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  • 1
    Publication Date: 2021-05-19
    Description: Due to the lack of information in the catalogue of historic earthquakes (1951-2010) and also of potential but unmapped faults in the field, the seismic zoning modeling for Ecuador does not define parameters of equivalent attenuations of the tectonic activity of the territory. The aim of this research is to provide new engineering techniques for seismic hazard evaluation. The technique of this study is based on the assumption that strong earthquakes are associated within structural nodes that are specific structures formed around intersections of fault zones. The nodes have been delineated with a morphostructural zoning method, based on the idea that the lithosphere is made-up of different-scaled blocks, separated by mobile boundaries. These blocks are represented on a morphostructural map, compiled with the GIS.
    Description: Debido a la escasa información en los catálogos de terremotos históricos, desde el año 1541 hasta el año 2010 y, además de la cartografía de los terrenos con fallas capaces de generarlos, no ha sido posible que los modelos de zonación sísmica para Ecuador definan parámetros de atenuaciones concordantes con la actividad tectónica del territorio. El presente estudio pretende proporcionar nuevas técnicas de ingeniería para evaluar la peligrosidad sísmica. La técnica asume que los fuertes terremotos corticales son generados alrededor de intersecciones de zonas de fallas, nudos estructurales. Los nudos han sido caracterizados por el método de zonación morfo-estructural, basado sobre la idea que la litósfera es formada por bloques de diferentes escalas, separadas por límites móviles. Estos bloques son representados en un mapa morfoestructural, compilado con la tecnología GIS a escala 1:5000.000 para las cadenas colinares costeras y subandina, y a escala 1:750.000 para las cadenas montañosas de los Andes septentrionales del Ecuador. Datos geológicos, topográficos, morfológicos y gravimétricos fueron obtenidos desde cada nudo estructural, posteriormente esta información ha sido insertada en el software "CORA 3" (Técnica "Pattern Recognition") para codificar y discretizar los valores qyue nos permiten individualizar los nudos sismogénicos capaces de generar terremotos con M≥6 y M≥6.5. Muchos de estos nudos son delineados a lo largo de estructuras de fallas. Los resultados en este estudio indican altos niveles de sismicidad en áreas en donde no existen registros de terremotos, además lo localización de nudos sismogénicos pueden proporcionar un catálogo sintético que podría ser complementado con el corto catálogo de terremotos históricos del Ecuador para la elaboración de modelos de zonación sísmica.
    Description: Published
    Keywords: Earthquakes ; Pattern recognition ; Joints ; Seismic zones
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed , Article
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  • 2
    Publication Date: 2022-11-10
    Description: © The Author(s), 2019. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in [citation], doi:[doi]. Gommenginger, C., Chapron, B., Hogg, A., Buckingham, C., Fox-Kemper, B., Eriksson, L., Soulat, F., Ubelmann, C., Ocampo-Torres, F., Nardelli, B. B., Griffin, D., Lopez-Dekker, P., Knudsen, P., Andersen, O., Stenseng, L., Stapleton, N., Perrie, W., Violante-Carvalho, N., Schulz-Stellenfleth, J., Woolf, D., Isern-Fontanet, J., Ardhuin, F., Klein, P., Mouche, A., Pascual, A., Capet, X., Hauser, D., Stoffelen, A., Morrow, R., Aouf, L., Breivik, O., Fu, L., Johannessen, J. A., Aksenov, Y., Bricheno, L., Hirschi, J., Martin, A. C. H., Martin, A. P., Nurser, G., Polton, J., Wolf, J., Johnsens, H., Soloviev, A., Jacobs, G. A., Collard, F., Groom, S., Kudryavtsev, V., Wilkin, J., Navarro, V., Babanin, A., Martin, M., Siddorn, J., Saulter, A., Rippeth, T., Emery, B., Maximenko, N., Romeiser, R., Graber, H., Azcarate, A. A., Hughes, C. W., Vandemark, D., da Silva, J., Van Leeuwen, P. J., Naveira-Garabato, A., Gemmrich, J., Mahadevan, A., Marquez, J., Munro, Y., Doody, S., & Burbidge, G. SEASTAR: A mission to study ocean submesoscale dynamics and small-scale atmosphere-ocean processes in coastal, shelf and polar seas. Frontiers in Marine Science, 6, (2019):457, doi:10.3389/fmars.2019.00457.
    Description: High-resolution satellite images of ocean color and sea surface temperature reveal an abundance of ocean fronts, vortices and filaments at scales below 10 km but measurements of ocean surface dynamics at these scales are rare. There is increasing recognition of the role played by small scale ocean processes in ocean-atmosphere coupling, upper-ocean mixing and ocean vertical transports, with advanced numerical models and in situ observations highlighting fundamental changes in dynamics when scales reach 1 km. Numerous scientific publications highlight the global impact of small oceanic scales on marine ecosystems, operational forecasts and long-term climate projections through strong ageostrophic circulations, large vertical ocean velocities and mixed layer re-stratification. Small-scale processes particularly dominate in coastal, shelf and polar seas where they mediate important exchanges between land, ocean, atmosphere and the cryosphere, e.g., freshwater, pollutants. As numerical models continue to evolve toward finer spatial resolution and increasingly complex coupled atmosphere-wave-ice-ocean systems, modern observing capability lags behind, unable to deliver the high-resolution synoptic measurements of total currents, wind vectors and waves needed to advance understanding, develop better parameterizations and improve model validations, forecasts and projections. SEASTAR is a satellite mission concept that proposes to directly address this critical observational gap with synoptic two-dimensional imaging of total ocean surface current vectors and wind vectors at 1 km resolution and coincident directional wave spectra. Based on major recent advances in squinted along-track Synthetic Aperture Radar interferometry, SEASTAR is an innovative, mature concept with unique demonstrated capabilities, seeking to proceed toward spaceborne implementation within Europe and beyond.
    Description: CG and AM received funding from the United Kingdom Centre for Earth Observation Instrumentation SEASTAR+ project (Contract No. RP10G0435A02). PVL was supported by the European Research Council (ERC) CUNDA project 694509 under the European Union Horizon 2020 Research and Innovation Program.
    Keywords: Satellite ; Air sea interactions ; Upper ocean dynamics ; Submesoscale ; Coastal ; Marginal ice zone ; Radar ; Along-track interferometry
    Repository Name: Woods Hole Open Access Server
    Type: Article
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