“…In seasonally dry ecosystems such as the TDF, carbon exchanges are highly dependent on the annual and seasonal variations of precipitation due the tight relation between water inputs and processes such as net primary production (NPP) [ Sala et al ., ; Méndez‐Barroso et al ., ], litter decomposition, and concomitant respiratory fluxes [ Fierer and Schimel , ; Anaya et al ., ] and transpiration [ Scott et al ., ; Reyes‐García et al ., ; Peng et al ., ], among other physiological and hydrological processes [ Leuzinger and Korner , ; Cherwin and Knapp , ]. Variations in precipitation during the summer season, for example, a delayed start of the monsoon, are recognized to affect the annual carbon balance through alterations of productivity and respiration [ Hutyra et al ., ].…”