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remains unclear to what extent. Complementary tracers of the carbon cycle, such as carbon dioxide and carbonyl sulfide isotopologues can provide novel insights on ecosystem processes and help constrain
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to quantify experimentally and numerically due to the spatial variability of the microclimate within an agroforestry system and the existence of antagonistic processes. Nevertheless, successfully predicting
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of the effects of policies on a few promising cases, for example using synthetic control or break detection methods. Details: https://cesaer-datas.inra.fr/index.php/s/dsoPU1vjLLCgTRh Where to apply E
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