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1

SATCHELL, JULIE. "Neolithic Archaeology in the Inter-Tidal Zone." International Journal of Nautical Archaeology 39, no. 1 (March 2010): 199–200. http://dx.doi.org/10.1111/j.1095-9270.2009.00260_3.x.

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2

Iwama, G., and A. Todgham. "Cross-tolerance in an inter-tidal sculpin." Comparative Biochemistry and Physiology Part A: Molecular & Integrative Physiology 150, no. 3 (July 2008): S155—S156. http://dx.doi.org/10.1016/j.cbpa.2008.04.401.

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3

Jeong, Shin Taek, Hongyeon Cho, and Dong Hui Ko. "Development of the Inter-tidal Exposure Duration Formulae Using Tidal Harmonic Constants." Journal of Korean Society of Coastal and Ocean Engineers 24, no. 5 (October 31, 2012): 319–25. http://dx.doi.org/10.9765/kscoe.2012.24.5.319.

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4

Donselaar, M. E., and C. R. Geel. "Facies architecture of heterolithic tidal deposits: the Holocene Holland Tidal Basin." Netherlands Journal of Geosciences - Geologie en Mijnbouw 86, no. 4 (December 2007): 389–402. http://dx.doi.org/10.1017/s001677460002360x.

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AbstractThe size, shape and spatial position of lithofacies types (or facies architecture) in a tidal estuarine basin are complex and therefore difficult to model. The tidal currents in the basin concentrate sand-sized sediment in a branching pattern of tidal channels and fringing tidal flats. Away from the sandy tidal flats the sediment gradually changes to mud-dominated heterolithic deposits and clay. In this paper the facies analysis of a tidal estuarine basin, the Holocene Holland Tidal Basin (HHTB) is presented based on core data and Cone Penetration Tests (CPT). Four lithofacies associations are recognized: (1) tidal channel sand, (2) sand-dominated heterolithic inter-tidal flat, (3) mud-dominated heterolithic inter-channel and (4) fresh-water peat. The high data density allowed for the construction of a detailed facies architecture model in which the size, shape and spatial position of the tidal estuarine facies elements were established. The results can be used to improve the reservoir modelling in highly heterogeneous estuarine reservoir settings.
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5

Couperthwaite, J. S., S. B. Mitchell, J. R. West, and D. M. Lawler. "Cohesive Sediment Dynamics on an Inter-tidal Bank on the Tidal Trent, UK." Marine Pollution Bulletin 37, no. 3-7 (March 1999): 144–54. http://dx.doi.org/10.1016/s0025-326x(98)00175-1.

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6

Caetano, M., M. Falcão, C. Vale, and M. J. Bebianno. "Tidal flushing of ammonium, iron and manganese from inter-tidal sediment pore waters." Marine Chemistry 58, no. 1-2 (October 1997): 203–11. http://dx.doi.org/10.1016/s0304-4203(97)00035-2.

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7

Freeman, D. P., L. E. Coates, M. C. Ockenden, W. Roberts, and J. R. West. "Cohesive sediment transport on an inter-tidal zone under combined wave-tidal flow." Netherlands Journal of Aquatic Ecology 28, no. 3-4 (September 1994): 283–88. http://dx.doi.org/10.1007/bf02334196.

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8

Wright, M. E., A. M. Abdelzaher, H. M. Solo-Gabriele, S. Elmir, and L. E. Fleming. "The inter-tidal zone is the pathway of input of enterococci to a subtropical recreational marine beach." Water Science and Technology 63, no. 3 (February 1, 2011): 542–49. http://dx.doi.org/10.2166/wst.2011.255.

