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José P. Vega-Camarena, Luis Brito-Castillo, Luis F. Pineda-Martínez and Luis M. Farfán
In the warm season, El Niño/Southern Oscillation (ENSO) causes periods with more rain in Northern Mexico during its positive phase, while less rainfall is recorded in the southern regions during the negative phase. This research study evaluates the varia...
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Emiliano Gorr-Pozzi, Héctor García-Nava, Marco Larrañaga, Melissa G. Jaramillo-Torres and Manuel G. Verduzco-Zapata
Most wave energy converters (WECs) are designed to operate in high-latitude energetic seas, limiting their performance in regions usually dominated by milder conditions. The present study assesses the performance of complete test-stage WECs in farms that...
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Alejandro García Huante, Yandy Rodríguez Cueto, Rodolfo Silva, Edgar Mendoza and Luis A. Vega
The energy potential of the oceanic thermal gradients of the Mexican Pacific Ocean was valued theoretically, using seasonal oceanographic data on surface and 1000 m depth ocean temperatures from 1955 to 2013, taken from the World Ocean Database (WOD). Th...
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The interannual variability of near-coastal eastern North Pacific tropical cyclones is described using a data set of cyclone tracks constructed from U.S. and Mexican oceanic and atmospheric reports for the period 1951-2006. Near-coastal cyclone counts ar...
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E. ROMERO VADILLO,O. ZAYTSEV,R. MORALES PÉREZ
The principal area of tropical cyclogenesis in the tropical eastern Pacific Ocean is offshore in the Gulf of Tehuantepec, between 8 and 15º N, and most of these cyclones move towards the west and northwest during their initial phase. Historical analys...
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B. MENDOZA,D. MARAVILLA,E. JÁUREGUI
Three minimum extreme temperature series from meteorological stations located in or near the Mexican Pacific coast, Acapulco, Comitán and Manzanillo, are spectrally analyzed. The series cover a period from 1941 to 1981. The sp...
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V. MANUEL MENDOZA,E. E. VILLANUEVA,JULIAN ADEM
Using an integrated mixed layer model we carry out a simulation of the annual cycle of the sea surface temperature (SST) and of the mixed layer depth (MLD) in the Gulf of México. We also compute the annual cycle of the entrainment velocit...
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