Tracing Diurnal Variations of Atmospheric CO <sub>2</sub> , O <sub>2</sub> , and δ13 ${\boldsymbol{\delta }}^{\mathbf{13}}$CO <sub>2</sub> Over a Tropical and a Temperate Forest

Abstract We analyze the diurnal variability of atmospheric , , and CO 2 above the canopies of two contrasting ecosystems: the Amazon tropical forest and the Loobos temperate forest. Using a coupled forest‐atmosphere model constrained by tower‐based and aircraft observations, we quantify the role of atmospheric processes—including entrainment, subsidence, and cloud ventilation—in shaping the diurnal amplitude, or diurnal range (DR), of carbon‐cycle tracers. Our results show that atmospheric processes can contribute more than twice as much as surface processes to DR. Misrepresenting these influences leads to substantial errors in interpreting observations and modeling tracer variability. We propose using DR as a metric to evaluate atmospheric tracer transport models and to compare site‐level measurements. We present a roadmap to identify which atmospheric or surface processes are poorly represented when modeled and observed DR diverge.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-10-15
DOI
https://doi.org/10.1029/2025gl118016
Primary Topic
Atmospheric and Environmental Gas Dynamics
Type
article
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article

Tracing Diurnal Variations of Atmospheric CO 2 , O 2 , and δ13 ${\boldsymbol{\delta }}^{\mathbf{13}}$CO 2 Over a Tropical and a Temperate Forest

John Bharat Miller, Oscar Hartogensis, Cléo Quaresma Dias‐Júnior, Jordi Vilà-Guerau De Arellano et al.
Geophysical Research Letters
Atmospheric and Environmental Gas Dynamics
article

Tracing Diurnal Variations of Atmospheric CO 2 , O 2 , and δ13 ${\boldsymbol{\delta }}^{\mathbf{13}}$CO 2 Over a Tropical and a Temperate Forest

John Bharat Miller, Oscar Hartogensis, Cléo Quaresma Dias‐Júnior, Jordi Vilà-Guerau De Arellano, Robbert Moonen, Kim A. P. Faassen, Ronald Hutjes, Luiz A. T. Machado, Raquel González‐Armas, Thomas Röckmann, Bert A. M. Kers, B.G. Heusinkveld, Wouter Mol, Getachew Agmuas Adnew, M. K. van der Molen, Henk Snellen, Ingrid T. Luijkx, Santiago Botía, Hugo J. de Boer, Hella van Asperen, Shujiro Komiya, Gerbrand Koren, Sam P. Jones, Vincent S. de Feiter, Lucas Hulsman, Giordane Martins
article en

Abstract

Abstract We analyze the diurnal variability of atmospheric , , and CO 2 above the canopies of two contrasting ecosystems: the Amazon tropical forest and the Loobos temperate forest. Using a coupled forest‐atmosphere model constrained by tower‐based and aircraft observations, we quantify the role of atmospheric processes—including entrainment, subsidence, and cloud ventilation—in shaping the diurnal amplitude, or diurnal range (DR), of carbon‐cycle tracers. Our results show that atmospheric processes can contribute more than twice as much as surface processes to DR. Misrepresenting these influences leads to substantial errors in interpreting observations and modeling tracer variability. We propose using DR as a metric to evaluate atmospheric tracer transport models and to compare site‐level measurements. We present a roadmap to identify which atmospheric or surface processes are poorly represented when modeled and observed DR diverge.

Geophysical Research LettersVol. 52(20)
University of Copenhagen (DK), National Oceanic and Atmospheric Administration (US), University of Groningen (NL), University of Applied Sciences Utrecht (NL), Universidade de São Paulo (BR), Instituto Nacional de Pesquisas da Amazônia (BR), Utrecht University (NL), Instituto Federal de Educação, Ciência e Tecnologia do Pará (BR), NOAA Chemical Sciences Laboratory (US), Max Planck Institute for Biogeochemistry (DE), Wageningen University & Research (NL)
Openalex Percentile: Top 73%
Atmospheric and Environmental Gas Dynamics
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