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Efforts were made to evaluate the source of enterococci levels at a recreational beach. Four monitoring efforts were implemented which included tidal studies, hourly sampling, runoff sampling, and spatially intensive sediment sampling. Spatially intensive sediment sampling indicated that enterococci concentrations consistently decreased away from the inter-tidal zone, both seaward and landward. During dry conditions, the highest concentrations in the water were observed during high tide (71±48 CFU/100 mL) and lower concentrations were observed during low tide (4±3 CFU/100 mL). Runoff was characterised by very high levels (11,700 CFU/100 mL). Results from these monitoring efforts collectively showed that the source of enterococci to the study beach is geographically located within the inter-tidal zone. Wash-in from the inter-tidal zone through tidal action and runoff plays a major role in controlling enterococci levels within the water column. Such results are significant in identifying the source and transport mechanisms of enterococci, which can subsequently be used as part of a modelling effort aimed at predicting enterococci levels at recreational beaches.
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9

Fitzsimons, MF, M. Dawit, DM Revitt, and C. Rocha. "Effects of early tidal inundation on the cycling of methylamines in inter-tidal sediments." Marine Ecology Progress Series 294 (2005): 51–61. http://dx.doi.org/10.3354/meps294051.

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10

Mao, Xinyan, Wensheng Jiang, Ping Zhang, and Shizuo Feng. "Numerical study on inter-tidal transports in coastal seas." Journal of Ocean University of China 15, no. 3 (May 7, 2016): 379–88. http://dx.doi.org/10.1007/s11802-016-2825-z.

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11

McCoy, Sophie J., Catherine A. Pfister, Gerard Olack, and Albert S. Colman. "Diurnal and tidal patterns of carbon uptake and calcification in geniculate inter-tidal coralline algae." Marine Ecology 37, no. 3 (March 17, 2016): 553–64. http://dx.doi.org/10.1111/maec.12295.

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12

Nash, S., N. O׳Brien, A. Olbert, and M. Hartnett. "Modelling the far field hydro-environmental impacts of tidal farms – A focus on tidal regime, inter-tidal zones and flushing." Computers & Geosciences 71 (October 2014): 20–27. http://dx.doi.org/10.1016/j.cageo.2014.02.001.

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13

Ritchie, W. "Inter-tidal and sub-tidal organic deposits and sea level changes in the Uists, Outer Hebrides." Scottish Journal of Geology 21, no. 2 (September 1985): 161–76. http://dx.doi.org/10.1144/sjg21020161.

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14

Latham, Dorian, Chris Milburn, Bruce Munro, John Wilson, Stephen Sherry, and Katy Baker. "Creating inter-tidal and freshwater habitat on a brownfield site." Proceedings of the Institution of Civil Engineers - Civil Engineering 169, no. 4 (November 2016): 185–92. http://dx.doi.org/10.1680/jcien.16.00001.

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15

Mendonça, Vanessa, Catarina Vinagre, Henrique Cabral, and Ana C. F. Silva. "Habitat use of inter-tidal chitons - role of colour polymorphism." Marine Ecology 36, no. 4 (September 13, 2014): 1098–106. http://dx.doi.org/10.1111/maec.12205.

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16

Hauk, Markus, and Roland Pail. "Gravity Field Recovery Using High-Precision, High–Low Inter-Satellite Links." Remote Sensing 11, no. 5 (March 5, 2019): 537. http://dx.doi.org/10.3390/rs11050537.

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Past temporal gravity field solutions from the Gravity Recovery and Climate Experiment (GRACE), as well as current solutions from GRACE Follow-On, suffer from temporal aliasing errors due to undersampling of the signal to be recovered (e.g., hydrology), which arise in terms of stripes caused by the north–south observation direction. In this paper, we investigate the potential of the proposed mass variation observing system by high–low inter-satellite links (MOBILE) mission. We quantify the impact of instrument errors of the main sensors (inter-satellite link and accelerometer) and high-frequency tidal and non-tidal gravity signals on achievable performance of the temporal gravity field retrieval. The multi-directional observation geometry of the MOBILE concept with a strong dominance of the radial component result in a close-to-isotropic error behavior, and the retrieved gravity field solutions show reduced temporal aliasing errors of at least 30% for non-tidal, as well as tidal, mass variation signals compared to a low–low satellite pair configuration. The quality of the MOBILE range observations enables the application of extended alternative processing methods leading to further reduction of temporal aliasing errors. The results demonstrate that such a mission can help to get an improved understanding of different components of the Earth system.
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17

Gonçalves, Ana Ribeiro, Liliana de Sousa, Pedro Duarte-Coelho, and Vitor Carvalho Almada. "Tidal variation in a rocky inter-tidal fish population: the case of white seabream Diplodus sargus juveniles." Marine Ecology 36, no. 4 (October 24, 2014): 1468–71. http://dx.doi.org/10.1111/maec.12216.

