Добірка наукової літератури з теми "Atmospheric tides"

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Пов'язані теми наукових робіт:

Статті в журналах з теми "Atmospheric tides":

1
Palumbo, A. "Atmospheric tides." Journal of Atmospheric and Solar-Terrestrial Physics 60, no. 3 (February 1998): 279–87. http://dx.doi.org/10.1016/s1364-6826(97)00078-3.
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2
Brahde, R. "Lunisolar Atmospheric Tides. III." Australian Journal of Physics 44, no. 1 (1991): 87. http://dx.doi.org/10.1071/ph910087.
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In two earlier papers (Brahde 1988, 1989) the atmospheric tide in Oslo (Norway) was studied using pressure data for 23 continuous years. In the present paper a similar study based on pressure data from Batavia (now Jakarta in Indonesia, latitude 6�08'S, longitude 106�45'E) is presented. The result is that the tidal wave caused by the lunisolar tide is represented by a one-day and a half-day oscillation with mean amplitudes of 0 �11 and 0�33 mb respectively. The amplitude spectrum reveals amplitudes of up to 1 mb of dynamiC origin. The 'thermal' tide is also studied and the connection between the thermal and dynamic effects is discussed.
3
Brahde, R. "Lunisolar Atmospheric Tides. II." Australian Journal of Physics 42, no. 4 (1989): 439. http://dx.doi.org/10.1071/ph890439.
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In an earlier paper (Brahde 1988) it was shown that series of measurements of the atmospheric pressure in Oslo contained information about a one�day oscillation with mean amplitude 0�17 mb. The data consisted of measurements every second hour during the years 1957-67, 1969 and 1977. In the present paper the intervening years plus 1978 and 1979 have been included, increasing the basis from 13 to 23 years. In addition the phase shift occurring when the Moon crosses the celestial equator has been defined precisely, thus making it possible to include all the data.
4
Forbes, Jeffrey M., and Gerald V. Groves. "Atmospheric tides below 80 km." Advances in Space Research 10, no. 12 (January 1990): 119–25. http://dx.doi.org/10.1016/0273-1177(90)90391-c.
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5
Wergen, W. "Normal mode initialization and atmospheric tides." Quarterly Journal of the Royal Meteorological Society 115, no. 487 (April 1989): 535–45. http://dx.doi.org/10.1002/qj.49711548706.
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6
Price, Colin, Ron Maor, and Hofit Shachaf. "Using smartphones for monitoring atmospheric tides." Journal of Atmospheric and Solar-Terrestrial Physics 174 (September 2018): 1–4. http://dx.doi.org/10.1016/j.jastp.2018.04.015.
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7
Palumbo, A. "Reply to comments on "Atmospheric Tides"." Journal of Atmospheric and Solar-Terrestrial Physics 60, no. 18 (December 1998): 1793. http://dx.doi.org/10.1016/s1364-6826(98)00148-5.
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8
French, Richard G., Anthony D. Toigo, Peter J. Gierasch, Candice J. Hansen, Leslie A. Young, Bruno Sicardy, Alex Dias-Oliveira, and Scott D. Guzewich. "Seasonal variations in Pluto’s atmospheric tides." Icarus 246 (January 2015): 247–67. http://dx.doi.org/10.1016/j.icarus.2014.05.017.
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9
Guzewich, Scott D., C. E. Newman, M. de la Torre Juárez, R. J. Wilson, M. Lemmon, M. D. Smith, H. Kahanpää, and A. M. Harri. "Atmospheric tides in Gale Crater, Mars." Icarus 268 (April 2016): 37–49. http://dx.doi.org/10.1016/j.icarus.2015.12.028.
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10
Lindzen, Richard S. "Richard J. Reed and Atmospheric Tides." Meteorological Monographs 53 (December 2003): 85–89. http://dx.doi.org/10.1175/0065-9401-31.53.85.
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Дисертації з теми "Atmospheric tides":

1
Oliver, Sophia. "Modelling studies of the atmospheric tides." Electronic Thesis or Dissertation, University of Oxford, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.365773.
