11/20/2023 0 Comments Sea breeze daytimeKeywords: Complex Empirical Orthogonal Function Analysis, surface wind variability, cold northerlies, Yucatán Peninsula.Įl equilibrio entre los fenómenos atmosféricos sinópticos y la brisa marina puede The results of this work have important implications for atmospheric pollutantĭispersion, wind wave generation and coastal erosion, among others. Second mode during this period is the occurrence of peninsula-wide sea breeze. A distinctive phenomenon seen in the high frequencies of the In this period cold fronts and tropical systems (mode 2) exert milder influence Mode) while land breezes exhibit lesser dominance than sea breezes (third mode). Peninsula is dominated by sea breezes accentuated at the western shelf (first By the end of this season, the influence of tropical systems,Īlthough smaller, is noticeable (third mode). Higher amplitude during the nighttime (land breezes) than during the daytime Show that for the period from October to March, cold fronts dominate in twoĭifferent patterns (first two modes), which damp the local winds that show Low-frequency temporal behavior that can be associated with the modes. The time series obtained from the CEOF analysis, to study the high and High-pass/low-pass filtering was applied to (May 2007-May 2017) of modeled surface winds from the North American Mesoscaleįorecast System (hereafter, NAM). We performed a Complex Empirical Orthogonal Function (CEOF) analysis on 10 years Variability over the surface wind field of the Yucatán Peninsula is described. In this paper, aĬomprehensive study to understand the quasi-permanent patterns of such ![]() Influence atmospheric circulation in coastal regions. The balance between synoptic and sea breeze atmospheric phenomena can profoundly
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