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18

Mehri, S., M. Shafie-khah, P. Siano, M. Moallem, M. Mokhtari, and J. P. S. Catalão. "Contribution of tidal power generation system for damping inter-area oscillation." Energy Conversion and Management 132 (January 2017): 136–46. http://dx.doi.org/10.1016/j.enconman.2016.11.023.

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19

Giri, Chandra. "Recent Advancement in Mangrove Forests Mapping and Monitoring of the World Using Earth Observation Satellite Data." Remote Sensing 13, no. 4 (February 5, 2021): 563. http://dx.doi.org/10.3390/rs13040563.

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20

Donner, Monika, Erik Pasche, and Edgar Nehlsen. "LONG-TERM APPROACH FOR MORPHODYNAMIC PROCESSES IN TIDAL MARSH-WATERCOURSES." Coastal Engineering Proceedings 1, no. 32 (January 25, 2011): 71. http://dx.doi.org/10.9753/icce.v32.sediment.71.

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Tidal marsh-watercourses form a significant link between marine and fluvial environment. As consequence bi-directional forces due to asymmetric tides and inland runoff deform morphodynamic processes with presence of cohesive and organic sediment. In combination with the high inter-tidal area proportion and additional anthropogenic deformations special requirements for the long-term approach restrict existing methods. This paper exposes significant processes in tidal marsh-watercourses based on a research study. The identified processes were integrated into a specified long-term approach taking these special requirements into account. By using a numerical model the range of uncertainty for different impacts were considered and results in a long-term riverbed evolution.
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21

Kessler, T. A., and T. R. Parsons. "Primary Production in a Tidally Energetic Fjord: Evidence of Seasonal and Inter-annual Tidal Forcing." Canadian Journal of Fisheries and Aquatic Sciences 46, no. 12 (December 1, 1989): 2166–72. http://dx.doi.org/10.1139/f89-268.

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A long term data set collected from a tidally energetic sill fjord was analyzed for its statistical relationships between primary production indices and several represented environmental variables. The analysis identified variance and covariance structure in these variables implicating changes in water column clarity, in inter-annual variability of phytoplankton carbon uptake rate, and the static stability of basin surface water in phytoplankton standing stock. The biomass–stability relationship was found to be seasonally dependent, with biomass positively correlated with stability in the summer and negatively correlated in the spring/fall, and restricted to waters under the direct mixing influence of the tidal inflow jet. These statistical patterns are discussed in terms of a possible control of primary production by seasonal and inter-annual variations in tidal inflow buoyancy.
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22

Ferrarin, Christian, Debora Bellafiore, Gianmaria Sannino, Marco Bajo, and Georg Umgiesser. "Tidal dynamics in the inter-connected Mediterranean, Marmara, Black and Azov seas." Progress in Oceanography 161 (February 2018): 102–15. http://dx.doi.org/10.1016/j.pocean.2018.02.006.

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23

Ehmke, Glenn, Grainne S. Maguire, Tomas Bird, Daniel Ierodiaconou, and Michael A. Weston. "An obligate beach bird selects sub-, inter- and supra-tidal habitat elements." Estuarine, Coastal and Shelf Science 181 (November 2016): 266–76. http://dx.doi.org/10.1016/j.ecss.2016.08.050.

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24

Silva, Ana C. F., Maryam Shapouri, Rui Cereja, Awantha Dissanayake, and Catarina Vinagre. "Variations in crab claw morphology and diet across contrasting inter-tidal habitats." Marine Ecology 38, no. 1 (February 2017): e12374. http://dx.doi.org/10.1111/maec.12374.