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2
Mertz, Gordon James. "Atmospheric and oceanic 40- to 50-day oscillations in the source region of the Somali Current." Thesis/Dissertation, University of British Columbia, 1985. http://hdl.handle.net/2429/25933.
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Current and temperature data were acquired in the source region of the Somali Current, jointly by the Universities of Kiel and Miami, as part of the INDEX pilot studies. The data were acquired over a six-month period (January-July, 1976) which spans the springtime Monsoon reversal. The experiment and the data are described in Düing and Schott (1978). This thesis describes the results of the spectrum analysis of fluctuations found in data from the experiment's two southernmost sensor locations. It is found that, once the annual cycle is removed, most of the variance in these current and temperature records resides in subinertial fluctuations. The most prominent spectral feature is a 40- to 50-day peak. This 40- to 50-day period is coincident with that of the global-scale circulation cells found in the tropical atmosphere by Madden and Julian (1971 and 1972). The analysis of wind stress and wind stress curl data for the years 1976 and 1979 presented in this thesis indicate that the 40-to 50-day oscillation was present over the Western Indian Ocean during these years. It is suggested here that wind-forcing excites a long coastally trapped wave. To test this idea, a wind-forced quasi-geostrophic, three-layer model and a reduced-gravity model incorporating lateral mean current shear are applied to the Somali Current regime. Model results suggest that the wind forcing is strong enough to excite the observed current and temperature fluctuations.
Science, Faculty of
Physics and Astronomy, Department of
Graduate
3
Wood, Andrew Richard. "Theoretical studies of atmospheric tides for the interpretation of satellite data." Electronic Thesis or Dissertation, University of Oxford, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.359582.
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4
Stine, Alexander 1973. "A survey of internal tides as seen in moored buoy records." Thesis, Massachusetts Institute of Technology, 2002. http://hdl.handle.net/1721.1/29579.
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Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, June 2003.
Includes bibliographical references (leaves 139-144).
We estimate the vertical structure of tidal frequency energy at various locations in the ocean by decomposing current records from the WHOI moored buoy archive. Estimates are made of the barotropic and baroclinic modes 1-4 for multiple locations, primarily in the North Atlantic and North Pacific. Estimates are also made for energy flux rates at some locations. The implied global dissipation rate fro the internal tides is significantly below estimates from altimetry.
by Alexander Stine.
S.M.
5
Kim, Sungphil. "Internal Tides and Internal Solitary Waves in the Northern South China Sea." Text, NCSU, 2007. http://www.lib.ncsu.edu/theses/available/etd-05152009-141246/.
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Large-amplitude internal solitary waves (ISWs) are frequently observed in the northern South China Sea (SCS). In a project sponsored by the US Office of Naval Research, four moorings were deployed between the Luzon Strait and the Chinese continental shelf by Steve Ramp of the Naval Postgraduate School and David Tang of National Taiwan University from late April 2005 to May 2006. Several CTD sections were taken during April and July in 2005. Satellite pictures were also collected during that period. In this study, these data were used to examine the characteristics, generation, and propagation of ISWs. In the satellite images, monthly change in stratification may cause northward shift of the propagation path, and ISWs are more frequently observed in July than in April and May. Speed estimation shows that ISWs propagate faster in the deep basin than over the continental margin and near the ridge. The generation of internal tides correlates with the eastward tidal flow over the ridge, while ISWs are produced by northwestward tidal currents over the ridges in the Luzon Strait.
6
Gagarin, Isa N. "TIDES." Text, VCU Scholars Compass, 2001. https://scholarscompass.vcu.edu/etd/5399.
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My artistic practice creates relationships between the abstract and the personal. I define the abstract in the context of my studio work as a material exploration of color and form. The personal encompasses autobiography in relation to my sense of time and place. In this text, I use my concept of oceanic tides (considered as a temporal and spatial shift between states) to chart my activities as an artist. These activities include making objects that change in character over time, and durational work including performance and video. Interwoven throughout Tides are narrative passages based on my personal experiences, including witnessing the total eclipse of the sun, a purple garden, a coincidence, and the death of a friend.
