降水
环境科学
土壤呼吸
呼吸
气候变化
大气科学
全球变化
土壤水分
生态学
土壤科学
生物
植物
气象学
地质学
地理
作者
Yue Du,Ying‐Ping Wang,Dafeng Hui,Fanglong Su,Junhua Yan
摘要
Abstract Global warming intensifies the hydrological cycle, which results in changes in precipitation regime (frequency and amount), and will likely have significant impacts on soil respiration ( R s ). Although the responses of R s to changes in precipitation amount have been extensively studied, there is little consensus on how R s will be affected by changes in precipitation frequency (PF) across the globe. Here, we synthesized the field observations from 296 published papers to quantify the effects of PF on R s and its components using meta‐analysis. Our results indicated that the effects of PF on R s decreased with an increase in background mean annual precipitation. When the data were grouped by climate conditions, increased PF showed positive effects on R s under the arid condition but not under the semi‐humid or humid conditions, whereas decreased PF suppressed R s across all the climate conditions. The positive effects of increased PF mainly resulted from the positive response of heterotrophic respiration under the arid condition while the negative effects of decreased PF were mainly attributed to the reductions in root biomass and respiration. Overall, our global synthesis provided for the first time a comprehensive analysis of the divergent effects of PF on R s and its components across climate regions. This study also provided a framework for understanding and modeling responses of ecosystem carbon cycling to global precipitation change.
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