Observational Evidence of Intensified Extreme Seasonal Climate Events in a Conurbation Area Within the Eastern Amazon
2025
Everaldo Barreiros de Souza | Douglas Batista da Silva Ferreira | Ana Paula Paes dos Santos | Alan Cavalcanti da Cunha | João de Athaydes Silva Junior | Alexandre Melo Casseb do Carmo | Victor Hugo da Motta Paca | Thaiane Soeiro da Silva Dias | Waleria Pereira Monteiro Correa | Tercio Ambrizzi
This study presents an integrated assessment of four decades (1985&ndash:2023) of environmental and climate alterations in the principal metropolitan conurbation of the eastern Brazilian Amazon, encompassing Belé:m and its adjacent municipalities. By combining high-resolution land use/land cover (LULC) dynamics with in situ meteorological data, including understudied elements, such as relative humidity (RH) and wind speed, and satellite-derived precipitation estimates (CHIRPS v3), we advance the scientific understanding of regional climate trends. Our results document significant climate shifts, including pronounced dry-season warming (+1.5 °:C), atmospheric drying (&minus:4% in RH), attenuated wind patterns (&minus:0.4 m s&minus:1), and altered precipitation regimes, which exhibit strong spatiotemporal coupling with extensive forest loss (&minus:20%) and rapid urban expansion (+84%) between 1985 and 2023. Multivariate analyses reveal that these land&ndash:climate interactions are strongest during the dry regime, underscoring the role of surface&ndash:atmosphere feedbacks in amplifying regional changes. Comparative analysis of past (1980&ndash:1999) and present (2005&ndash:2024) decades demonstrates a marked intensification in the frequency and magnitude of extreme seasonal climate events. These findings elucidate a critical feedback mechanism that exacerbates climate risks in tropical urban areas. Consequently, we argue that mitigation public policies must prioritize the strict conservation of peri-urban forest fragments (vital for moisture recycling and local climate regulation) and the strategic implementation of green infrastructure aligned with prevailing wind patterns to enhance thermal comfort and resilience to hydrological extremes.
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