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25

BRYANT, R., A. TYLER, D. GILVEAR, P. MCDONALD, I. TEASDALE, J. BROWN, and G. FERRIER. "A preliminary investigation into the spectral characteristics of inter-tidal estuarine sediments." International Journal of Remote Sensing 17, no. 2 (January 1996): 405–12. http://dx.doi.org/10.1080/01431169608949016.

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26

Wilson, Peter, Kieran Westley, Ruth Plets, and Michael Dempster. "Radiocarbon dates from the inter-tidal peat bed at Portrush, County Antrim." Irish Geography 44, no. 2-3 (July 2011): 323–29. http://dx.doi.org/10.1080/00750778.2011.620415.

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27

Callaghan, Des A., and Gareth Farr. "The unusual inter-tidal niche of the rare moss Bryum marratii Wilson." Journal of Bryology 40, no. 4 (October 2, 2018): 371–76. http://dx.doi.org/10.1080/03736687.2018.1525972.

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28

Clark, Melody S., Paul Geissler, Catherine Waller, Keiron P. P. Fraser, David K. A. Barnes, and Lloyd S. Peck. "Low heat shock thresholds in wild Antarctic inter-tidal limpets (Nacella concinna)." Cell Stress and Chaperones 13, no. 1 (February 7, 2008): 51–58. http://dx.doi.org/10.1007/s12192-008-0015-7.

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29

Jiang, Dengrong, Zixuan Lin, Peiying Liu, Sandeepa Sur, Cuimei Xu, Kaisha Hazel, George Pottanat, et al. "Normal variations in brain oxygen extraction fraction are partly attributed to differences in end-tidal CO2." Journal of Cerebral Blood Flow & Metabolism 40, no. 7 (August 5, 2019): 1492–500. http://dx.doi.org/10.1177/0271678x19867154.

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Cerebral oxygen extraction fraction is an important physiological index of the brain’s oxygen consumption and supply and has been suggested to be a potential biomarker for a number of diseases such as stroke, Alzheimer’s disease, multiple sclerosis, sickle cell disease, and metabolic disorders. However, in order for oxygen extraction fraction to be a sensitive biomarker for personalized disease diagnosis, inter-subject variations in normal subjects must be minimized or accounted for, which will otherwise obscure its interpretation. Therefore, it is essential to investigate the physiological underpinnings of normal differences in oxygen extraction fraction. This work used two studies, one discovery study and one verification study, to examine the extent to which an individual’s end-tidal CO2 can explain variations in oxygen extraction fraction. It was found that, across normal subjects, oxygen extraction fraction is inversely correlated with end-tidal CO2. Approximately 50% of the inter-subject variations in oxygen extraction fraction can be attributed to end-tidal CO2 differences. In addition, oxygen extraction fraction was found to be positively associated with age and systolic blood pressure. By accounting for end-tidal CO2, age, and systolic blood pressure of the subjects, normal variations in oxygen extraction fraction can be reduced by 73%, which is expected to substantially enhance the utility of oxygen extraction fraction as a disease biomarker.
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30

Prasad, M. Bala Krishna, Michael C. Maddox, Aditya Sood, Sujay Kaushal, and Raghu Murtugudde. "Nutrients, chlorophyll and biotic metrics in the Rappahannock River estuary: implications of urbanisation in the Chesapeake Bay watershed, USA." Marine and Freshwater Research 65, no. 6 (2014): 475. http://dx.doi.org/10.1071/mf12351.

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In the Chesapeake Bay watershed, various endeavours such as the inter-state agreements and Chesapeake 2000 agreement have been implemented to improve water quality and ecological conditions, and have produced mixed results at best in various tributaries. So as to evaluate the management efforts on ecological conditions in the Rappahannock River watershed, we analysed the long-term variability in land use, nutrient content and ecological biotic metrics. It appears that the inter-annual variability in nutrient loadings and concentrations is largely influenced by changes in urbanisation and climate. Significant increases in urban development (35%) and population growth have exacerbated both point and non-point nutrient pollution in the Rappahannock River. The comparatively low N : P ratio in the tidal zone, with respect to the non-tidal zone, may be due to salinity-induced P leaching from sediments regulating the water quality along the river–estuary continuum. In addition, inter-annual variability in ecological biotic metrics demonstrates degrading ecological conditions in the Rappahannock River watershed, which are primarily due to increasing watershed urbanisation driving high nutrient loadings and altered nutrient stoichiometry.
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31

