Bibliografias temáticas / The Tides Of Time

Literatura científica selecionada sobre o tema "The Tides Of Time"

Autor: Grafiati

Publicado: 26 de julho de 2024

Última modificação: 27 de julho de 2024

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Artigos de revistas sobre o assunto "The Tides Of Time"

Agnew, Duncan C. "Time and tide: pendulum clocks and gravity tides". History of Geo- and Space Sciences 11, n.º 2 (16 de setembro de 2020): 215–24. http://dx.doi.org/10.5194/hgss-11-215-2020.

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Abstract. Tidal fluctuations in gravity will affect the period of a pendulum and hence the timekeeping of any such clock that uses one. Since pendulum clocks were, until the 1940s, the best timekeepers available, there has been interest in seeing if tidal effects could be observed in the best performing examples of these clocks. The first such observation was in 1929, before gravity tides were measured with spring gravimeters; at the time of the second (1940–1943), such gravimeters were still being developed. Subsequent observations, having been made after pendulum clocks had ceased to be the best available timekeepers and after reliable gravimeter measurements of tides, have been more of an indication of clock quality than a contribution to our knowledge of tides. This paper describes the different measurements and revisits them in terms of our current knowledge of Earth tides. Doing so shows that clock-based systems, though noisier than spring gravimeters, were an early form of an absolute gravimeter that could indeed observe Earth tides.

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Link, Denise, e Lois Wessel. "Time and Tides". Journal for Nurse Practitioners 18, n.º 4 (abril de 2022): 351–52. http://dx.doi.org/10.1016/j.nurpra.2022.02.021.

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Melchior, Paul. "Tides in our time". Nature 398, n.º 6723 (março de 1999): 119–20. http://dx.doi.org/10.1038/18153.

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Ray, Richard D., e David E. Cartwright. "Times of peak astronomical tides". Geophysical Journal International 168, n.º 3 (março de 2007): 999–1004. http://dx.doi.org/10.1111/j.1365-246x.2006.03293.x.

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Dawes, Kwame, e Jared Angira. "Tides of Time: Selected Poems". World Literature Today 71, n.º 4 (1997): 851. http://dx.doi.org/10.2307/40153466.

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Zaron, Edward D., e Gary D. Egbert. "Time-Variable Refraction of the Internal Tide at the Hawaiian Ridge". Journal of Physical Oceanography 44, n.º 2 (1 de fevereiro de 2014): 538–57. http://dx.doi.org/10.1175/jpo-d-12-0238.1.

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Abstract The interaction of the dominant semidiurnal M2 internal tide with the large-scale subtidal flow is examined in an ocean model by propagating the tide through an ensemble of background fields in a domain centered on the Hawaiian Ridge. The background fields are taken from the Simple Ocean Data Assimilation (SODA) ocean analysis, at 2-month intervals from 1992 through 2001. Tides are computed with the Primitive Equation Z-coordinate Harmonic Analysis of Tides (PEZ-HAT) model by 14-day integrations using SODA initial conditions and M2 tidal forcing. Variability of the tide is found to occur primarily as the result of propagation through the nonstationary background fields, rather than via generation site variability. Generation of incoherent tidal variability is mapped and shown to occur mostly in association with waves generated at French Frigate Shoals scattering near the Musicians Seamounts to the north of the ridge. The phase-coherent internal tide loses energy at a domain-average rate of 2 mW m−2 by scattering into the nonstationary tide. Because of the interference of waves from multiple generation sites, variability of the internal tide is spatially inhomogeneous and values of the scattering rate 10 times larger occur in localized areas. It is estimated that 20% of the baroclinic tidal energy flux is lost by adiabatic scattering (refraction) within 250 km of the ridge, a value regarded as a lower bound because of the smoothed nature of the SODA fields used in this study.

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Gao, Guanghai, Junqiang Xia, Roger A. Falconer e Yingying Wang. "Modelling Study of Transport Time Scales for a Hyper-Tidal Estuary". Water 12, n.º 9 (30 de agosto de 2020): 2434. http://dx.doi.org/10.3390/w12092434.