7
Baumgaertner, Andreas Josef Gerhard. "Observations of Middle Atmosphere Dynamics over Antarctica." Electronic thesis or dissertation, University of Canterbury. Physics and Astronomy, 2007. http://hdl.handle.net/10092/1397.
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This thesis is concerned with the dynamics of the middle atmosphere over the southern-most continent on our planet, Antarctica. Building on previous observational and theoretical efforts to understand the dynamics of this region of the atmosphere, the work encompasses instrument improvements as well as data analysis studies of gravity waves in the lower and middle stratosphere, tides in the upper mesosphere and lower thermosphere, and short-period planetary waves in the stratosphere and mesosphere. An upgrade of the Medium-Frequency Spaced Antenna (MFSA) radar at Scott Base, Antarctica, was carried out in 2004/5 in order to ensure continued operation and enhance its capabilities to measure gravity waves. As a result, the quality of the wind measurements was greatly enhanced and the amount of data collected is now greater by a factor of approximately 15 compared with before the upgrade. Analysis of over two decades of wind velocity data from Scott Base yields a reliable climatology of the dynamics of the upper mesosphere and lower thermosphere in this area, namely the tidal oscillations and the background winds. In addition, interannual variability is assessed and periodicities of approximately 11 years and strong positive trends in tidal amplitudes are reported. Mechanisms that could explain the observed behaviour are proposed. The data are then combined with wind measurements from Halley, the longitudinal conjugate site, in order to study the zonal character of the semi-diurnal tide. Zonal wavenumber 1 and 2 waves are both found and mechanisms that could explain the generation of a wavenumber 1 component are suggested. Two further sets of MFSA radar wind measurements are used to investigate the behaviour of planetary waves with periods of between two and four days in the Antarctic middle atmosphere. Satellite temperature measurements further help to create a more complete picture of these waves. Baroclinic and barotropic instabilities, which result from shears of the zonal wind, appear to be responsible for much of the observed wave activity. In addition, a quasi-to day wave event in mid-May 2005 with unusually large amplitudes is examined and suggested to be linked to a solar proton event. Gravity wave activity over Antarctica is studied using temperature profiles obtained through the satellite radio occultation technique. Although the measurements are restricted to below 35 km altitude, high-resolution temperature profiles allow conclusions to be drawn about the seasonal, geographical, and height distribution of gravity wave activity. Mountain waves are found to be important over the Antarctic Peninsula and the Transantarctic mountains where they contribute more than 20% of the observed wave activity in the lower stratosphere. In addition, the analysis indicates the importance of critical-level filtering and Doppler-shifting.
8
Baumgaertner, Andreas Josef Gerhard. "Observations of Middle Atmosphere Dynamics over Antarctica." University of Canterbury. Physics and Astronomy, 2007. http://hdl.handle.net/10092/1397.
