Vol. 30 (2020)
Artículos de Investigación

Climate characterization and temperature variability of the coastal plain of Nayarit and their teleconnection with ENSO and PDO

Areli Nájera González, Mtra
Estudiante del Doctorado en Ciencias en Biosistemática, Ecología y Manejo de Recursos Naturales y Agrícolas en la Universidad de Guadalajara, Centro Universitario de la Costa, Av. Universidad 203, Delegación Ixtapa, CP. 48280 Puerto Vallarta, Jalisco, México
Fátima Maciel Carrillo González
Universidad de Guadalajara
Oyolsi Nájera González, Dr
Profesor Investigador, Cuerpo Académico Recursos Naturales, Secretaría de Investigación y Posgrado, Universidad Autónoma de Nayarit, Ciudad de la Cultura "Amado Nervo", C.P. 63155 Tepic, Nayarit. México
Rosa María Chávez Dagostino, Dra
Profesor Investigador, Departamento de Ciencias Biológicas de la Universidad de Guadalajara, Centro Universitario de la Costa, Av. Universidad 203, Delegación Ixtapa, CP. 48280 Puerto Vallarta, Jalisco, México

Published 2020-12-02

How to Cite

González, A. N., Carrillo González, F. M., González, O. N., & Dagostino, R. M. C. (2020). Climate characterization and temperature variability of the coastal plain of Nayarit and their teleconnection with ENSO and PDO. Acta Universitaria, 30, 1–21. https://doi.org/10.15174/au.2020.2651

Abstract

To understand climate change, climate variability should be studied. Climate variability focuses on denoting those weather behaviors that are considered out of the ordinary and their relationship with the planet’s natural variation, such as El Niño-Southern Oscillation (ENSO) and the Pacific Decadal Oscillation (PDO) phenomena. The objective of this research was to know the climatic variability of a fragment of the coastal plain of the state of Nayarit, Mexico, a predominant area of mangrove cover, lagoons, and agricultural use. The investigation is presented in three parts: climatic characterization, variability analysis (annual, monthly, and interdecadal), and its teleconnection with ENSO and PDO indices. The interdecadal variation showed an increase in the minimum temperature, a decrease in the maximum temperature, and a decrease in the precipitation in the last two decades. A 30% correlation was found with ENSO (the highest correlations in the summer months) and 25% with PDO.