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This paper presents a study of two transport timescales (TTS), i.e., the residence time and exposure time, of a hyper-tidal estuary using a widely used numerical model. The numerical model was calibrated against field measured data for various tidal conditions. The model simulated current speeds and directions generally agreed well with the field data. The model was then further developed and applied to study the two transport timescales, namely the exposure time and residence time for the hyper-tidal Severn Estuary. The numerical model predictions showed that the inflow from the River Severn under high flow conditions reduced the residence and exposure times by 1.5 to 3.5% for different tidal ranges and tracer release times. For spring tide conditions, releasing a tracer at high water reduced the residence time and exposure time by 49.0% and 11.9%, respectively, compared to releasing the tracer at low water. For neap tide conditions, releasing at high water reduced the residence time and exposure time by 31.6% and 8.0%, respectively, compared to releasing the tracer at low water level. The return coefficient was found to be vary between 0.75 and 0.88 for the different tidal conditions, which indicates that the returning water effects for different tidal ranges and release times are all relatively high. For all flow and tide conditions, the exposure times were significantly greater than the residence times, which demonstrated that there was a high possibility for water and/or pollutants to re-enter the Severn Estuary after leaving it on an ebb tide. The fractions of water and/or pollutants re-entering the estuary for spring and neap tide conditions were found to be very high, giving 0.75–0.81 for neap tides, and 0.79–0.88 for spring tides. For both the spring and neap tides, the residence and exposure times were lower for high water level release. Spring tide conditions gave significantly lower residence and exposure times. The spatial distribution of exposure and residence times showed that the flow from the River Severn only had a local effect on the upstream part of the estuary, for both the residence and exposure time.

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Hart-Davis, Michael G., Denise Dettmering, Roman Sulzbach, Maik Thomas, Christian Schwatke e Florian Seitz. "Regional Evaluation of Minor Tidal Constituents for Improved Estimation of Ocean Tides". Remote Sensing 13, n.º 16 (21 de agosto de 2021): 3310. http://dx.doi.org/10.3390/rs13163310.

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Satellite altimetry observations have provided a significant contribution to the understanding of global sea surface processes, particularly allowing for advances in the accuracy of ocean tide estimations. Currently, almost three decades of satellite altimetry are available which can be used to improve the understanding of ocean tides by allowing for the estimation of an increased number of minor tidal constituents. As ocean tide models continue to improve, especially in the coastal region, these minor tides become increasingly important. Generally, admittance theory is used by most global ocean tide models to infer several minor tides from the major tides when creating the tidal correction for satellite altimetry. In this paper, regional studies are conducted to compare the use of admittance theory to direct estimations of minor tides from the EOT20 model to identify which minor tides should be directly estimated and which should be inferred. The results of these two approaches are compared to two global tide models (TiME and FES2014) and in situ tide gauge observations. The analysis showed that of the eight tidal constituents studied, half should be inferred (2N2, ϵ2, MSF and T2), while the remaining four tides (J1, L2, μ2 and ν2) should be directly estimated to optimise the ocean tidal correction. Furthermore, for certain minor tides, the other two tide models produced better results than the EOT model, suggesting that improvements can be made to the tidal correction made by EOT when incorporating tides from the two other tide models. Following on from this, a new approach of merging tidal constituents from different tide models to produce the ocean tidal correction for satellite altimetry that benefits from the strengths of the respective models is presented. This analysis showed that the tidal correction created based on the recommendations of the tide gauge analysis provided the highest reduction of sea-level variance. Additionally, the combination of the EOT20 model with the minor tides of the TiME and FES2014 model did not significantly increase the sea-level variance. As several additional minor tidal constituents are available from the TiME model, this opens the door for further investigations into including these minor tides and optimising the tidal correction for improved studies of the sea surface from satellite altimetry and in other applications, such as gravity field modelling.

