Preprints
https://doi.org/10.2139/ssrn.6429182
https://doi.org/10.2139/ssrn.6429182
28 Aug 2026
 | 28 Aug 2026
Status: this preprint is open for discussion and under review for Biogeosciences (BG).

Evaluation of Partitioning Methods to Identify Timescale-Dependent Drivers of Light Use Efficiency in a Wet Tropical Forest

Julia Bigwood, Jochen Stutz, Milagros Rodriguez-Caton, Troy Magney, Diego Dierick, Nicholas Parazoo, Gregory R. Goldsmith, Sol Cooperdock, and Ulrike Seibt

Abstract. Tropical forests play a major role in the global terrestrial carbon cycle; however, substantial uncertainties remain regarding their capacity to continue acting as a carbon sink under changing climate conditions. This uncertainty is driven largely by the limited number of carbon flux observations in tropical regions. Using eddy covariance (EC) measurements over an 11-month period at La Selva, Costa Rica, we quantified net ecosystem exchange (NEE) and evaluated partitioning methods to estimate gross primary production (GPP) and ecosystem respiration. Daytime partitioning using morning flux data introduced substantial variability in respiration estimates due to rapidly changing micrometeorological conditions. In contrast, daytime afternoon, nighttime, and sundown partitioning methods produced strong agreement and physiologically realistic results. We therefore use the afternoon daytime partitioning method for subsequent light use efficiency (LUE) analysis. The La Selva rainforest functioned as a strong temporally stable carbon sink with no detectable seasonal trend, averaging 2.5 µmol CO2 m-2 s-1, corresponding to an annual carbon uptake of 947 g C m-2 yr-1. GPP averaged 11.8 µmol CO2 m-2 s-1. Random forest modeling revealed timescale-dependent environmental controls on LUE, with photosynthetically active radiation dominating short-term variability, while temperature and atmospheric moisture increasingly constrained productivity at weekly timescales. VPD and temperature exerted a strong negative effect on half-hourly LUE, indicating vulnerability to increasing atmospheric dryness. Our findings demonstrate that partitioning method choice and temporal scale strongly shape inferred GPP magnitude and drivers in this wet tropical forest, with important implications for interpreting carbon flux estimates from EC measurements.

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Julia Bigwood, Jochen Stutz, Milagros Rodriguez-Caton, Troy Magney, Diego Dierick, Nicholas Parazoo, Gregory R. Goldsmith, Sol Cooperdock, and Ulrike Seibt

Status: open (until 09 Oct 2026)

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Julia Bigwood, Jochen Stutz, Milagros Rodriguez-Caton, Troy Magney, Diego Dierick, Nicholas Parazoo, Gregory R. Goldsmith, Sol Cooperdock, and Ulrike Seibt
Julia Bigwood, Jochen Stutz, Milagros Rodriguez-Caton, Troy Magney, Diego Dierick, Nicholas Parazoo, Gregory R. Goldsmith, Sol Cooperdock, and Ulrike Seibt
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Latest update: 28 Aug 2026
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Short summary
Tropical forests absorb a large amount of carbon from the atmosphere. Even so, we still have a limited understanding of how this may change with a changing climate. We measured carbon exchange in a Costa Rican rainforest and found that the forest remained a strong carbon sink. However, estimates of carbon uptake depended on how measurements are analyzed and the time period considered, highlighting important challenges for predicting tropical forest responses to climate change.
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