wave shoaling zone. Analysis of the data revealed that, in the surf zone, the nature of the infragravity wave field was dependent upon the distribution of energy between higher (>0.02Hz) and lower (<0.02Hz) infragraviiy frequencies. Lower frequency infragravity waves were found to shoal as free waves, while higher frequency infragravity waves were dissipated near to shore on low gradient beaches. Inftagravity wave reflection coefficients showed a dependence on frequency and beach slope (parameterised by the Iribarren number), varied between 50-90% for lower infragravity frequencies, and could be less than 50% for higher infragraviiy frequencies. Incident wave heights were modulated in the shoaling zone with a 'groupy' form. Modulation was also observed in the surf zone, but in the form of individual large waves occurring at low frequency. In the shoaling zone and very close to shore, non-linear interactions occurred between the incident and infragravity components, and calculated phase values between modulated incident waves and infragravity waves indicated a phase shift from a value of less than 180° in the shoaling zone toward 0° close to shore. However, the two signals were not significantly correlated for much of the surf zone. High velocities resulting from a combination of the mean, infragravity and incident wave components drove sediment suspension. Large suspension events occurring at infragravity frequencies were correlated with incident wave groupiness in the shoaling zone, and in high energy conditions with infragravity waves near to the swash zone. Such variations in suspension were related not only to velocity magnitude, but the duration for which a threshold for suspension was exceeded. The bed response to forcing also varied during a tide, possibly as a result of changing bed conditions (e.g. due to bedforms). The infragravity contribution to suspension was independent of the magnitude of suspended sediment concentration, and increased from approximately 30% at the breaker line to 90% in an infragravity wave dominated inner surf zone. The contribution of the infragravity component to transport did not show a similar behaviour, due to phase effects, which produced a reversal in the transport direction between higher and lower infragravity frequencies. Comparison of the observations of sediment transport with energetics predictors identified several cases where the observed transport was qualitatively different from the model prediction as a result of sediment transport thresholds being exceeded at, or for, infragravity timescales.
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Thurston, William. "Turbulence as a mediator of processes in a macrotidal estuary." Thesis, University of Leeds, 2009. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.515412.

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Souchu, Philippe. "Contribution à l'étude du cycle de l'azote en écosystème macrotidal." Brest, 1986. http://www.theses.fr/1986BRES2034.

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L'evolution saisonniere des transferts biogeochimiques d'azote inorganique dissous (nid) aux trois interfaces (eau douce-eau de mer; eau-sediment; eau-atmosphere) est etudiee dans un ecosysteme littoral macrotidal d'europe occidentale (la rade de brest, france). En periode hivernale et printaniere, la principale voie de fertilisation (azote nitrique) est d'origine fluviale (lessivage des sols de bassins versants agricoles). Le recyclage de l'azote, a l'interface eau-sediment, sous forme ammoniacale, permet le maintien d'une production primaire importante en ete et en automne. Les flux de nid d'origine atmospherique sont mesures sur trois sites de bretagne occidentale (influence marine, agricole et urbaine). S'ils restent faibles a l'echelle annuelle, ces flux peuvent representer pour l'ecosysteme littoral une source transitoire non negligeable, en periode estivale et automnale. Des budgets saisonniers des flux de nid entrant dans le systeme sont dresses et compares aux besoins de la production primaire pelagique. La dynamique du nid et de l'activite des producteurs primaires est interpretee en relation avec le concept d'ergocline
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Van, Proosdij Danika. "Spatial and temporal controls on the sediment budget of a macrotidal saltmarsh." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2001. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/NQ61989.pdf.

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Maspataud, Aurélie. "Impacts des tempêtes sur la morphodynamique du profil côtier en milieu macrotidal." Phd thesis, Université du Littoral Côte d'Opale, 2011. http://tel.archives-ouvertes.fr/tel-00658671.