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Ferraz-Mello, S. "On Tides and Exoplanets". Proceedings of the International Astronomical Union 15, S364 (outubro de 2021): 20–30. http://dx.doi.org/10.1017/s1743921322000059.

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AbstractThis paper reviews the basic equations used in the study of the tidal variations of the rotational and orbital elements of a system formed by one star and one close-in planet as given by the creep tide theory and Darwin’s constant time lag (CTL) theory. At the end, it reviews and discusses the determinations of the relaxation factors (and time lags) in the case of host stars and hot Jupiters based on actual observations of orbital decay, stellar rotation and age, etc. It also includes a recollection of the basic facts concerning the variations of the rotation of host stars due to the leakage of angular momentum associated with stellar winds.

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Allbrooke, Jill. "The Life and Times of Time and Tide". Serials: The Journal for the Serials Community 8, n.º 1 (1 de março de 1995): 72–75. http://dx.doi.org/10.1629/0872.

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Teses / dissertações sobre o assunto "The Tides Of Time"

Li, Tak-wai Wilson. "Forecasting of tide heights : an application of smoothness priors in time series modelling /". [Hong Kong] : University of Hong Kong, 1991. http://sunzi.lib.hku.hk/hkuto/record.jsp?B13154357.

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Li, Tak-wai Wilson, e 李德煒. "Forecasting of tide heights: an application of smoothness priors in time series modelling". Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 1991. http://hub.hku.hk/bib/B3121048X.

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Coughenour, Christopher Lynn Lacovara Kenneth J. "An analysis of cyclic tidal deposits : statistical time series properties, extraction of earth-moon parameters, and observed intertidal sedimentation /". Philadelphia, Pa. : Drexel University, 2009. http://hdl.handle.net/1860/3135.

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Wai, Siu-wah. "Red tides : a detrimentall threat to the environment /". Hong Kong : University of Hong Kong, 1998. http://sunzi.lib.hku.hk/hkuto/record.jsp?B20038203.

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Kemp, Kirsty M. "Temporal dynamics in the deep sea : time-series at food falls, seasonality in condition of grenadiers, and tides as time signals". Thesis, University of Aberdeen, 2006. http://digitool.abdn.ac.uk/R?func=search-advanced-go&find_code1=WSN&request1=AAIU222698.

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The deep demersal community of the bathyal Porcupine Seabight is subject to environmental forcing on diel, seasonal and annual scales, in addition to the stochastic and transient influence of nutritional windfalls from the photic zone. The current regime at bathyal depth in the Porcupine Seabight is characterised by oscillations in current flow with periods of 12.4h and 14.8d. Increased current velocity and particle suspension in summer months synchronises well with the seasonal input of phytoplankton to the seafloor. These physical characteristics may constitute time signals in the deep ocean environment. Consumption and succession processes at bathyal food falls in the North Atlantic are suggestive of a fundamental difference in the community response between the North Atlantic and North Pacific oceans. The sinking of small cetacean carcasses constitutes a transient environmental impact on the local community structure which is not limited to the scavenging fauna. There is limited evidence of a response to the seasonal increase in available organic carbon in the white muscle of North Atlantic macrourids. This is in accordance with results from Pacific macrourids and suggests that the seasonal food pulse, experienced by the deep benthos under productive surface waters, is not greatly manifested at higher trophic levels. The successful adaptation of existing baited camera technology to incorporate an autonomous periodic bait-release system has enabled long-term high frequency time-series observations of deep-sea scavenging demersal fish and crustaceans to be made for the first time. An understanding of temporal environmental cues, and of the resultant interactions between organisms and their environment, effectively pervades the study of any aspect of organismal or population ecology.

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Devlin, Adam Thomas. "On the variability of Pacific Ocean tides at seasonal to decadal time scales| Observed vs modelled". Thesis, Portland State University, 2016. http://pqdtopen.proquest.com/#viewpdf?dispub=10128376.

