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Revisiting the cumulative effects of drought on global gross primary productivity based on new long‐term series data (1982–2018)

环境科学 蒸散量 温带气候 初级生产 植被(病理学) 降水 气候变化 气候学 灌木丛 干旱 生产力 自然地理学 地理 生态系统 生态学 地质学 病理 气象学 经济 宏观经济学 生物 医学
作者
Zhenyu Zhang,Weimin Ju,Yanlian Zhou,Xiaoyu Li
出处
期刊:Global Change Biology [Wiley]
卷期号:28 (11): 3620-3635 被引量:85
标识
DOI:10.1111/gcb.16178
摘要

Abstract Drought has broad and deep impacts on vegetation. Studies on the effects of drought on vegetation have been conducted over years. Recently, the cumulative effect of drought is recognized as another key factor affecting plant growth. However, global‐scale studies on this phenomenon are still lacking. Thus, based on new satellite based gross primary productivity (GPP) and multi‐temporal scale Standardized Precipitation Evapotranspiration Index data sets, we explored the cumulative effect duration (CED) of drought on global vegetation GPP and analyzed its variability across elevations and climatic zones. The main findings were as follows: (1) The cumulative effect of drought on GPP was widespread, with an average CED of 4.89 months. (2) CED of drought on GPP varied among vegetation types. Specifically, grasslands showed the longest duration, with an average value of 5.28 months, followed by shrublands (5.09 months), wetlands (5.03 months), croplands (4.85 months), savannas (4.58 months), and forestlands (4.57 months). (3) CED of drought on GPP changes with climate conditions. It decreased with the decrease of precipitation in the driest month (P dry ) and mean annual precipitation in tropical and arid climate zones, respectively. In both temperate and cold climate zones, CED of drought on GPP was shorter in areas with dry winter than that in areas with dry summer. It increased with the decrease of mean annual air temperature in tropical climate zones and decreased with the increase of summer temperature in temperate and cold climatic zones. (4) With increasing elevation, CED of drought on GPP showed a pattern of increasing (0–3000 m), then decreasing (3000–5000 m), and increasing again (>5000 m). Our findings highlight the heterogeneity of CED of drought on GPP, owing to differences in vegetation types, long‐term hydrothermal conditions, elevation, etc. The results could deepen our understanding of the effects of drought on global vegetation.
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