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Le littoral Est dunkerquois, comme la plupart des côtes méridionales de la Mer du Nord, est constitué de larges plages sableuses à barres intertidales et de dunes côtières qui protègent des zones basses densément peuplées particulièrement vulnérables dans le contexte actuel de montée du niveau marin associée au changement climatique. Les objectifs de ce travail et la démarche méthodologique adoptée reposent sur une approche à plusieurs échelles spatiales et temporelles afin dévaluer l'impact des tempêtes sur l'évolution d'une côte basse macrotidale à fetch limité. A l'échelle évènementielle, les mesures ont souligné une réponse morphologique très différente de la côte face aux conditions énergétiques et tempétueuses, sur deux secteurs d'étude situés à 4 km de distance. Cette réponse très contrastée se traduit par des conditions hydrodynamiques différentes sur les deux sites, avec un secteur Ouest plus sensible à l'érosion que le secteur Est, plutôt stable voire en accrétion. Sur une échelle saisonnière à pluriannuelle, l'évolution de la côte et notamment sa capacité à se reconstruire durant les phases post-érosives a été mise en évidence, soulignant notamment l'efficacité des transports éoliens dans l'alimentation et la cicatrisation des dunes. A moyen terme, de 1957 à 2010, l'évolution du trait de côte a montré une grande variabilité à la fois spatiale et temporelle, qui semble être expliquée par une variabilité spatiale de l'énergie de la houle à la côte, en partie liée à la bathymétrie de l'avant-côte, mais aussi par les variations des forçages météo-marins et des interventions anthropiques locales. Certaines conditions météorologiques plus morphogènes ont été mises en évidence, telles que des vents persistants de secteur N-NW soufflant à plus de 8 m/s pendant plus de 48 heures, par exemple. Les mesures réalisées dans cette étude ont également permis la mise en place et la validation de deux codes morphodynamiques de modélisation à court terme de la réponse de la côte aux évènements de tempête, SBEACH et X-BEACH, qui ont tous deux donné des résultats cohérents sur le littoral étudié. Si le premier restitue mieux l'évolution morphodynamique et le second les conditions hydrodynamiques mesurées in-situ, ils restent tous les deux pertinents voire complémentaires.
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Evans, Paul Stephen. "Hydrodynamic characteristics of macrotidal straits and implications for tidal stream turbine deployment." Thesis, Cardiff University, 2014. http://orca.cf.ac.uk/70531/.

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National efforts to reduce energy dependency on fossil fuels have prompted examination of macrotidal nearshore zones around the UK for potential tidal stream resource development. Although a number of prospective tidal energy sites have been identified, the local hydrodynamics of these sites are often poorly understood. Tidal-energy developers rely on detailed characterisation of tidal energy sites prior to device field trials and installation. Although first-order appraisals may make macrotidal tidal straits appear attractive for development, detailed, site-specific hydrodynamic and bathymetric surveys are important for determining site suitability for tidal stream turbine (TST) installation. Understanding the ways in which coastal features affect tidal velocities at potential TST development sites will improve identification and analysis of physical constraints on tidal-energy development. Ramsey Sound (Pembrokeshire, Wales, UK) will soon host Wales’ first TST demonstration project. However, the local hydrodynamics of the sound have been underexamined. Ramsey Sound experiences a marked tidal asymmetry, with local bathymetric features that affect flow fields which are spatially heterogeneous in three dimensions. Using Ramsey Sound as a case study, this thesis has three objectives: (1) to examine the wake created by submerged objects through field- and laboratory-based measurements, (2) to experimentally investigate the effect of submergence on wake development and decay downstream of a conical island, and (3) to develop a TST suitability tool, which examines the effects of velocity, water depth and bed slope on power availability within a macrotidal coastal area. Laboratory experiments have shown that submergence level is an important parameter controlling wake structure and extent, and that changes in submergence level affect both the 3-D flow structure in the near wake and the 2-D far wake of islands. Analysis of physical and hydrodynamic characteristics in Ramsey Sound, including tidal velocities across the swept area of the pilot TST, vertical shear in the stream flow, estimated power output, water depth and bed slope, suggests that the spatial and temporal variability in the flow field may render much of Ramsey Sound unsuitable for tidal power extraction. Although the resource potential depends on velocity and bathymetric conditions that are fundamentally local, many prospective tidal energy sites are subject to similar physical and hydrodynamic constraints. Results of this study can help inform site selection in these complicated, highly dynamic macrotidal environments.
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Dobroniak, Christine. "Géomorphologie, hydrodynamique et écologie d'un estuaire temperé macrotidal : l'Authie, Manche Orientale, France." Littoral, 2000. http://www.theses.fr/2000DUNK0036.