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Ocean tides worldwide have exhibited secular changes in the past century, simultaneous with a global secular rise in mean sea level (MSL). The combination of these two factors contributes to higher water levels, and may increase threats to coastal regions and populations over the next century. Equally as important as these long-term changes are the short-term fluctuations in sea levels and tidal properties. These fluctuations may interact to yield locally extreme water level events, especially when combined with storm surge. This study, presented in three parts, examines the relationships between tidal anomalies and MSL anomalies on yearly and monthly timescales, with a goal of diagnosing dynamical factors that may influence the long-term evolution of tides in the Pacific Ocean. Correlations between yearly averaged properties are denoted tidal anomaly trends (TATs), and will be used to explore interannual behavior. Correlations of monthly averaged properties are denoted seasonal tidal anomaly trends (STATs), and are used to examine seasonal behavior. Four tidal constituents are analyzed: the two largest semidiurnal (twice daily) constituents, M2 and S2, and the two largest diurnal (once daily) constituents, K1 and O1.

Part I surveys TATs and STATs at 153 Pacific Ocean tide gauges, and discusses regional patterns within the entire Pacific Ocean. TATs with statistically significant relations between MSL and amplitudes (A-TATs) are seen at 89% of all gauges; 92 gauges for M2, 66 for S2, 82 for K1, and 59 for O1. TATs with statistically significant relations between tidal phase (the relative timing of high water of the tide) and MSL (P-TATs) are observed at 55 gauges for M2, 47 for S2, 42 for K1, and 61 for O1. Significant seasonal variations (STATs) are observed at about a third of all gauges, with the largest concentration in Southeast Asia. The effect of combined A-TATs was also considered. At selected stations, observed tidal sensitivity with MSL was extrapolated forward in time to the predicted sea level in 2100. Results suggest that stations with large positive combined A-TATs produce total water levels that are greater than those predicted by an increase in MSL alone, increasing the chances of high-water events.

Part II examines the mechanisms behind the yearly (TAT) variability in the Western Tropical Pacific Ocean. Significant amplitude TATs are found at more than half of 26 gauges for each of the two strongest tidal constituents, K1 (diurnal) and M2 (semidiurnal). For the lesser constituents analyzed (O1 and S2), significant trends are observed at ten gauges.

Part III analyzes the seasonal behavior of tides (STATs) at twenty tide gauges in the Southeast Asian waters, which exhibit variation by 10 – 30% of mean tidal amplitudes. A barotropic ocean tide model that considers the seasonal effects of MSL, stratification, and geostrophic and Ekman velocity is used to explain the observed seasonal variability in tides due to variations in monsoon-influenced climate forcing, with successful results at about half of all gauges. The observed changes in tides are best explained by the influence of non-tidal velocities (geostrophic and Ekman), though the effect of changing stratification is also an important secondary causative mechanism.

From the results of these surveys and investigations, it is concluded that short-term fluctuations in MSL and tidal properties at multiple time scales may be as important in determining the state of future water levels as the long-term trends. Global explanations for the observed tidal behavior have not been found in this study; however, significant regional explanations are found at the yearly time scale in the Solomon Sea, and at the seasonal time scale in Southeast Asia. It is likely that tidal sensitivity to annual and seasonal variations in MSL at other locations also are driven by locally specific processes, rather than factors with basin-wide coherence. (Abstract shortened by ProQuest.)

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Geißler, Christoph, e Ch Jacobi. "Forcing of the Quarterdiurnal Tide". Universität Leipzig, 2018. https://ul.qucosa.de/id/qucosa%3A31792.

