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Your search keyword '"Jiménez-Illescas, A. R."' showing total 6 results
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6 results on '"Jiménez-Illescas, A. R."'

1. Contributors

Author

Achary, M.S., primary, Amaratunga, Dilanthi, additional, Jiménez-Illescas, Ángel R., additional, Amir, Md Sharif Imam Ibne, additional, Anandkumar, A., additional, Arockiaraj, S., additional, Ashar, Faisal, additional, Azuz Adeath, Isaac, additional, Banerjee, K., additional, Basu, Mrittika, additional, Biswas, S., additional, Choudhury, Smitanjali, additional, Cortés Ruiz, Alejandra, additional, Das, N.P.I., additional, DasGupta, Rajarshi, additional, Gevaña, Dixon T., additional, Glaeser, Bernhard, additional, Gómez, Cristina, additional, Gregory, Billy J., additional, Green, David R., additional, Hagon, Jason J., additional, Haigh, Richard, additional, Jayakumar, K., additional, Jonathan, M.P., additional, Kankara, R.S., additional, Khan, M. Shah Alam, additional, Kumar, Bharat, additional, Lakshmanan, Elango, additional, Lakshmi, Ahana, additional, Le Bail, Maxime, additional, Espinosa-Carreón, T. Leticia, additional, López, Alfredo Salazar, additional, Zayas-Esquer, Ma Magdalena, additional, Mohanty, A.K., additional, Muñoz Sevilla, Norma Patricia, additional, Murakami, Tomokazu, additional, Nagarajan, R., additional, Rekha Nianthi, K.W.G., additional, Nimal Sri Rajarathna, W.A., additional, Ogasawara, Toshinori, additional, Padhi, R.K., additional, Paneerselvam, A., additional, Panigrahi, S.N., additional, Panigrahy, R.C., additional, Pérez, Omar Mayorga, additional, Pulhin, Juan M., additional, Purvaja, R., additional, Raghunathan, C., additional, Raghuraman, R., additional, Ramesh, R., additional, Rawlins, B.K., additional, Retama, I., additional, Rivera Rivera, D.M., additional, Rodríguez, María Concepción Martínez, additional, Rodríguez-Espinosa, P.F., additional, Sahu, G., additional, Samantara, M.K., additional, Sarkar, S.K., additional, Satpathy, K.K., additional, Shaw, Rajib, additional, Shimokawa, Shinya, additional, Shruti, V.C., additional, Sridarran, Pournima, additional, Sujitha, S.B., additional, Tapia, Maricel A., additional, Vengadesan, Manivannan, additional, Vetrimurugan, E., additional, and Vijith, H., additional

Published
2019
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3. Modelo hidrodinámico en el Sistema Lagunar Navachiste, Guasave, Sinaloa, México

Author

Sánchez-Lindoro, Fernando de J, Jiménez-Illescas, Ángel R, Espinosa-Carreón, T. Leticia, and Obeso-Nieblas, Maclovio

Subjects
Corrientes de marea, Sistema Lagunar San Ignacio - Navachiste - Macapule, modelo hidrodinámico numérico, coastal lagoons, flow simulation, hydrodynamic numerical model, lagunas costeras, simulación de corrientes, Tidal currents, San Ignacio-Navachiste-Macapule Lagoon System
Abstract

El Sistema Lagunar Navachiste se encuentra conectado con el Golfo de California (GC) a través de 3 canales de marea. El sistema cuenta con un área de 301 km² aproximadamente, con una profundidad promedio de 2,5 m y una altura de mareas promedio de 1,5 m. Para simular las corrientes de mareas y el efecto del viento se aplicó un modelo hidrodinámico numérico barótropico, integrado en la vertical y en diferencias finitas; para calibrar el modelo se hicieron mediciones lagrangeanas y se compararon con las corrientes simuladas en los canales de marea del sistema. El modelo simula el comportamiento hidrodinámico del sistema lagunar y presenta una correlación superior al 85% con las trayectorias trazadas por los cuerpos de deriva y con las velocidades máximas eulerianas medidas en los canales internos y en las bocas del sistema. The Navachiste Lagoon System is connected to the Gulf of California (GC) via 3 tidal channels. The system has an area of approximately 301 km², with an average depth of 2.5 m and an average tide height of 1.5 m. In order to simulate tidal currents and the effect of wind, a numerical hydrodynamic model was applied, integrated in the vertical and in finite differences; to calibrate the model, lagrangean measurements were made and compared with simulated currents in the tidal channels of the system. The model simulates the hydrodynamic behavior of the lagoon system and has a correlation higher than 85% with the trajectories traced by the drift bodies and with the maximum Eulerian velocities measured in the internal channels and in the mouths of the system.

Published
2017

5. Modelo hidrodinámico en el Sistema Lagunar Navachiste, Guasave, Sinaloa, México.

Author

de J. Sánchez-Lindoro, Fernando, Jiménez-Illescas, Ángel R., Espinosa-Carreón, T. Leticia, and Obeso-Nieblas, Maclovio

Abstract

Copyright of Revista de Biologia Marina y Oceanografía (RBMO) is the property of Universidad de Valparaiso, Facultad de Ciencias del Mar and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Published
2017
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6. Hidrografía en la Boca Norte de la Bahía de La Paz, Baja California Sur, México.

Author

Obeso-Nieblas, M., Shirasago-Germán, B., Gaviño-Rodríguez, J. H., Obeso-Huerta, H., Pérez-Lezama, E. L., and Jiménez-Illescas, A. R.

Subjects
*EARTH science education, *MARINE sciences, *HYDROGRAPHY, *OCEANOGRAPHY, *AQUATIC sciences, *WATER masses, *BAYS
Abstract

To describe the hydrographical variability at the North Mouth of La Paz Bay, its main point of communication with the Gulf of California, CTD data were analyzed from four sampling surveys conducted during an annual cycle (May, July and October 2001, and February 2002). The results showed an absence of the mixed layer and intense temperature and salinity stratification in spring and summer. In autumn a 30-m mixed layer was registered, with a temperature of 28.5°C, while in winter an unusual 100-m mixed layer was detected, with a temperature of 17.9°C. Particular noteworthy is the similarity of the structure between the surface and subsurface layers of the bay and gulf. The most significant difference was the presence of Pacific Intermediate Water (PIW) in the gulf, which does not intrude into the bay due to the barrier created by the sill at the mouth. The T-S diagrams revealed the presence of Gulf of California Water (GCW), Subtropical Subsurface Water (SSW) and PIW in May. In July, however, four water masses were identified: GCW, Equatorial Surface Water (ESW), SSW and PIW. In October, a significant amount of ESW and a considerable decrease in GCW were detected, but in February only GCW and SSW were found. This study shows important hydrographic seasonal variability in the area of the North Mouth, with marked differences between the bay and the gulf, contributing to the understanding of the regional oceanography. [ABSTRACT FROM AUTHOR]

Published
2007
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