Reconfiguración del Régimen Térmico y Estabilidad Pluviométrica en Manabí mediante ERA5-Land y Proyecciones Climáticas CMIP6

Palabras clave: demarcación Hidrográfica de Manabí, variabilidad climática, ERA5-Land, modelos CMIP6, amplitud térmica diaria

Resumen

La Demarcación Hidrográfica de Manabí (DHM), situada en la costa ecuatoriana del Pacífico tropical oriental, es un área con una fuerte influencia océano-atmósfera y con baja densidad de estaciones meteorológicas, lo que dificulta caracterizar de manera robusta su variabilidad climática. Esta investigación, fusiona el reanálisis ERA5-Land (procesado mediante Google Earth Engine) con datos de series históricas de diez modelos climáticos del Proyecto de Intercomparación de Modelos Acoplados fase 6 (CMIP6), para evaluar las tendencias de temperatura media, máxima y mínima, la amplitud térmica diaria (DTR), la precipitación y el balance hídrico superficial de la DHM entre 1964 y 2012, además de evaluar la fidelidad de los modelos climáticos frente a las observaciones satelitales. Las tendencias se identificaron mediante la prueba no paramétrica de Mann-Kendall y el estimador de pendiente de Sen. Los resultados revelan que la temperatura media anual fue estable (pendiente de Sen = +0,013 °C década⁻¹; p = 0,845), aunque la temperatura máxima disminuyó (−0151 °C década⁻¹; p = 0,063) y la mínima aumentó (+0,070 °C década⁻¹; p = 0,062), y se asociaron con la amplitud térmica diaria que mostró una disminución significativa (−0,236 °C década⁻¹; p = 0,001). La precipitación anual mostró una tendencia ligeramente positiva (+53,85 mm década⁻¹; τ = 0,115; p = 0,248). La evaluación del conjunto CMIP6 mostró un sesgo cálido sistemático en la amplitud térmica (sesgo promedio = +3,30 °C) y un sesgo seco en la precipitación (PBIAS promedio = −5,3%), siendo los modelos con el mejor rendimiento relativo GFDL-ESM4, EC-Earth3 y ACCESS-ESM1-5. Demostrando que, el cambio climático en la DHM no se refleja en un calentamiento uniforme, sino que es una reestructuración del régimen térmico diario modulado por la dinámica del Pacífico oriental, la Oscilación del Sur de El Niño y el balance energético superficial, situación que los modelos CMIP6 reproducen parcialmente.

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Publicado
2026-07-28
Cómo citar
Rivadeneira Vera , J. F., & Zambrano Mera, Y. E. (2026). Reconfiguración del Régimen Térmico y Estabilidad Pluviométrica en Manabí mediante ERA5-Land y Proyecciones Climáticas CMIP6. Ciencia Latina Revista Científica Multidisciplinar, 10(4), 357-383. https://doi.org/10.37811/cl_rcm.v10i4.24995
Sección
Ciencias y Tecnologías