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L'Authie est un estuaire macrotidal (marnage moyen de vive-eau à l'embouchure = 8. 54 m) qui a été largement comblé par des sables d'origine marine et introduits dans l'estuaire par des courants de marée dominés par le flot, et par des vagues de tempêtes. L'estuaire, qui constitue le terminus d'un petit fleuve côtier (longueur = 98 km), a une longue histoire d'occupation humaine et se situe sur une côte riche en sables stockés dans des bancs et des dunes côtiers. Les tendances évolutives de l'embouchure de l'estuaire ont été analysées à partir de documents historiques, de cartes bathymétriques anciennes, et de photographies aériennes. La démarche méthodologique a été complétée par plusieurs campagnes de mesures hydrodynamiques, in situ, portant sur les niveaux d'eau, les houles et les courants, et par des suivis topométriques de la rive nord. Elles montrent un ensablement progressif de l'estuaire du fait surtout d'une accrétion importante d'une plate-forme sableuse en rive sud qui s'étend vers le nord, à travers l'embouchure, et qui est alimentée en sables par des courants de dérive littorale liés à la marée et aux houles. Les travaux révèlent aussi une rétention, à l'intérieur de l'estuaire, de sables érodes des dunes de la rive nord exposées aux tempêtes et aux forts courants de marée à asymétrie liée au flot. Cette accrétion importante, qui a pu être exacerbée par les effets mal connus d'une importante poldérisation au sein de l'estuaire, a pratiquement comblé l'embouchure, et conditionne de plus en plus la distribution de la faune et de la flore estuariennes. L'Authie diffère ainsi des estuaires macrotidaux peu combles comportant des bancs et des chenaux longitudinaux tidaux. L'érosion localisée et l'accrétion généralisée posent aussi des problèmes sévères d'aménagement, notamment en matière de protection des rivages estuariens, et de survie à terme de l'estuaire<br>The Authie is a macrotidal (mean estuary-mouth spring tide range = 8. 54 m) estuary that has been largely infilled by marine sand transported by fllord dominant tides and storm waves. The estuary, which forms the terminus of a short (98 km) coastal river in northern France, has a long history of human occupation and is located on a sand-rich coast characterized by nearshore banks and coastal dunes. The patterns of recent sedimentation and erosion within the estuary were deduced from analyses of historical documents, bathymetric charts, aerial photographs, and from field work involving several hydrodynamic surveys covering water levels, waves and currents, and topographic surveys of the north bank of the estuary. The results show rapid infill of the Authie as a result of both massive accretion of a south bank sand platform that has extended northwards across the estuary mouth, under the influence of wave – and tide – induced longshore sand transport, and estuarine retention of sand, through flood-dominant asymmetry, eroded from north bank dunes exposed to storm waves. This massive accretion has almost completely infilled the estuary mouth which lacks the linear tidal ridges and channels typical of unfilled macrotidal estuaries. It also increasingly conditions the distribution of the estuarine fauna and flora. Large-scale empoldering of the estuary may have exacerbated flood asymmetry. The localized erosion and generalized sedimentation at the mouth of th estuary pose a number of severe management problems, notably estuarine shoreline protection, and call into question the very survival of the estuary itself
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Ishak, Abdul Kadir. "Suspended sediment dynamics and flux in the macrotidal Taf estuary, South Wales." Thesis, Bangor University, 1997. https://research.bangor.ac.uk/portal/en/theses/suspended-sediment-dynamics-and-flux-in-the-macrotidal-taf-estuary-south-wales(2a686e53-be86-4731-ac19-aa998d5400ba).html.

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Books on the topic "Macrotidal"

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Bayer, Angelika Karolina. Biogeochemical and geomorphological controls on mercury dynamics in a macrotidal salt marsh, Bay of Fundy, Canada. 2004.

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Book chapters on the topic "Macrotidal"

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Krumme, U., and U. Saint-Paul. "Dynamics in Mangrove Fish Assemblages on a Macrotidal Coast." In Ecological Studies. Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-642-13457-9_12.

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Tweedley, James, Richard Warwick, and Ian Potter. "The Contrasting Ecology of Temperate Macrotidal and Microtidal Estuaries." In Oceanography and Marine Biology - An Annual Review. CRC Press, 2016. http://dx.doi.org/10.1201/9781315368597-3.

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Ajani, Penelope, Gustaaf Hallegraeff, Drew Allen, et al. "The Contrasting Ecology of Temperate Macrotidal and Microtidal Estuaries." In Oceanography and Marine Biology - An Annual Review. CRC Press, 2016. http://dx.doi.org/10.1201/9781315368597-9.

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Lessa, G. "Tidal dynamics and sediment transport in a shallow macrotidal estuary." In Mixing in Estuaries and Coastal Seas. American Geophysical Union, 1996. http://dx.doi.org/10.1029/ce050p0338.

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Sautour, Benoît, and Jacques Castel. "Comparative spring distribution of zooplankton in three macrotidal European estuaries." In Major Biological Processes in European Tidal Estuaries. Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-009-0117-9_12.

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Valéry, L., and J. C. Lefeuvre. "The Macrotidal Bay of Mont-Saint-Michel (France): The Function of Salt Marshes." In The Wetland Book. Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6173-5_137-2.

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Valéry, Loïc, and Jean-Claude Lefeuvre. "The Macrotidal Bay of Mont-Saint-Michel (France): The Function of Salt Marshes." In The Wetland Book. Springer Netherlands, 2018. http://dx.doi.org/10.1007/978-94-007-4001-3_137.