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Ensemble calculations for the period from 2000 to 2010 were carried out with the middle and upper atmosphere model (MUAM), and an analysis of the quarterdiurnal tide is performed. The global temporal and latitudinal distributions of the quarterdiurnal tide are modeled with MUAM, and their forcing mechanisms are examined. The quarterdiurnal tides show a similar distribution over the year in the northern and southern hemisphere, with maxima of the amplitude in late winter and spring as well as in autumn. In the latitude-height distribution is also shown that the largest amplitudes of the quarterdiurnal tide are seen at midlatitudes. Due to the decreasing density with height, there is a general increase of the tidal amplitudes with height. The results of the forcing analyses show that direct solar forcing is most important, but also that non-linear forcing and gravity wave interaction with other tides have a non-negligible influence on the quarterdiurnal tide in the middle and upper atmosphere.
Mit dem Modell für die mittlere und obere Atmosphäre MUAM wurden Ensemble-Berechnungen für den Zeitraum 2000 bis 2010 durchgeführt und die vierteltägigen Gezeiten analysiert. Es wird auf die globale zeitliche und räumliche Verteilung der vierteltägigen Gezeiten eingegangen und deren Anregungsmechanismen untersucht. Die vierteltägigen Gezeiten zeigen einen ähnlichen Verlauf über das Jahr auf der Nord- und Südhalbkugel mit Maxima der Amplitude im späten Winter und Frühjahr sowie im Herbst. Ein ähnliches Bild zeigt sich auch für die Verteilung im Breiten-Höhen-Schnitt, wo die größten Amplituden der vierteltätigen Gezeiten in den mittleren Breiten zu finden sind. Aufgrund der abnehmenden Dichte mit der Höhe ist eine allgemeine Zunahme der Amplituden mit der Höhe zu beobachten. Es zeigte sich, dass der direkte solare Antrieb am stärksten ausgeprägt ist, aber auch, dass der nichtlinearer Antrieb und die Interaktion von Schwerewellen mit anderen Gezeiten einen nicht zu vernachlässigenden Einfluss auf die vierteltägigen Gezeiten in der mittleren und oberen Atmosphäre haben.

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Haselmaier, Lawrence H. "Computation of a Virtual Tide Corrector to Support Vertical Adjustment of Autonomous Underwater Vehicle Multibeam Sonar Data". ScholarWorks@UNO, 2015. http://scholarworks.uno.edu/td/2080.

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One challenge for Autonomous Underwater Vehicle (AUV) multibeam surveying is the limited ability to assess internal vertical agreement rapidly and reliably. Applying an external ellipsoid reference to AUV multibeam data would allow for field comparisons. A method is established to merge ellipsoid height (EH) data collected by a surface vessel in close proximity to the AUV. The method is demonstrated over multiple collection missions in two separate areas. Virtual tide corrector values are derived using EH data collected by a boat and a measured ellipsoid to chart datum separation distance. Those values are compared to measurements by a traditional tide gauge installed nearby. Results from the method had a mean difference of 6 centimeters with respect to conventional data and had a mean total propagated uncertainty of 15 centimeters at the 95% confidence interval. Methodologies are examined to characterize their accuracies and uncertainty contribution to overall vertical correction.

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Ho, Kin-chung. "Subtropical red tides and their ecological significance in Hong Kong waters /". [Hong Kong : University of Hong Kong], 1991. http://sunzi.lib.hku.hk/hkuto/record.jsp?B12997213.

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Wai, Siu-wah, e 衛兆華. "Red tides: a detrimentall threat to the environment". Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 1998. http://hub.hku.hk/bib/B31254135.

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Livros sobre o assunto "The Tides Of Time"

Dove, Jane. Time and tide. London: Hodder & Stoughton, 1995.

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Brasch, Nicolas. Times, tides, and revolutions. Mankato, Minn: Smart Apple Media, 2011.

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Bottoms, Bill. Time and tides. Place of publication not identified]: [Heins Publications], 2008.

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Tides in time: Photographs. Santa Monica, Calif: Photo Department, 1996.

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Angira, Jared. Tides of time: Selected poems. Nairobi: East African Educational Publishers, 1996.

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Christopherson, Anne. Greenwich - time and tides: Paintings. London: Unicorn Press, 2001.

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Guru, Giridhari Prasad. The tides of time: A memoir. Bhubaneswar: Geeta Guru, 2003.

