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15 results on '"Flores‐Vidal, Xavier"'

1. An affordable operational oil spill monitoring system in action: A diachronic multiplatform analysis of recent incidents in the southern Gulf of Mexico

Author

Uribe-Martínez, Abigail, Espinoza-Tenorio, Alejandro, Cruz-Pech, Johnny Bryan, Cupido-Santamaría, Deysi Guadalupe, Trujillo-Córdova, Jorge Alfredo, García-Nava, Héctor, Flores-Vidal, Xavier, Gudiño-Elizondo, Napoleón, Herguera, Juan Carlos, Appendini, Christian Mario, and Cuevas, Eduardo

Published
2024
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4. Ocean Monitoring and Prediction Network for the Sustainable Development of the Gulf of Mexico and the Caribbean.

Author

Carlos Herguera, Juan, Peters, Edward M., Sheinbaum, Julio, Pérez-Brunius, Paula, Magar, Vanesa, Pallàs-Sanz, Enric, Estrada Allis, Sheila, Leopoldina Aguirre-Macedo, M., Manuel Vidal-Martinez, Victor, Enriquez, Cecilia, Mariño Tapia, Ismael, García Nava, Hector, Flores Vidal, Xavier, Salgado, Tomas, Romero-Centeno, Rosario, Zavala-Hidalgo, Jorge, Cuevas Flores, Eduardo Amir, Uribe Martínez, Abigail, and Carrillo, Laura

Subjects
TROPICAL cyclones, TROPICAL storms, SUSTAINABLE development, MODIS (Spectroradiometer), OCEAN, ATMOSPHERIC sciences
Published
2023
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6. Contributors

Author

Anderson, Eric J., primary, Archer, Matthew R., additional, de Freitas Assad, Luiz Paulo, additional, Baltes, Becky, additional, Bergman, Cecília, additional, Bickel, Aric, additional, Bjorkstedt, Eric P., additional, Boechat, Ana Carolina, additional, Borge, Jose Carlos Nieto, additional, Bundy, Marie, additional, Buskey, Edward J., additional, Cabral, Marcelo Montenegro, additional, Callender, Russell, additional, Carrasco, Ruben, additional, Carratelli, Eugenio Pugliese, additional, Carrier, Matthew, additional, Carter, Melissa L., additional, de Carvalho, Gabriel Vieira, additional, Castro, Rubén, additional, Cothran, Jeremy, additional, Marques da Cruz, Leonardo Maturo, additional, Dentale, Fabio, additional, Dixon, L. Kellie, additional, Dominguez, Feliciano, additional, Dorton, Jennifer, additional, Durazo, Reginaldo, additional, Edwards, Christopher A., additional, Fake, Todd, additional, Ferner, Matthew C., additional, Fiechter, Jerome, additional, Flores-Vidal, Xavier, additional, da Rocha Fragoso, Maurício, additional, Galvarino, Charlton, additional, Garção, Henery Ferreira, additional, Gil, Eduardo, additional, Gill, Eric W., additional, Gurgel, Klaus-Werner, additional, Harlan, Jack, additional, Hazard, Lisa, additional, Hernandez, Debra, additional, Horstmann, Jochen, additional, Howard, Matthew K., additional, Howard, Meredith D.A., additional, Huang, Weimin, additional, Jacox, Michael G., additional, Jaimes, Benjamin, additional, Jensen, Robert E., additional, Jochens, Ann E., additional, Jones, Adrian, additional, Keen, Carolyn, additional, Kelsey, Heath, additional, Kerkering, Heather, additional, Kirkpatrick, Barbara, additional, Kirkpatrick, Gary J., additional, Kobara, Shinichi, additional, Kohut, Josh, additional, Kudela, Raphael M., additional, Landau, Luiz, additional, Lembke, Chad, additional, Leonard, Lynn, additional, Liu, Yonggang, additional, Ludeno, Giovanni, additional, Luettich, Rick, additional, Lund, Bjoern, additional, Manderson, John, additional, Mariano, Lívia Sant'Angelo, additional, Martinez-Pedraja, Jorge, additional, McCammon, Molly, additional, Merz, Clifford R., additional, de Miranda, Tiago Cardoso, additional, Moore, Andrew M., additional, Muscarella, Philip, additional, Natale, Antonio, additional, Navarro, Luis F., additional, Ngodock, Hans, additional, Santi Coimbra de Oliveira, André Luis, additional, Otero, Mark, additional, de Castro Pellegrini, Júlio Augusto, additional, Petersen, Leif, additional, Peterson, William T., additional, Pimentel, Flávia Pozzi, additional, Porter, Dwayne E., additional, Quintrell, Josie, additional, Ramage, Dan, additional, Read, Jennifer, additional, Reale, Ferdinando, additional, Reay, William G., additional, Rinaldi, Frederico Luna, additional, Rosenfeld, Leslie, additional, Roughan, Moninya, additional, Alves dos Santos, Francisco, additional, dos Santos, Natalia Gomes, additional, Schaeffer, Amandine, additional, Schofield, Oscar M., additional, Schwab, David J., additional, Seemann, Jorg, additional, Serafino, Francesco, additional, Shapiro, Justin, additional, Shay, Lynn K., additional, Simoniello, Christina, additional, Smith, Erik, additional, Smith, Scott, additional, Mendes Soares, Felipe Lobo, additional, Souopgui, Innocent, additional, Spranger, Michael, additional, Stumpf, Richard P., additional, Subramanian, Vembu, additional, Suthers, Iain M., additional, Terrill, Eric, additional, Thomas, Julie, additional, São Tiago, Pedro Marques, additional, Tomlinson, Michelle, additional, Trueblood, Dwight, additional, Watson, Stephanie, additional, Weisberg, Robert H., additional, Willis, Zdenka, additional, Wyatt, Lucy R., additional, and Zheng, Lianyuan, additional