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Thiébaut, E., Y. Lagadeuc, F. Olivier, J. C. Dauvin, and C. Retière. "Do hydrodynamic factors affect the recruitment of marine invertebrates in a macrotidal area?" In Recruitment, Colonization and Physical-Chemical Forcing in Marine Biological Systems. Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-017-2864-5_14.

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Elliott, T., and A. R. Gardiner. "Ripple, Megaripple and Sandwave Bedforms in the Macrotidal Loughor Estuary, South Wales, U.K." In Holocene Marine Sedimentation in the North Sea Basin. Blackwell Publishing Ltd., 2009. http://dx.doi.org/10.1002/9781444303759.ch4.

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Kitazawa, Toshiyuki, and Naomi Murakoshi. "Tidal ravinement surfaces in the Pleistocene macrotidal tide-dominated Dong Nai estuary, southern Vietnam." In Contributions to Modern and Ancient Tidal Sedimentology. John Wiley & Sons, Ltd, 2016. http://dx.doi.org/10.1002/9781119218395.ch13.

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Conference papers on the topic "Macrotidal"

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PRODGER, SAM, PAUL RUSSELL, MARK DAVIDSON, and JON MILES. "GRAIN SIZE VARIABILITY ON HIGH-ENERGY MACROTIDAL BEACHES." In Coastal Sediments 2015. WORLD SCIENTIFIC, 2015. http://dx.doi.org/10.1142/9789814689977_0059.

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2

Fisher, Paul R., and Tim J. O’Hare. "Modelling Sand Transport and Profile Evolution on Macrotidal Beaches." In 25th International Conference on Coastal Engineering. American Society of Civil Engineers, 1997. http://dx.doi.org/10.1061/9780784402429.232.

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3

Simmonds, David J., Tim J. O’Hare, and David A. Huntley. "The Influence of Long Waves on Macrotidal Beach Morphology." In 25th International Conference on Coastal Engineering. American Society of Civil Engineers, 1997. http://dx.doi.org/10.1061/9780784402429.239.

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4

Leonardi, Nicoletta. "Modelling of Intertidal Sediment Transport in a Macrotidal Embayment." In Proceedings of the 39th IAHR World Congress From Snow to Sea. International Association for Hydro-Environment Engineering and Research (IAHR), 2022. http://dx.doi.org/10.3850/iahr-39wc2521711920221050.

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5

Buscombe, Daniel, Martin J. Austin, and Gerhard Masselink. "Field Observations of Step Dynamics on a Macrotidal Gravel Beach." In Sixth International Symposium on Coastal Engineering and Science of Coastal Sediment Process. American Society of Civil Engineers, 2007. http://dx.doi.org/10.1061/40926(239)44.

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6

CARDONA, CAMILO JARAMILLO, MAURICIO GONZÁLEZ RODRÍGUEZ, RAÚL MEDINA SANTAMARÍA, ERIK EGUIGUREN CABEZAS, LUCAS DE FREITAS PEREIRA, and ERICA PELLÓN DE PABLO. "EQUILIBRIUM-BASED SHORELINE EVOLUTION MODELS APPLIED TO A MACROTIDAL ENVIRONMENT." In Coastal Sediments 2023. WORLD SCIENTIFIC, 2023. http://dx.doi.org/10.1142/9789811275135_0128.

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7

VALIENTE, N. G., J. MCCARROLL, G. MASSELINK, T. SCOTT, D. CONLEY, and E. KING. "CIRCULATION AND SEDIMENT FLUXES ON A MACROTIDAL, EXPOSED AND EMBAYED COASTLINE." In International Conference on Coastal Sediments 2019. WORLD SCIENTIFIC, 2019. http://dx.doi.org/10.1142/9789811204487_0048.

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8

Stépanian, Alexis, Brigitte Vlaswinkel, Franck Levoy, and Claude Larsonneur. "Sediment Transport on a Macrotidal Ridge and Runnel Beach during Accretion Conditions." In Fourth Conference on Coastal Dynamics. American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40566(260)104.

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9

Voulgaris, George, Travis Mason, and Michael B. Collins. "An Energetics Approach for Suspended Sand Transport on Macrotidal Ridge and Runnel Beaches." In 25th International Conference on Coastal Engineering. American Society of Civil Engineers, 1997. http://dx.doi.org/10.1061/9780784402429.305.

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10

SUANEZ, Serge, Jean-Marie CARIOLET, and Bernard FICHAUT. "Dynamique morphosédimentaire des cordons dunaires et cinématique du trait de côte en contexte macrotidal." In Journées Nationales Génie Côtier - Génie Civil. Editions Paralia, 2012. http://dx.doi.org/10.5150/jngcgc.2012.050-s.

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