Yoo, Jeseon, Sungwon Shin, Ki-Cheon Jun, and Jae-Seol Shim. "FIELD OBSERVATIONS AND MODEL PREDICTIONS OF WAVE TRANSFORMATION ON A MACRO-TIDAL BEACH, KOREA." Coastal Engineering Proceedings 1, no. 33 (December 15, 2012): 43. http://dx.doi.org/10.9753/icce.v33.waves.43.

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Macro-tidal beach processes are influenced by complicated interactions of tide actions, coastal waves and morphological changes. Tidal cycles may be a primary forcing responsible for specific characteristics of hydrodynamic and morphological processes complicated on the intertidal flat in space and time. Macro-tidal sandy beaches are frequently developed in the west coast of Korea, experiencing seasonal variations of inter-tidal processes caused by a monsoonal climate in the Yellow Sea. Large winter waves tend to excite active beach morphological processes, inducing beach erosion and seaward-directed sediment transports. This study is intended to investigate and characterize intertidal hydrodynamics including wave dynamics in a macro-tide environment in Korea, by using a numerical model named COBRAS. The measured water surface elevation data are divided into wave and tidal components, in order to be used as inputs of the model. Tidal components in terms of water level change are implemented in the model by adding constant currents at the offshore boundary. Comparisons of the measurements and the predictions show a good performance of the model for wave height transformation and wave set-up across the macro-tidal beach
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32

Ortega, Arturo, Joseph Praful Tomy, Jonathan Shek, Stephane Paboeuf, and David Ingram. "An Inter-Comparison of Dynamic, Fully Coupled, Electro-Mechanical, Models of Tidal Turbines." Energies 13, no. 20 (October 15, 2020): 5389. http://dx.doi.org/10.3390/en13205389.

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Production of electricity using hydrokinetic tidal turbines has many challenges that must be overcome to ensure reliable, economic and practical solutions. Kinetic energy from flowing water is converted to electricity by a system comprising diverse mechanical and electrical components from the rotor blades up to the electricity grid. To date these have often been modelled using simulations of independent systems, lacking bi-directional, real-time, coupling. This approach leads to critical effects being missed. Turbulence in the flow, results in large velocity fluctuations around the blades, causing rapid variation in the shaft torque and generator speed, and consequently in the voltage seen by the power electronics and so compromising the export power quality. Conversely, grid frequency and voltage changes can also cause the generator speed to change, resulting in changes to the shaft speed and torque and consequently changes to the hydrodynamics acting on the blades. Clearly, fully integrated, bi-directional, models are needed. Here we present two fully coupled models which use different approaches to model the hydrodynamics of rotor blades. The first model uses the Blade Element Momentum Theory (BEMT), resulting in an efficient tool for turbine designers. The second model also uses BEMT, combines this with an actuator line model of the blades coupled to an unsteady computational fluid dynamics simulation by OpenFOAM (CFD/BEMT). Each model is coupled to an OpenModelica model of the electro-mechanical system by an energy balance to compute the shaft speed. Each coupled system simulates the performance of a 1.2 m diameter, three-bladed horizontal axis tidal turbine tested in the University of Edinburgh FloWave Ocean Energy Research Facility. The turbulent flow around the blades and the mechanical-electrical variables during the stable period of operation are analysed. Time series and tabulated average values of thrust, torque, power, and rotational speed, as well as, electrical variables of generator power, electromagnetic torque, voltage and current are presented for the coupled system simulation. The relationship between the mechanical and electrical variables and the results from both tidal turbine approaches are discussed. Our comparison shows that while the BEMT model provides an effective design tool (leading to slightly more conservative designs), the CFD/BEMT simulations show the turbulence influence in the mechanical and electrical variables which can be especially important in assessing an additional source of stresses in the whole electro-mechanical system (though at an increased computational cost).
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33

Ejechi, Bernard Onyekweli. "Microbial deterioration of partially submerged service timbers in a tropical inter-tidal zone." International Biodeterioration & Biodegradation 51, no. 2 (March 2003): 115–18. http://dx.doi.org/10.1016/s0964-8305(02)00093-8.

