Decreased precipitation in the late growing season weakens an ecosystem carbon sink in a semi‐arid grassland. Issue 10 (3rd September 2021)

• Record Type: Journal Article
• Authors: Yang, Zhongling; Wei, Yueyue; Fu, Guangya; Xiao, Rui; Chen, Ji; Zhang, Yaojun; Wang, Dong; Li, Junyong
• Is Part Of: Journal of applied ecology. Volume 58:Issue 10(2021)
• Page Start: 2101
• Page End: 2112
• Publication Date: 2021-09-03
• Subjects: carbon processes -- carbon sink -- climate change -- decreased precipitation -- drought timing -- photosynthetic substrate -- plant community cover -- semi‐arid steppe; Agriculture -- Periodicals; Biology, Economic -- Periodicals; Agricultural ecology -- Periodicals; Applied ecology -- Periodicals; 577
• DOI: 10.1111/1365-2664.13942
• Languages: English
• ISSNs: 0021-8901

Abstract

Abstract: Net ecosystem gas exchange (NEE), a balance between gross ecosystem primary productivity (GPP) and ecosystem respiration (ER), is an important indicator of terrestrial ecosystem CO2 sink or source. Increasing frequency in droughts during different periods of the growing season may affect terrestrial ecosystem carbon (C) balance. However, detecting how drought timing controls ecosystem C processes is insufficiently explored because it is a challenge to accurately monitor and forecast drought dynamics. In a 5‐year (2015–2019) precipitation manipulation experiment in a temperate steppe in northern China, we imposed a 60% decrease in precipitation in the early (April–June, DEP) and late (July–September, DLP) growing seasons in plots under rainout shelters to simulate drought occurrence timing. The responses of GPP, ER and NEE to DEP and DLP were examined to determine how the timing of decreased precipitation affects CO2 fluxes. Both DEP and DLP reduced GPP and ER. Decreased precipitation in the late growing season reduced NEE due to a greater decline in GPP than ER. In contrast, the lack of an effect of DEP on NEE can be attributed to a proportional decline in GPP and ER. Reduced normalized difference vegetation index (NDVI) and GPP induced by decreased precipitation explained the decline in GPP and ER respectively. Drought in the late growing season weakened the ecosystem C sink. The result indicates a low resistance in net C uptake to DLP. However, we did not find evidence that previous precipitation decreases resulted in a lower overall rate of ecosystem C exchange, indicating a high resilience in C processes in this semi‐arid grassland. Synthesis and applications . Our study provides solid evidence that drought in the late growing season weakens ecosystem C sink in the semi‐arid grassland. The findings suggest that management practices aimed at enhancing water availability during the late growing season should be preferred for increasing C sequestration. Abstract : Our study provides solid evidence that drought in the late growing season weakens ecosystem carbon (C) sink in the semi‐arid grassland. The findings suggest that management practices aimed at enhancing water availability during the late growing season should be preferred for increasing C sequestration.