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Azuike, Amaka. Tides of time: A collection of poems. Jos, Nigeria: Mazlink Nigeria, 2000.

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Trust, Mumbai Port, ed. Tides of time: History of Mumbai Port. Mumbai: Mumbai Port Trust, 2000.

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McKay, Shirley. Time & tide. Edinburgh: Polygon, 2012.

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Capítulos de livros sobre o assunto "The Tides Of Time"

Smith, Philip M. "The Admiralty Tide Tables". In Tides, 17–21. First edition. | Routledge : Abingdon, Oxon ; New York, NY, [2018]: Routledge, 2018. http://dx.doi.org/10.4324/9781315561110-2.

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Tamura, Yoshiaki. "Analysis of Earth Tides Data". In The Practice of Time Series Analysis, 327–39. New York, NY: Springer New York, 1999. http://dx.doi.org/10.1007/978-1-4612-2162-3_20.

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Poli, Roberto. "Time and Times". In Introduction to Anticipation Studies, 139–66. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-63023-6_8.

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Zilboorg, Caroline. "Time and tide". In The Life of Gregory Zilboorg, 1940–1959, 240–63. London: Routledge, 2021. http://dx.doi.org/10.4324/9781003190974-9.

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Naicker, Kamil. "Time and Tide". In Women and Water in Global Fiction, 155–70. New York: Routledge, 2023. http://dx.doi.org/10.4324/9780429298837-11.

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Albritton, Robert. "Conclusion: “Time and Tides Wait for No One”". In Palgrave Insights into Apocalypse Economics, 115–22. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-05183-9_9.

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Southerton, Dale. "Time: Gershuny’s Changing Times". In Doing Social Science, 59–79. London: Macmillan Education UK, 2009. http://dx.doi.org/10.1007/978-1-137-02054-3_4.

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"Time and tides". In Physics to a Degree, 203–4. CRC Press, 2018. http://dx.doi.org/10.1201/9781315273839-19b.

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"TIMES AND TIDES". In Chan Insights and Oversights, 175–94. Princeton University Press, 2020. http://dx.doi.org/10.2307/j.ctv14164rh.11.

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"CHAPTER SIX Times and Tides". In Chan Insights and Oversights, 175–94. Princeton University Press, 1993. http://dx.doi.org/10.1515/9780691218106-009.

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Trabalhos de conferências sobre o assunto "The Tides Of Time"

Афанасьев, В., e V. Afanas'ev. "MORPHODYNAMICS OF COASTAL TIDAL SUBARCTIC SEAS AFTER A STABLE TRANSITION OF AVERAGE DAILY TEMPERATURE THROUGH 0 AND COASTAL PROTECTION". In Sea Coasts – Evolution ecology, economy. Academus Publishing, 2018. http://dx.doi.org/10.31519/conferencearticle_5b5ce387b8bb03.63862372.

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It was noted that in a homogeneous coastal bluffs, the beach at comparable settings (the basic structure of the wave energy dissipation), and hydrodynamic effects (tides, surges, long waves and wind), the most intense erosion occurs in November–January. During this period, at the upper levels of the coastal profile, which are equilibrium for storm conditions with maximum tides, beach sediments are freezing and the consequent deterioration of their dissipation properties. Loss of redistribution of snow and blizzard in the profile essentially simulates morphodynamics beach properties at this time.

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Spitz, Andreas, Jannik Strötgen, Thomas Bögel e Michael Gertz. "Terms in Time and Times in Context". In WWW '15: 24th International World Wide Web Conference. New York, NY, USA: ACM, 2015. http://dx.doi.org/10.1145/2740908.2741693.

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Venkateswaran, Sriram, e Upamanyu Madhow. "Space-time localization using times of arrival". In 2011 49th Annual Allerton Conference on Communication, Control, and Computing (Allerton). IEEE, 2011. http://dx.doi.org/10.1109/allerton.2011.6120351.