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34

Bennett, Matthew R., Silvia Gonzalez, David Huddart, Jason Kirby, and Emma Toole. "Probable Neolithic footprints preserved in inter-tidal peat at Kenfig, South Wales (UK)." Proceedings of the Geologists' Association 121, no. 1 (January 2010): 66–76. http://dx.doi.org/10.1016/j.pgeola.2010.01.002.

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35

Cacabelos, Eva, Gustavo M. Martins, Richard Thompson, Afonso C. L. Prestes, José Manuel N. Azevedo, and Ana I. Neto. "Material type and roughness influence structure of inter-tidal communities on coastal defenses." Marine Ecology 37, no. 4 (March 28, 2016): 801–12. http://dx.doi.org/10.1111/maec.12354.

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36

Cox, Traci Erin, Heather L. Spalding, and Michael S. Foster. "Spatial and temporal variation of diverse inter-tidal algal assemblages in Southwest O‘ahu." Marine Ecology 38, no. 3 (June 2017): e12429. http://dx.doi.org/10.1111/maec.12429.

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37

Mason, D. C., I. J. Davenport, G. J. Robinson, R. A. Flather, and B. S. McCartney. "Construction of an inter-tidal digital elevation model by the ‘Water-Line’ Method." Geophysical Research Letters 22, no. 23 (December 1, 1995): 3187–90. http://dx.doi.org/10.1029/95gl03168.

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38

Chanda, Abhra, Anirban Akhand, Sudip Manna, Sachinandan Dutta, Indrani Das, Sugata Hazra, K. H. Rao, and V. K. Dadhwal. "Measuring daytime CO2 fluxes from the inter-tidal mangrove soils of Indian Sundarbans." Environmental Earth Sciences 72, no. 2 (November 30, 2013): 417–27. http://dx.doi.org/10.1007/s12665-013-2962-2.

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39

Ibrahim, Elsy, and Jaak Monbaliu. "Suitability of spaceborne multispectral data for inter-tidal sediment characterization: A case study." Estuarine, Coastal and Shelf Science 92, no. 3 (May 2011): 437–45. http://dx.doi.org/10.1016/j.ecss.2011.01.017.

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40

Devi, Gadi Subhadra, and K. P. Rajashekhar. "Annual shifts in inter-tidal foraminiferal diversity in the west coast of India." Anuário do Instituto de Geociências 29, no. 1 (January 1, 2006): 534–35. http://dx.doi.org/10.11137/2006_1_534-535.

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41

Hulot, O., M. Jaouen, J. B. Barreau, Y. Bernard, Q. Petit, R. Gaugne, and V. Gouranton. "STUDY OF A WRECK IN FORESHORE CONTEXT." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XL-5/W5 (April 9, 2015): 131–38. http://dx.doi.org/10.5194/isprsarchives-xl-5-w5-131-2015.

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We present the study of a wreck, in a foreshore area, in the North of Brittany, France, using two different digitization methods, photogrammetry and laser scanning. The digitization process had to deal with the tide constraints. The 3D data produced using these technologies has been deployed in a large immersive infrastructure dedicated to virtual reality research, in order to propose new practises for archaeologists. <br><br> The overall purpose of our research project is to define an innovative and efficient methodology for the study and preservation of cultural heritage in an inter-tidal context. In the inter-tidal context, heritage is really fragile and the risk of destruction is real (storms, erosion, coastal development...). The traditional methods are no longer efficient. This paper describes preliminary results, through the joint work of a research institute specialized in underwater archaeology, a research laboratory of archaeology and archaeosciences, and a research laboratory in computer science.
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42

Draper, Scott, Thomas A. A. Adcock, Alistair G. L. Borthwick, and Guy T. Houlsby. "An electrical analogy for the Pentland Firth tidal stream power resource." Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences 470, no. 2161 (January 8, 2014): 20130207. http://dx.doi.org/10.1098/rspa.2013.0207.

