Soil moisture drives the spatiotemporal patterns of asymmetry in vegetation productivity responses across China

环境科学 生态系统 植被(病理学) 生产力 陆地生态系统 含水量 水槽(地理) 碳汇 土壤水分 土壤碳 生态学 大气科学 自然地理学 土壤科学 地理 生物 地质学 宏观经济学 病理 地图学 经济 岩土工程 医学
作者
Qiang Chang,Honglin He,Xiaoli Ren,Li Zhang,Lili Feng,Yan Lv,Mengyu Zhang,Qian Xu,Weihua Liu,Yonghong Zhang,Tianxiang Wang
出处
期刊:Science of The Total Environment [Elsevier]
卷期号:855: 158819-158819 被引量:6
标识
DOI:10.1016/j.scitotenv.2022.158819
摘要

Increasingly drastic global change is expected to cause hydroclimatic changes, which will influence vegetation productivity and pose a threat to the terrestrial carbon sink. Asymmetry represents an imbalance between vegetation growth and loss of growth during dry and wet periods, respectively. However, the mechanisms of asymmetric plant responses to hydrological changes remain poorly understood. Here, we examined the spatiotemporal patterns of asymmetric responses of vegetation productivity across terrestrial ecosystems in China. We analyzed several observational and satellite-based datasets of plant productivity and several reanalyzed datasets of hydroclimatic variables from 2001 to 2020, and used a random forest model to assess the importance of hydroclimatic variables for these responses. Our results showed that the productivity of >50 % of China's vegetated areas showed a more positive asymmetry (2.3 ± 9.4 %) over the study period, which were distributed broadly in northwest China (mainly grasslands and sparse vegetation ecosystems). Negative asymmetries were most common in forest ecosystems in northeast China. We demonstrated that one-third of vegetated areas tended to exhibit significant changes in asymmetry during 2001–2020. The trend towards stronger positive asymmetry (0.95 % yr−1) was higher than that towards stronger negative asymmetry (−0.55 % yr−1), which is beneficial for the carbon sink. We further showed that in China, soil moisture was a more important driver of spatiotemporal changes in asymmetric productivity than precipitation. We identified thresholds of surface soil moisture (20–30 %, volume water content) and root-zone soil moisture (200–350 mm, equivalent water height) that were associated with changes in asymmetry. Our findings highlight the necessity of considering the dynamic responses of vegetation to hydrological factors in order to fully understand the physiological growth processes of plants and avoid the possible loss of productivity due to future climate change.
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