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This thesis is concerned with the dynamics of the middle atmosphere over the southern-most continent on our planet, Antarctica. Building on previous observational and theoretical efforts to understand the dynamics of this region of the atmosphere, the work encompasses instrument improvements as well as data analysis studies of gravity waves in the lower and middle stratosphere, tides in the upper mesosphere and lower thermosphere, and short-period planetary waves in the stratosphere and mesosphere. An upgrade of the Medium-Frequency Spaced Antenna (MFSA) radar at Scott Base, Antarctica, was carried out in 2004/5 in order to ensure continued operation and enhance its capabilities to measure gravity waves. As a result, the quality of the wind measurements was greatly enhanced and the amount of data collected is now greater by a factor of approximately 15 compared with before the upgrade. Analysis of over two decades of wind velocity data from Scott Base yields a reliable climatology of the dynamics of the upper mesosphere and lower thermosphere in this area, namely the tidal oscillations and the background winds. In addition, interannual variability is assessed and periodicities of approximately 11 years and strong positive trends in tidal amplitudes are reported. Mechanisms that could explain the observed behaviour are proposed. The data are then combined with wind measurements from Halley, the longitudinal conjugate site, in order to study the zonal character of the semi-diurnal tide. Zonal wavenumber 1 and 2 waves are both found and mechanisms that could explain the generation of a wavenumber 1 component are suggested. Two further sets of MFSA radar wind measurements are used to investigate the behaviour of planetary waves with periods of between two and four days in the Antarctic middle atmosphere. Satellite temperature measurements further help to create a more complete picture of these waves. Baroclinic and barotropic instabilities, which result from shears of the zonal wind, appear to be responsible for much of the observed wave activity. In addition, a quasi-to day wave event in mid-May 2005 with unusually large amplitudes is examined and suggested to be linked to a solar proton event. Gravity wave activity over Antarctica is studied using temperature profiles obtained through the satellite radio occultation technique. Although the measurements are restricted to below 35 km altitude, high-resolution temperature profiles allow conclusions to be drawn about the seasonal, geographical, and height distribution of gravity wave activity. Mountain waves are found to be important over the Antarctic Peninsula and the Transantarctic mountains where they contribute more than 20% of the observed wave activity in the lower stratosphere. In addition, the analysis indicates the importance of critical-level filtering and Doppler-shifting.
9
Hupe, Patrick [Verfasser], and Markus [Akademischer Betreuer] Rapp. "Global infrasound observations and their relation to atmospheric tides and mountain waves / Patrick Hupe ; Betreuer: Markus Rapp." Online-Ressource, München : Universitätsbibliothek der Ludwig-Maximilians-Universität, 2019. http://d-nb.info/1182228437/34.
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10
Das, Pritha School of Methematics UNSW. "Modelling of ocean tides." Awarded by:University of New South Wales. School of Methematics, 1998. http://handle.unsw.edu.au/1959.4/19038.
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In this thesis three independent studies of tidal dynamics have been pesented. The first is an analytical study of continental shelf tides forced at the ocean boundary. Earlier studies have shown that the response for a sloping shelf and a flat shelf differ and that the response for a flat shelf changes when tides are incident at an angle. Other studies considered a sloping shelf but they did not take into account a possible non-zero depth at a coastal wall. This study shows that the effects of a sloping shelf, a coastal wall and obliquely incident tides an all significantly modify the response on the shelf. The modification increases with the width of the shelf, and in a wide shelf scenario, near resonance, it greatly modifies the response. Secondly, the Princeton Ocean Model in barotropic mode along with a tracer transport module has been used to study the tides of Sydney Harbour. The tidally induced residual circulation due to the semi-diurnal tide consists of a series of recirculating gyres which are due to the interaction of flow with topography. This study shows that in the harbour it is the Lagrangian residual velocity not the Eulerian residual velocity which determines the net transport of material over a tidal cycle. In addition, the flushing time of the harbour varies significantly in space, and the tidal mixing is restricted in the vicinity of the entrance. The third is a theoretical study of forced oscillations in a rotating, flat-bottomed, circular basin. This study shows that the direction of propagation of waves in a basin depends on the ratio of its radius to depth. At each latitude there is a critical value of this ratio and this value decreases with increase in latitude. Beyond this value, waves start to propagate around the basin in the opposite direction to the earth ???s rotation (clockwise in the northern hemisphere and anti-clockwise in the southern hemisphere).The presence of friction increases this critical value which shows that friction plays an important role in determining the response.

Книги з теми "Atmospheric tides":

1
Chapman, Sydney. Atmospheric tides: Thermal and gravitational. New York: Gordon and Breach, 1987.
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2
Stanford, John. Oscillations in D-region absorption at periods of one to two months. [Washington, D.C: National Aeronautics and Space Administration, 1989.
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3
Stanford, John. Oscillations in D-region absorption at periods of one to two months. [Washington, D.C: National Aeronautics and Space Administration, 1989.
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4
Volland, Hans. Atmospheric tidal and planetary waves. Dordrecht: Kluwer Academic Publishers, 1988.
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5
Kähler, Malte. Thermische Gezeiten in einem dreidimensionalen Zirkulationsmodell. Berlin: D. Reimer, 1988.
