An evaluation of global tidal models on the inner continental shelf of Argentina, South America
Nowadays several global tidal models, most of them freely available for the community, provide tidal sea level heights practically everywhere around the World Ocean, constituting powerful tools for scientists, oceanographers and users of different areas of geosciences. In addition, most of these glo...
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Nova Science Publishers, Inc.
2011
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| Acceso en línea: | Registro en Scopus Handle Registro en la Biblioteca Digital |
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| LEADER | 07797caa a22005897a 4500 | ||
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| 001 | PAPER-10117 | ||
| 003 | AR-BaUEN | ||
| 005 | 20250306091919.0 | ||
| 008 | 190411s2011 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84861870391 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Dragani, W. | |
| 245 | 1 | 3 | |a An evaluation of global tidal models on the inner continental shelf of Argentina, South America |
| 260 | |b Nova Science Publishers, Inc. |c 2011 | ||
| 270 | 1 | 0 | |m Dragani, W.; Servicio de Hidrografía Naval, ESCM-INUN, Ciudad Autonoma, Argentina |
| 504 | |a Balay, M.A., Determination of mean sea level of Argentine Sea. Influences of oscillations of the sea not caused by tides (1956) International Hydrographic Review (Monaco), 33 (2), pp. 31-65 | ||
| 504 | |a Dragani, W., D'Onofrio, E., Grismeyer, W., Fiore, M., Violante, R., Rovere, E., Vulnerability of the Atlantic Patagonian coast to tsunamis generated by submarine earthquakes located in the Scotia Arc region. Some numerical experiments (2008) Natural Hazards, 49, pp. 437-458. , DOI: 10.1007/s11069-008-9289-4 | ||
| 504 | |a Egbert, G., Bennett, A., Foreman, M., TOPEX/POSEIDON tides estimated using a global inverse model (1994) Journal of Geophysical Research, 99 (C12), pp. 24821-24852 | ||
| 504 | |a Egbert, G.D., Erofeeva, S.Y., Efficient inverse modeling of barotropic ocean tides (2002) Journal of Atmospheric and Oceanic Technology, 19 (2), pp. 183-204 | ||
| 504 | |a Fang, G., Wang, Y., Wei, Z., Choi, B.H., Wang, X., Wang, J., Empirical cotidal charts of the Bohai, Yellow, and East China Seas from 10 years of TOPEX/Poseidon altimetry (2004) J. Geophys. Res., 109, pp. C11006. , doi:10.1029/2004JC002484 | ||
| 504 | |a Foreman, M.G.G., Manual for tidal heights analysis and prediction (1977) Pac. Mar. Sci. Rep., pp. 77-10+97. , Inst. of Ocean Sci., Patricia Bay, Sidney, B. C., Canada | ||
| 504 | |a Glorioso, P.D., Simpson, J.H., Numerical modeling of the M2 tide on the northern Patagonian shelf (1994) Continental Shelf Research, 14, pp. 267-278 | ||
| 504 | |a Glorioso, P.D., Flather, R.A., A barotropic model of the currents off SE South America (1995) Journal of Geophysical Research, 100, pp. 13427-13440 | ||
| 504 | |a Glorioso, P.D., Flather, R.A., The Patagonian Shelf tides (1997) Progress in Oceanography, 40, pp. 263-283 | ||
| 504 | |a Glorioso, P.D., Patagonian Shelf 3-D tide and surge model (2000) Journal of Marine Systems, 24, pp. 141-151 | ||
| 504 | |a Lefevre, F., Lyard, F.H., Le Provost, C., Schrama, E.J.O., FES99: a global tide finite element solution assimilating tide gauge and altimetric information (2002) Journal of Atmospheric and Oceanic Technology, 19, pp. 1345-1356 | ||
| 504 | |a Lyard, F., Lefevre, F., Letellier, T., Francis, O., Modeling the global ocean tides: modern insights from FES2004 (2006) Ocean Dynamics, 56, pp. 394-415 | ||
| 504 | |a O'Connor, W.P., A numerical model of tides and storm surges in the Río de la Plata estuary (1991) Continental Shelf Research, 11, pp. 1491-1508 | ||
| 504 | |a Palma, E.D., Matano, R.P., Piola, A.R., A numerical study of the Southwestern Atlantic Shelf circulation: Barotropic response to tidal and wind forcing (2004) J. Geophys. Res., 109, pp. C08014. , doi: 10.1029/2004JC002315 | ||
