The variability of microclimate in the Amazon Rainforest

• A network of 145 sensors recorded nearly four million temperature readings (2016–2023), offering unprecedented insights into Amazonian microclimate variability. • Microclimate buffering capacity against macroclimatic temperatures is 8.6 % greater during the rainy season, highlighting the role of precipitation in thermal regulation. • Canopy height and foliage density enhance microclimate buffering, while terrain slope and solar radiation negatively impact it. • Findings highlight the importance of maintaining forest structural integrity to preserve stable microclimatic conditions essential for biodiversity conservation. The Amazon rainforest represents one of the most biodiverse places on Earth. However, the temperature experienced by organisms inside Amazonian forests, and the biophysical factors regulating microclimate, remain understudied. Microclimate patterns influence the nuances of ecological processes such as nutrient cycling, species dynamics, and tree regeneration, which cannot be captured by coarse resolution free-air temperature datasets. This study presents an unprecedented effort to measure microclimate across different biogeographical sites using standardized in-situ data collection and methodology. We analyzed temperature data from 145 sensors across eight distinct areas within the Amazon basin. From 2016 to 2023, nearly four million temperature readings revealed that Amazonian understory temperatures remained consistently lower than those of the surrounding macroclimate. The central Amazon exhibited the greatest difference between microclimate and macroclimate temperatures. All monitored sites exhibit higher buffering capacity against macroclimate during the rainy season than in the dry season. Higher precipitation, Leaf Area Index, and canopy height enhance microclimatic buffering capacity, while increased terrain slope exert negative effects. Our study provides new insights into the spatial and temporal patterns of microclimate across the Amazon basin, thus advancing our understanding of the impacts of climate change on the Amazonian Forest ecosystem.

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Publication Details

Journal
Agricultural and Forest Meteorology
Published
2025-10-08
DOI
https://doi.org/10.1016/j.agrformet.2025.110866
Citations
1
Primary Topic
Urban Heat Island Mitigation
Type
article
Field-Weighted Citation Impact
0.80
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The variability of microclimate in the Amazon Rainforest

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1 citations
Agricultural and Forest Meteorology
Urban Heat Island Mitigation
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article

The variability of microclimate in the Amazon Rainforest

Samuel de Pádua Chaves e Carvalho, Eduardo Eiji Maeda, Sabina Cerruto Ribeiro, Darlene Gris, Carolina V. Castilho, Ilya M. D. Maclean, José Luís Camargo, Raphael Tapajós, Wilderclay Machado, Leena Kalliovirta, Zhimin Ma, Miércio Júnior, Paulo de Jesus Feitosa Paes do Nascimento
article en
1 citations

Abstract

• A network of 145 sensors recorded nearly four million temperature readings (2016–2023), offering unprecedented insights into Amazonian microclimate variability. • Microclimate buffering capacity against macroclimatic temperatures is 8.6 % greater during the rainy season, highlighting the role of precipitation in thermal regulation. • Canopy height and foliage density enhance microclimate buffering, while terrain slope and solar radiation negatively impact it. • Findings highlight the importance of maintaining forest structural integrity to preserve stable microclimatic conditions essential for biodiversity conservation. The Amazon rainforest represents one of the most biodiverse places on Earth. However, the temperature experienced by organisms inside Amazonian forests, and the biophysical factors regulating microclimate, remain understudied. Microclimate patterns influence the nuances of ecological processes such as nutrient cycling, species dynamics, and tree regeneration, which cannot be captured by coarse resolution free-air temperature datasets. This study presents an unprecedented effort to measure microclimate across different biogeographical sites using standardized in-situ data collection and methodology. We analyzed temperature data from 145 sensors across eight distinct areas within the Amazon basin. From 2016 to 2023, nearly four million temperature readings revealed that Amazonian understory temperatures remained consistently lower than those of the surrounding macroclimate. The central Amazon exhibited the greatest difference between microclimate and macroclimate temperatures. All monitored sites exhibit higher buffering capacity against macroclimate during the rainy season than in the dry season. Higher precipitation, Leaf Area Index, and canopy height enhance microclimatic buffering capacity, while increased terrain slope exert negative effects. Our study provides new insights into the spatial and temporal patterns of microclimate across the Amazon basin, thus advancing our understanding of the impacts of climate change on the Amazonian Forest ecosystem.

Agricultural and Forest MeteorologyVol. 375
Finnish Meteorological Institute (FI), Universidade Federal do Oeste do Pará (BR), Universidade Federal do Acre (BR), University of Helsinki (FI), Universidade Federal Rural do Rio de Janeiro (BR), Instituto Nacional de Pesquisas da Amazônia (BR), University of Exeter (GB), Sustainability Institute (ZA), Sustainable Development Institute (US), Universidade Estadual de Roraima (BR), General Electric (Finland) (FI), Institute for Sustainable Development (ET), Universidade Federal de Roraima (BR)
Openalex Percentile: Top 24%
Urban Heat Island Mitigation
0.80
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