The role of interannual,seasonal, and synoptic climate on the carbon isotope ratio of ecosystem respiration at a semiarid woodland

The terrestrial carbon cycle is influenced by environmental variability at scales ranging from diurnal to interannual. Here, we present 5‐years of growing season (day 131–275) observations of the carbon isotope ratio of ecosystem respiration (δ¹³C_R) from a semiarid woodland. This ecosystem has a large necromass component resulting from 97%Pinus edulis mortality in 2002, is dominated by drought‐tolerant Juniperus monosperma trees, and experiences large variability in the timing and intensity of seasonal and synoptic water availability. Mean growing season δ¹³C_R was remarkably invariant (?23.57±0.4‰), with the exception of particularly enriched δ¹³C_R in 2006 following a winter with anomalously low snowfall. δ¹³C_R was strongly coupled to climate during premonsoon periods (～May to June), including fast (≤2 days) responses to changes in crown‐level stomatal conductance (G_c) and vapor pressure deficit (vpd) following rain pulses. In contrast, δ¹³C_R was relatively decoupled from G_c and environmental drivers during monsoon and postmonsoon periods (July–August and September, respectively), exhibiting only infrequent couplings of δ¹³C_R to vpd and soil water content (SWC) with longer lags (～8 days) and variable response slopes (both positive and negative). Notably, δ¹³C_R exhibited consistent dynamics after rainfall events, with depleted δ¹³C_R occurring within 1 h, progressive hourly δ¹³C_R enrichment over the remainder of the night, and net δ¹³C_R depletions over the multiple nights postevent in monsoon and postmonsoon periods. Overall this ecosystem demonstrated strong dependence of δ¹³C_R on precipitation, with an apparent dominance by the autotrophic δ¹³C signal in premonsoon periods when deep soil moisture is abundant and surface soil moisture is low, and weaker coupling during monsoonal periods consistent with increasing heterotrophic dominance when deep soil moisture has declined and surface moisture is variable.