| 504 | |a Ray, R.D., A global ocean tide model from TOPEX/POSEIDON altimetry: GOT99 (1999), Technical Report NASA Tech. Mem. 209478, Goddard Space Flight Centre, Greenbelt, MD, USA; Schureman, P., Manual of harmonic analysis and prediction of tides (1988), p. 317. , Washington, U.S. Government Printing Office, Special Publ. No. 98; Simionato, C., Dragani, W.C., Nuñez, M.N., Engel, M., A set of 3-d nested models for tidal propagation from the Argentinean Continental Shelf to Río de la Plata Estuary (2004) Journal of Coastal Research, 3 (20), pp. 893-912 | ||
| 504 | |a Shum, C.K., Woodworth, P.L., Andersen, O.B., Egbert, G.D., Francis, O., King, C., Klosko, S.M., Wunsch, C.I., Accuracy assessment of recent ocean tide models (1997) Journal of Geophysical Research, 102 (C11), pp. 25+173-25+194 | ||
| 504 | |a on sea level measurement and interpretation (1985), p. 83. , UNESCO, Intergovernmental Oceanographic Commission; Zahran, K.H., Jentzsch, G., Seeber, G., Accuracy assessment of ocean tide loading computations for precise geodetic observations (2006) Journal of Geodynamics, 42, pp. 159-174 | ||
| 506 | |2 openaire |e Política editorial | ||
| 520 | 3 | |a Nowadays several global tidal models, most of them freely available for the community, provide tidal sea level heights practically everywhere around the World Ocean, constituting powerful tools for scientists, oceanographers and users of different areas of geosciences. In addition, most of these global models are frequently used to provide tidal heights at the open boundaries of regional high resolution coastal models. This work is an evaluation of the performance of three of the most recognized global tidal models: FES2004 (Lyard et al., 2006), GOT 4.7, an update of GOT00 (Ray, 1999) and TPXO 7.2, an update of TPXO 6 (Egbert et al., 1994; Egbert and Erofeeva, 2002). The tidal harmonic constants from these models are compared to the ones obtained from ten sea level data series gathered at tidal stations located along the Argentine coast (from the Río de la Plata estuary to Tierra del Fuego) and from twenty data series of sea level heights obtained on the crossing of the satellite tracks from the Ocean Topography Experiment (Topex/Poseidon: T/P) on the Argentine continental shelf (in the period 1992-2002). Four semidiurnal constituents (M2, S2, N2 and K2) and four diurnal ones (K1, O1, P1 and Q1) are studied and the corresponding harmonic vectorial differences of observed sea level and altimeter data series are presented and discussed. The main differences between harmonic amplitudes and phases obtained from observations and from global models are detected in coastal waters of the Río de la Plata (a shallow area characterized by a micro tidal regime). Such differences, in general, significantly decrease towards the south, where the tidal range is greater than 10 m and the tide is practically semidiurnal. © 2011 by Nova Science Publishers, Inc. All rights reserved. |l eng | |
| 593 | |a Servicio de Hidrografía Naval, ESCM-INUN, Ciudad Autonoma, Argentina | ||
| 593 | |a Departamento Ciencias de la Atmósfera y los Océanos, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad Autonoma, Argentina | ||
| 593 | |a Instituto de Geodesia y Geofísica Aplicadas, Facultad de Ingeniería, Universidad de Buenos Aires, Ciudad Autonoma, Argentina | ||
| 593 | |a CONICET, Consejo Nacional de Investigaciones Científicas y Técnicas, Ciudad Autonoma, Argentina | ||
| 690 | 1 | 0 | |a ARGENTINE CONTINENTAL SHELF |
| 690 | 1 | 0 | |a HARMONIC CONSTANTS |
| 690 | 1 | 0 | |a MODELED TIDE |
| 690 | 1 | 0 | |a OBSERVED TIDE |
| 700 | 1 | |a D'Onofrio, Enrique Eduardo | |
| 700 | 1 | |a Fiore, M. | |
| 700 | 1 | |a Grismeyer, W. | |
| 700 | 1 | |a Oreiro, F. | |
| 773 | 0 | |d Nova Science Publishers, Inc., 2011 |h pp. 235-249 |p Sea Level Rise, Coastal Eng., Shorelines and Tides |z 9781617286551 |t Sea Level Rise, Coastal Engineering, Shorelines and Tides | |
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