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6
Caldwell, V. M. Tides. Minneapolis, MN: Milkweed Editions, 2001.
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7
MacKay, Scott. Tides. Amherst, NY: Pyr, 2005.
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8
MacKay, Scott. Tides. Amherst, NY: Pyr, 2005.
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9
Godin, Gabriel. Tides. Ottawa: Anadyomene Edition, 1997.
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10
Godin, Gabriel. Tides. Ensenada, Mexico: Centro de Investigacion y Educacion Superior de Ensenada (C, 1988.
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Частини книг з теми "Atmospheric tides":

1
Dieminger, Walter, Gerd K. Hartmann, and Reinhart Leitinger. "Atmospheric Tides." In The Upper Atmosphere, 97–109. Berlin, Heidelberg: Springer Berlin Heidelberg, 1996. http://dx.doi.org/10.1007/978-3-642-78717-1_3.
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2
Lindzen, Richard S. "Richard J. Reed and Atmospheric Tides." In A Half Century of Progress in Meteorology: A Tribute to Richard Reed, 85–89. Boston, MA: American Meteorological Society, 2003. http://dx.doi.org/10.1007/978-1-878220-69-1_6.
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3
Müller, Peter, and Hans von Storch. "The Dynamics of Tides and Climate." In Computer Modelling in Atmospheric and Oceanic Sciences, 69–89. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-662-06381-1_4.
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4
Parker, Bruce. "Tides." In Encyclopedia of Earth Sciences Series, 1–16. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-48657-4_324-2.
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5
Massel, Stanisław Ryszard. "Tides." In Fluid Mechanics for Marine Ecologists, 155–82. Berlin, Heidelberg: Springer Berlin Heidelberg, 1999. http://dx.doi.org/10.1007/978-3-642-60209-2_5.
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6
Mustoe, George, Paolo A. Pirazzoli, Rhodes W. Fairbridge, Terry R. Healy, Edward B. Hands, B. W. Flemming, Duncan M., et al. "Tides." In Encyclopedia of Coastal Science, 987–96. Dordrecht: Springer Netherlands, 2005. http://dx.doi.org/10.1007/1-4020-3880-1_324.
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7
Schwiderski, Ernst W. "Tides." In The Nordic Seas, 191–210. New York, NY: Springer New York, 1986. http://dx.doi.org/10.1007/978-1-4615-8035-5_8.
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8
Haigh, Ivan D. "Tides." In Encyclopedia of Estuaries, 706–12. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-8801-4_91.
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9
Parker, Bruce. "Tides." In Encyclopedia of Earth Sciences Series, 1750–64. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-93806-6_324.
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10
Smith, Philip M. "Terminology used in tidal calculations." In Tides, 1–16. First edition. | Routledge : Abingdon, Oxon ; New York, NY, [2018]: Routledge, 2018. http://dx.doi.org/10.4324/9781315561110-1.
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Тези доповідей конференцій з теми "Atmospheric tides":

1
Tatikonda, Shirish, Srinivasan Parthasarathy, and Tahsin Kurc. "TRIPS and TIDES." In the 15th ACM international conference. New York, New York, USA: ACM Press, 2006. http://dx.doi.org/10.1145/1183614.1183680.
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2
Plink-Bjorklund, Piret. "TIDES AND DELTAIC MORPHODYNAMICS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-279594.
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3
Efroimsky, Michael, and Valéry Lainey. "On the Theory of Bodily Tides." In NEW TRENDS IN ASTRODYNAMICS AND APPLICATIONS III. AIP, 2007. http://dx.doi.org/10.1063/1.2710050.
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4
Tolman, Hendrik L. "Propagation of Wind Waves on Tides." In 21st International Conference on Coastal Engineering. New York, NY: American Society of Civil Engineers, 1989. http://dx.doi.org/10.1061/9780872626874.037.