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Several locations in the Pentland Firth, UK, have been earmarked for the deployment of separate farms of tidal turbines. However, recent numerical modelling suggests that these farms will be inter-dependent and that they must work together to optimize their collective performance. To explain this inter-dependence, in this paper we develop an electrical circuit analogy to describe flow through the Pentland Firth, in which parallel connections in the circuit represent different sub-channels formed by the islands of Swona, Stroma and the Pentland Skerries. The analogy is introduced in stages, beginning with turbines placed in a single channel, then turbines placed in a sub-channel connected in parallel to another sub-channel, and finally more complicated arrangements, in which turbines are installed both in parallel and in series within a multiply connected channel. The analogy leads to a general formula to predict the tidal power potential of turbines placed in a sub-channel connected in parallel to another sub-channel, and a predictive model for more complicated multiply connected channel arrangements. Power estimates made using the formula and predictive model (which may be applied using only measurements of the undisturbed natural tidal hydrodynamics) are shown to agree well with numerical model predictions for the Pentland Firth, providing useful insight into how to best develop the resource.
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43

Xiong, C., and H. Lühr. "Nonmigrating tidal signatures in the magnitude and the inter-hemispheric asymmetry of the equatorial ionization anomaly." Annales Geophysicae 31, no. 6 (June 27, 2013): 1115–30. http://dx.doi.org/10.5194/angeo-31-1115-2013.

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Abstract. Based on nine years of observations from the satellites CHAMP and GRACE the tidal signatures in the magnitude and the inter-hemisphere asymmetry of the equatorial ionization anomaly (EIA) have been investigated in this study. The EIA magnitude parameters show longitudinal wavenumber 4 and 3 (WN4/WN3) patterns during the months around August and December, respectively, while for different EIA parameters the contributions of the various tidal parameters are different. For the crest-to-trough ratio (CTR) the dominating nonmigrating tidal component contributing to WN4 is DE3 during the months around August, while during the months around December solstice the stationary planetary wave, SPW3, takes a comparable role to DE2 in contributing to WN3. For the apex height index (ApexHC) of the EIA fluxtube the stationary planetary waves, SPW4/SPW3, exceed the amplitudes of DE3/DE2 taking the leading role in causing the longitudinal WN4/WN3 patterns. During the months around December solstice the SW3 tide is prominent in both CTR and ApexHC. SW3 shows a strong dependence on the solar flux level, while it is hardly dependent on magnetic activity. For the EIA inter-hemispheric asymmetry only WN1 and WN2 longitudinal patterns can be seen. During June solstice months the pattern can be explained by stationary planetary waves SPW1 and SPW2. Conversely, around December solstice months longitudinal features exhibit some local time evolution, in particular the diurnal nonmigrating tide D0 takes the leading role.
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44

Yam, Rita S. W., Yen-Tzu Fan, Zhehan Tan, Tzu-Dan Wang, and Chiu-Yu Chiu. "Assessing Impacts of Metallic Contamination along the Tidal Gradient of a Riverine Mangrove: Multi-metal Bioaccumulation and Biomagnification of Filter-Feeding Bivalves." Forests 11, no. 5 (May 1, 2020): 504. http://dx.doi.org/10.3390/f11050504.

