Anthropogenic Activity in the Topo-Climatic Interaction of the Tapajós River Basin, in the Brazilian Amazon

Author:

Franco Vânia dos Santos12ORCID,Lima Aline Maria Meiguins de1ORCID,Oliveira Rodrigo Rafael Souza de3ORCID,Souza Everaldo Barreiros de1ORCID,Sodré Giordani Rafael Conceição4,Santos Diogo Correa2ORCID,Adami Marcos5ORCID,Serrão Edivaldo Afonso de Oliveira2ORCID,Dias Thaiane Soeiro da Silva1

Affiliation:

1. Programa de Pós-Graduação em Ciências Ambientais, Universidade Federal do Pará, Belém 66075-110, Brazil

2. Instituto Tecnológico Vale, Desenvolvimento Sustentável, Belém 66055-090, Brazil

3. Departamento de Geografia, Universidade do Estado do Pará, Belém 66050-540, Brazil

4. Faculdade de Meteorologia, Universidade Federal do Pará, Belém 66075-110, Brazil

5. Instituto Nacional de Pesquisas Espaciais—INPE, São José dos Campos 12227-010, Brazil

Abstract

This research aimed to analyze the relationship between deforestation (DFT) and climatic variables during the rainy (CHU+) and less-rainy (CHU−) seasons in the Tapajós River basin. Data were sourced from multiple institutions, including the Climatic Research Unit (CRU), Center for Weather Forecasts and Climate Studies (CPTEC), PRODES Program (Monitoring of Brazilian Amazon Deforestation Project), National Water Agency (ANA) and National Centers for Environmental Prediction/National Oceanic and Atmospheric Administration (NCEP/NOAA). The study assessed anomalies (ANOM) in maximum temperature (TMAX), minimum temperature (TMIN) and precipitation (PREC) over three years without the occurrence of the El Niño–Southern Oscillation (ENSO) atmospheric–oceanic phenomenon. It also examined areas with higher DFT density using the Kernel methodology and analyzed the correlation between DFT and climatic variables. Additionally, it assessed trends using the Mann–Kendall technique for both climatic and environmental data. The results revealed significant ANOM in TEMP and PREC. In PREC, the highest values of ANOM were negative in CHU+. Regarding temperature, the most significant values were positive ANOM in the south, southwest and northwestern regions of the basin. Concerning DFT density, data showed that the highest concentration was of medium density, primarily along the highways. The most significant correlations were found between DFT and TEMP during the CHU− season in the Middle and Lower Tapajós sub-basins, regions where the forest still exhibits more preserved characteristics. Furthermore, the study identified a positive trend in TEMP and a negative trend in PREC.

Publisher

MDPI AG

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