Abstract

Coffee is one of the most commonly traded agricultural commodities globally. It is important for the livelihoods of over 25 million families worldwide, but it is also a crop sensitive to climate change, which has forced producers to implement management practices with effects on carbon balance and water use efficiency (WUE) that are not well understood due to data scarcity. From this perspective, we propose crop canopy coupling to the atmosphere (Ώ) as an index of resilience and stability. We undertook an integrated observational approach for the scaling-up of measurements along the soil–plant–atmosphere continuum at different stages of the coffee crop phenological cycle. Additionally, we develop this perspective under pronounced climatic seasonality and variability, in order to assess carbon balance, WUE, and agroecosystem resilience in a sun-grown coffee field. Further, we devised a field layout that facilitates the measurement of intrinsic, instantaneous, and actual water use efficiency and the assessment of whether coffee fields differ in canopy structure, complexity, and agronomic management and whether they are carbon sources or sinks. Partitioning soil and canopy energy balances and fluxes in a sun-grown coffee field using eco-physiological techniques at the leaf and whole plant levels (i.e., sap flow and gas exchange), as proposed here, will allow the scaling-up to whole fields in the future. Eddy covariance was used to assess real-time surface fluxes of carbon, gross primary productivity (GPP), and evapotranspiration, as well as components of the energy balance and WUE. The preliminary results support the approach used here and suggested that coffee fields are CO2 sinks throughout the year, especially during fruit development, and that the influence of seasonality drives the surface–atmosphere coupling, which is dominant prior to and during the first half of the rainy season. The estimated WUE showed consistency with independent studies in coffee crops and a marked seasonality driven by the features of the rainy season. A plan for the arborization of the coffee agroecosystem is suggested and the implications for WUE are described. Future comparison of sun- and shade-grown coffee fields and incorporation of other variables (i.e., crop coefficient-KC for different leaf area index (LAI) values) will allow us to better understand the factors controlling WUE in coffee agroecosystems.

Highlights

  • Introduction conditions of the Creative CommonsCoffee is one of the most popular beverages, consumed by about one-third of the world’s population; it is one of the most commonly traded agricultural commodities worldwide [1]

  • We used the eddy covariance (EC) method and focused on the quantification of the water and carbon balance, as well as the estimation of evapotranspiration, in order to determine the general components of the energy balance and their associated fluxes, RN, H, E, S (Soil heat flux), and FC (Carbon assimilation), in this case, E is estimated based on the surface fluxes balance approximation

  • Canopy development and structure determine the leaf area index (LAI), light interception, and crop productivity, and they greatly affect the partitioning of the radiative flux between evapotranspiration, heat, and soil heat fluxes

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Summary

Introduction conditions of the Creative Commons

Coffee is one of the most popular beverages, consumed by about one-third of the world’s population; it is one of the most commonly traded agricultural commodities worldwide [1]. To better understand the effects of climate change and variability on coffee production systems, we need to face the limitations imposed by data scarcity At this point, meteorological data to link environmental dynamism and climatic changes to crop productivity are scant, and it is crucial to upscale the analysis to include the physiological responses to environmental changes. Meteorological data to link environmental dynamism and climatic changes to crop productivity are scant, and it is crucial to upscale the analysis to include the physiological responses to environmental changes To fill these gaps, a multi-scale approach is necessary so that the soil–plant–atmosphere continuum (SPAC) can be used as a framework to understand the impacts of climate and the feedback at the crop scale, and to enhance our capacity to deliver an integral model of climate-smart agriculture to producers. The current perspective was only focused on a sungrown coffee field, the same setup will be implemented in a shade-grown coffee field in the near future so that the impact of shade on WUE and the coupling between plants and the atmosphere can be addressed (Section 4)

Feedback in the Soil–Plant–Atmosphere Continuum
Gas Exchange at the Canopy Scale
Canopy–Atmosphere Coupling
Preliminary Results
The Study Site
Long Term Climatology
Coffee Field Structure
Surface Fluxes
Annual Cycle of Surface Fluxes
Annual Cycle of CO2 Fluxes and Productivity
Soil CO2 Fluxes and Water Content
Sap Flow Measurements and Latent Heat Flux Partitioning
Water Use Efficiency in the Agroecosystem
Shading the Coffee Agroecosystem
Concluding Remarks
Full Text
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