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Martins, P. Medina. "Toys, toddlers and the times of time". In The first international conference on computing anticipatory systems. AIP, 1998. http://dx.doi.org/10.1063/1.56333.

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Zhao, Xin, Gilles Goncalves e Remy Dupas. "Dynamic Vehicle Routing Problem with real-time time-dependent travel times". In 2009 IEEE Intelligent Vehicles Symposium (IV). IEEE, 2009. http://dx.doi.org/10.1109/ivs.2009.5164383.

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Kodaira, Tsubasa, Natacha Bernier e Keith R. Thompson. "Application of the Spectral Nudging on Global Tides Towards a Global Total Water Level Prediction System". In ASME 2019 38th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2019. http://dx.doi.org/10.1115/omae2019-95842.

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Abstract With the long-term goal of developing an ensemble forecast system for coastal flooding, we are developing a dynamically-based, numerical model of the global ocean. The model is based on the NEMO framework and has been used to predict global tides and surges in previous studies. This study focuses on the optimization of the joint prediction of both tides and surges, the two main components of total water level that cause coastal flooding. To improve the predictions of the tide we use a modified form of “spectral nudging”. We show this leads to significant improvements in the prediction of the M2 tide in the open ocean, and also in the shallow regions closer to shore where the model is not nudged. The median value of the vector difference of the tidal amplitude based on sea level observations and a data-assimilative model, and the predictions of our ocean model, is reduced from 11.2 cm to 2.66 cm by the nudging. The improvement deteriorates significantly however if additional tidal constituents are included in the model (most notably S2). This is explained in terms of spectral leakage between tidal bands associated with the nudging methodology and a straightforward solution is proposed.

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Kurland, Oren. "Session details: Session 8b: time and tide". In SIGIR '14: The 37th International ACM SIGIR Conference on Research and Development in Information Retrieval. New York, NY, USA: ACM, 2014. http://dx.doi.org/10.1145/3255819.

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Kherani, Arzad A. "Sojourn times in (discrete) time shared systems and their continuous time limits". In the 1st international conference. New York, New York, USA: ACM Press, 2006. http://dx.doi.org/10.1145/1190095.1190099.

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Tiong, KahYong, Zhenliang Ma e Carl-William Palmqvist. "Real-time Train Arrival Time Prediction at Multiple Stations and Arbitrary Times". In 2022 IEEE 25th International Conference on Intelligent Transportation Systems (ITSC). IEEE, 2022. http://dx.doi.org/10.1109/itsc55140.2022.9922299.

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Jones, B. F., e J. Wegener. "Measurement of extreme execution times for software". In IEE Colloquium on Real-Time Systems. IEE, 1998. http://dx.doi.org/10.1049/ic:19980525.

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Relatórios de organizações sobre o assunto "The Tides Of Time"

Devlin, Adam. On the Variability of Pacific Ocean Tides at Seasonal to Decadal Time Scales: Observed vs Modelled. Portland State University Library, janeiro de 2000. http://dx.doi.org/10.15760/etd.2920.

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Torres, Marissa, e Norberto Nadal-Caraballo. Rapid tidal reconstruction with UTide and the ADCIRC tidal database. Engineer Research and Development Center (U.S.), agosto de 2021. http://dx.doi.org/10.21079/11681/41503.

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The quantification of storm surge is vital for flood hazard assessment in communities affected by coastal storms. The astronomical tide is an integral component of the total still water level needed for accurate storm surge estimates. Coastal hazard analysis methods, such as the Coastal Hazards System and the StormSim Coastal Hazards Rapid Prediction System, require thousands of hydrodynamic and wave simulations that are computationally expensive. In some regions, the inclusion of astronomical tides is neglected in the hydrodynamics and tides are instead incorporated within the probabilistic framework. There is a need for a rapid, reliable, and accurate tide prediction methodology to provide spatially dense reconstructed or predicted tidal time series for historical, synthetic, and forecasted hurricane scenarios. A methodology is proposed to combine the tidal harmonic information from the spatially dense Advanced Circulation hydrodynamic model tidal database with a rapid tidal reconstruction and prediction program. In this study, the Unified Tidal Analysis program was paired with results from the tidal database. This methodology will produce reconstructed (i.e., historical) and predicted tidal heights for coastal locations along the United States eastern seaboard and beyond and will contribute to the determination of accurate still water levels in coastal hazard analysis methods.