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5
Charlier, R. H., P. Morand, C. W. Finkl, and A. Thys. "Green tides on the Brittany coasts." In 2006 IEEE US/EU Baltic International Symposium on Integrated Ocean Observation Syst. for Managing Global & Regional Ecosys.Marine Resch. IEEE, 2006. http://dx.doi.org/10.1109/baltic.2006.7266128.
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6
CALKOEN, CHARLES J. "TIDES IN COASTAL AREAS FROM ALTIMETER DATA." In Proceedings of the 29th International Conference. World Scientific Publishing Company, 2005. http://dx.doi.org/10.1142/9789812701916_0365.
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7
Nakaza, Eizo, Seikoh Tsukayama, Yasutomo Kawamitsu, Toshiaki Makino, and Rika Takeuchi. "Abnormal High Tides Induced by Surf-Beats." In 27th International Conference on Coastal Engineering (ICCE). Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40549(276)271.
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8
van Smirren, J., and Shejun Fan. "The complex tides of the Torres Straits." In OCEANS 2012. IEEE, 2012. http://dx.doi.org/10.1109/oceans.2012.6405016.
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9
Billa, Jayadev, Mohamed Noamany, Amit Srivastava, John Makhoul, and Francis Kubala. "Arabic speech and text in TIDES OnTAP." In the second international conference. Morristown, NJ, USA: Association for Computational Linguistics, 2002. http://dx.doi.org/10.3115/1289189.1289245.
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10
LI, HSIEN-WEN, and YUNG-CHING WU. "A NUMERICAL PREDICTIVE MODEL OF TIDES AROUND TAIWAN." In Advances in Engineering Mechanics - Reflections and Outlooks - In Honor of Theodore Y.-T. Wu. WORLD SCIENTIFIC, 2005. http://dx.doi.org/10.1142/9789812702128_0023.
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Звіти організацій з теми "Atmospheric tides":

1
Niles, Keron. Resilience Amidst Rising Tides. Geneva, Switzerland: International Centre for Trade and Sustainable Development, 2010. http://dx.doi.org/10.7215/co_ip_20100224.
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2
Boyd, Timothy, and Laurence Padman. Arctic Mixing and Tides. Fort Belvoir, VA: Defense Technical Information Center, September 1997. http://dx.doi.org/10.21236/ada627887.
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3
Egbert, Gary D. Inverse Modeling of Coastal Tides. Fort Belvoir, VA: Defense Technical Information Center, September 1999. http://dx.doi.org/10.21236/ada613935.
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4
Egbert, Gary D. Inverse Modeling of Ocean Tides. Fort Belvoir, VA: Defense Technical Information Center, September 1997. http://dx.doi.org/10.21236/ada627881.
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5
Girton, James B., and Eric Kunze. AESOP Internal Tides and Mixing. Fort Belvoir, VA: Defense Technical Information Center, May 2012. http://dx.doi.org/10.21236/ada561696.
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6
Bartone, Paul T., Mark A. Vaitkus, Kathleen Jocoy, Jocelyn V. Bartone, II Wells, Wells Linton, and Linda M. Organizational Analysis of the TIDES Project and the STAR-TIDES Network Using the 7-S Framework. Fort Belvoir, VA: Defense Technical Information Center, April 2013. http://dx.doi.org/10.21236/ada622059.
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7
Wallcraft, Alan J. Eddy Resolving Global Ocean Prediction including Tides. Fort Belvoir, VA: Defense Technical Information Center, September 2010. http://dx.doi.org/10.21236/ada542414.
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8
Wallcraft, Alan J. Eddy Resolving Global Ocean Prediction including Tides. Fort Belvoir, VA: Defense Technical Information Center, September 2012. http://dx.doi.org/10.21236/ada574793.
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9
Wallcraft, Alan J. Eddy Resolving Global Ocean Prediction Including Tides. Fort Belvoir, VA: Defense Technical Information Center, January 2009. http://dx.doi.org/10.21236/ada518715.
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10
Wallcraft, Alan J. Eddy Resolving Global Ocean Prediction including Tides. Fort Belvoir, VA: Defense Technical Information Center, September 2011. http://dx.doi.org/10.21236/ada557069.
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