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Most riverine mangroves (characterized by salinity fluctuations and tidal inundations), are seriously threatened by metallic pollution. Whether differences in salinity and tidal effects along the river continuum can affect metallic bioaccumulation and the biomagnification of species is still unknown. Bivalves are representative sessile inhabitants in mangrove ecosystems, with a high capacity to bioaccumulate metallic contaminants. The present study used two bivalves, Meretrix lusoria and Mytilopsis sallei, to monitor inter-site changes in metallic contamination and assess the associated ecological impacts along the tidal gradients of riverine mangroves. The concentrations of a total of six metals (Cr, Ni, Cu, Zn, Cd and Pb) in M. lusoria and M. sallei, collected at three different sites along Danshuei Riverine Mangrove, were investigated. The metallic concentrations of the whole soft body of the studied bivalves, and the associated surface sediment from each site, were analyzed using inductively coupled plasma mass spectrometry (ICP-MS) to determine the inter-site effects on the bioaccumulation and biomagnification of metallic contaminants in bivalves. There are increasing concentrations of four metallic contaminants, Zn, Cr, Cd and Cu, in the seaward direction of the bivalves. The increasing mean metallic concentrations along the seaward direction may be the effect of salinity, further decreasing the rate of the elimination of these metals, thus resulting in a net increase in metallic contaminants. Our results clearly show prominent inter-site changes in the metallic burdens of bivalves in our study on riverine mangrove ecosystems associated with different levels of bioaccumulation and biomagnification of metallic contaminants. Thus, it is important to monitor multiple sites along the dynamic environment of riverine mangroves in order to gain a good understanding of the ecological impact of metallic pollution risks. The present findings provide important evidence of the use of simple indices to assess the ecological impacts of metallic pollution in riverine mangroves.
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45

Rosenquist, Shawn E., and Christopher J. Hintz. "Supporting Coastal Resiliency by Investigating Tidal Reach and Inter-Connected Factors in Coastal Georgia." Journal of South Carolina Water Resources, no. 6 (January 1, 2020): 3–17. http://dx.doi.org/10.34068/jscwr.06.01.

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Increasing our understanding of the tidal dynamics, the extent of tidal reach, and storm surge impacts on near-coastal areas of Georgia and South Carolina rivers is a significant research opportunity. It has the potential to yield benefits to sustainable planning, ecosystem protection, and risk management for regulators and state agencies, local municipalities, coastal residents, and other regional stakeholders. This study leveraged existing United States Geological Survey (USGS) water level data for the Savannah River, added additional water level gauges in key areas for less than one year, and analyzed these combined large data sets with modified wavelet analysis and Fourier analysis. One significant outcome of the research included confirmation of river mile 45, historically referred to as Ebenezer Landing, as the head of tide. We also provide information on the dynamics of wave propagation through the near-coastal area of the Savannah River, give indication of critical areas of concern for flooding resulting from interactions between the interconnected factors affecting elevated upstream flows and storm tides, and discuss relevance of study results for various stakeholders.
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46

White, Gemma E., Grant C. Hose, and Culum Brown. "Influence of rock-pool characteristics on the distribution and abundance of inter-tidal fishes." Marine Ecology 36, no. 4 (November 27, 2014): 1332–44. http://dx.doi.org/10.1111/maec.12232.

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47

Shanks, Alan L., Peter Sheesley, and Leyia Johnson. "Phytoplankton subsidies to the inter-tidal zone are strongly affected by surf-zone hydrodynamics." Marine Ecology 38, no. 3 (June 2017): e12441. http://dx.doi.org/10.1111/maec.12441.

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48

Lindahl, Patric, Paul Worsfold, Miranda Keith-Roach, Morten B. Andersen, Peter Kershaw, Kins Leonard, Min-Seok Choi, Dominique Boust, and Patrick Lesueur. "Temporal record of Pu isotopes in inter-tidal sediments from the northeastern Irish Sea." Science of The Total Environment 409, no. 23 (November 2011): 5020–25. http://dx.doi.org/10.1016/j.scitotenv.2011.08.019.

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49

Jayasiri, H. B., A. Vennila, and C. S. Purushothaman. "Spatial and temporal variability of metals in inter-tidal beach sediment of Mumbai, India." Environmental Monitoring and Assessment 186, no. 2 (September 25, 2013): 1101–11. http://dx.doi.org/10.1007/s10661-013-3441-7.

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50

de Vries, J. J., H. Ridderinkhof, L. R. M. Maas, and H. M. van Aken. "Intra- and inter-tidal variability of the vertical current structure in the Marsdiep basin." Continental Shelf Research 93 (February 2015): 39–57. http://dx.doi.org/10.1016/j.csr.2014.12.002.

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