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Sevilla, Almudena, Angus Phimister, Sonya Krutikova, Christine Farquharson e Sarah Cattan. Trying times: how might the lockdown change time use in families? Institute for Fiscal Studies, abril de 2020. http://dx.doi.org/10.1920/bn.ifs.2020.bn0284.

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Dinkelman, Taryn, e L. Rachel Ngai. Time Use and Gender in Africa in Times of Structural Transformation. Cambridge, MA: National Bureau of Economic Research, dezembro de 2021. http://dx.doi.org/10.3386/w29571.

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Brill, Percy H., e Carl M. Harris. Waiting Times for M/G/1 Queues with Service-Time-Dependent Server Vacations. Fort Belvoir, VA: Defense Technical Information Center, junho de 1989. http://dx.doi.org/10.21236/ada209597.

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Davidson, D. F., M. A. Oehlschiaeger, J. T. Herbon e R. K. Hanson. Shock Tube Measurements Of Iso-Octane Ignition Times And OH Concentration Time Histories. Fort Belvoir, VA: Defense Technical Information Center, janeiro de 2002. http://dx.doi.org/10.21236/ada422570.

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Arhin, Stephen. Predicting Acceptable Wait Times for Patrons at Transit Bus Stops by Time of Day. Mineta Transportation Institute, outubro de 2019. http://dx.doi.org/10.31979/mti.2019.1801.

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Hammack, E., e Morgan Johnston. Three-dimensional numerical model study of flow near a scour hole in Isle of Wight Bay near Ocean City, Maryland. Engineer Research and Development Center (U.S.), abril de 2022. http://dx.doi.org/10.21079/11681/43921.

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A scour hole has developed in Isle of Wight Bay near Ocean City, MD. This hole could grow to the point that nearby land developments are threatened, so channel-bed protection measures may be implemented near this scour hole. Appropriately designing those bed protection measures requires knowledge of the flow behavior in the scour hole, so a three-dimensional model study has been conducted to determine the flow behavior at the extreme flood and ebb tides present during a pre-selected month of tide cycles. Steady-state simulations of the flows during those two tide conditions have been completed. Contour plots of the flow velocity near the bed and the corresponding bed shear stresses are provided as input for the design of the bed protection measures.

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Santos, Nierlson, e A. E. Gene Freeman. Adjusting Dairy Yield Records From 3 Times to 2 Time Milking Using a Random Regression Model. Ames (Iowa): Iowa State University, janeiro de 2004. http://dx.doi.org/10.31274/ans_air-180814-939.

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Graziano, Alejandro, Georg Schaur, Christian Volpe Martincus e Jerónimo Carballo. Endogenous Border Times. Inter-American Development Bank, junho de 2016. http://dx.doi.org/10.18235/0011740.

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We examine transaction-level Peruvian import data to show that firms are subject to significant costs of port-of-entry delays. At the transaction level, we observe the time it takes a shipment to clear each step in the entry process. Our theory shows conditions under which observed entry times are endogenous. As a result, total entry delays potentially lead to biased policy conclusions and non-informative efficiency rankings of countries' entry procedures. We make three empirical contributions that help unbundle sources for time costs in trade and border effects. First, we provide evidence that at least part of the total port-entry-time is endogenous. Second, we identify the effect of entry delays on imports based on exogenous necessary entry processing. Third, we provide evidence that trade costs due to entry delays are heterogeneous across firm types. New and large importersare more elastic with respect to entry delays. This information allows researchers and policymakers to interpret aggregate port of entry delay data and their costs across different types of firms.

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