Published
2015
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10. The Global High Frequency Radar Network

Author

Roarty, Hugh, primary, Cook, Thomas, additional, Hazard, Lisa, additional, George, Doug, additional, Harlan, Jack, additional, Cosoli, Simone, additional, Wyatt, Lucy, additional, Alvarez Fanjul, Enrique, additional, Terrill, Eric, additional, Otero, Mark, additional, Largier, John, additional, Glenn, Scott, additional, Ebuchi, Naoto, additional, Whitehouse, Brian, additional, Bartlett, Kevin, additional, Mader, Julien, additional, Rubio, Anna, additional, Corgnati, Lorenzo, additional, Mantovani, Carlo, additional, Griffa, Annalisa, additional, Reyes, Emma, additional, Lorente, Pablo, additional, Flores-Vidal, Xavier, additional, Saavedra-Matta, Kelly Johanna, additional, Rogowski, Peter, additional, Prukpitikul, Siriluk, additional, Lee, Sang-Ho, additional, Lai, Jian-Wu, additional, Guerin, Charles-Antoine, additional, Sanchez, Jorge, additional, Hansen, Birgit, additional, and Grilli, Stephan, additional

Published
2019
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13. Circulación residual en Bahía San Quintín, BC. México

Author

Flores Vidal, Xavier and Reginaldo Durazo Arvizu

Subjects
2510 [cti], 1 [cti], Viento,Fricción,Circulación,Ciencias del mar [Autor], 25 [cti]
Abstract

Datos de ADCP´s (Acoustic Doppler Current Profilers) anclados por 60 días se usan para estudiar el patrón de circulación residual en Bahía San Quintín, Baja California México. El patrón de circulación residual es complementado con datos de un ADCP adaptado a una embarcación, que realizó pases sobre un transecto cercano a la boca de conexión, lo que permitió estimar los flujos netos de intercambio entre la bahía y el océano adyacente. Los datos muestran una circulación de dos capas originada por el esfuerzo del viento en la superficie, mismo que da lugar a un apilamiento de agua hacia el sur-este, del orden de 8 cm. Durante periodos de vientos débiles el nivel del mar disminuye y da lugar a corrientes del orden de 1 cm s⁻¹ en dirección contraria al viento. La marea juega un papel secundario en la circulación de la capa superficial, en contraste, es el agente dominante en la capa de fondo. Durante vientos débiles se inhibe la circulación de dos capas, dando lugar a una circulación homogénea en toda la columna de agua y modulada por la marea. En la boca de conexión la circulación es homogénea en la vertical, dominada por la marea y sin presentar ningún indicio de la influencia del viento. Aquí los flujos netos de entrada se restringen al canal profundo (lado oeste de la boca), mientras que los flujos de salida se ubican en el canal somero (lado este de la boca). Este patrón de circulación es similar al esperado por la teoría, en el que el hecho de que los flujos netos de entrada sean restringidos al canal profundo en este tipo de sistemas, se debe a que los efectos de fricción son más importantes que los efectos de la rotación de la tierra (número de Ekman ≈ 1). Current data from 60 days moored ADCP’s (Acoustic Doppler Current Profilers)are used to study the residual circulation of the San Quintín Bay in Baja California,México. The residual circulation pattern was completed with data from a towed ADCP,that made cross transects near the inlet bay, this allowed the estimation of the meanflow between the bay and the adjacent ocean. Data showed a two layers circulation dueto wind stress forcing over the surface, this caused a rising of surface level around 8 cm.During low wind periods the sea level diminish and give place to weak currents (≈ 1cm s⁻¹ ) against wind direction. Tide has a secondary roll in the surface layer, whereasin the bottom layer it dominates the circulation. In the low wind periods, the twolayer circulation is inhibited and a vertically homogeneous tide modulated circulationits developed. In the inlet bay the circulation is vertically homogeneous, dominated bythe tide and without influence of the wind. Here the inflows are restricted to the deepchannel (western side of the inlet), while the outflows are located over the shallow channel(eastern side of the inlet). This pattern of circulation is similar to expected by thetheory, in which the net inflows are restricted to the deep channel due to large frictionalinfluences or less important effects of the earth’s rotation (Ekman number ≈ 1).

Published
2006

15. Simulación numérica de la hidrodinámica de un puerto y el efecto de un sistema de bombeo por energía de oleaje.

Author

Flores-Vidal, Xavier, Ramírez-Aguilar, Isabel, and Czitrom-Baus, Steven

Subjects
*SALINITY, *ROCK-forming minerals, *EMBARGO, *INTERNATIONAL sanctions, *WINDS, *SOIL salinity
Abstract

A three-dimensional numerical model was adapted to study the circulation, stratification and mixing patterns inside the port of El Sauzal. Salinity, temperature and density field data were measured, showing that density variations were mainly due to the temperature field with a very small contribution from salinity. The model simulated surface currents and the temperature field. The simulation was compared against field data showing that the model reproduces satisfactorily the circulation, stratification and mixing patterns. Surface circulation and vertical mixing were mainly forced by the tide, although winds greater than 6 m s-1 became the main forcing of vertical mixing and surface circulation. The surface currents traveled outside the port during ebb tide and vice versa during flood tide; however, with winds greater than 6 m s-1the surface velocity followed the wind direction. When a discharge of 0.2 m³ s-1 was introduced into the system, the simulation showed an increase of 0.5 cm s-1 in the surface current velocity, during ebb tide. The vertical temperature structure increased as much as the discharge temperature (17.2°C). This result verifies that a controlled discharge could improve circulation and mixing, reducing the residence time and improving the levels of oxygen in the water. [ABSTRACT FROM AUTHOR]

Published
2005

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