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Drought dominates the interannual variability in global terrestrial net primary production by controlling semi-arid ecosystems

机译:干旱通过控制半干旱生态系统统治全球陆地净初级生产的际变化

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Drought is a main driver of interannual variation in global terrestrial net primary production. However, how and to what extent drought impacts global NPP variability is unclear. Based on the multi-timescale drought index SPEI and a satellite-based annual global terrestrial NPP dataset, we observed a robust relationship between drought and NPP in both hemispheres. In the Northern Hemisphere, the annual NPP trend is driven by 19-month drought variation, whereas that in the Southern Hemisphere is driven by 16-month drought variation. Drought-dominated NPP, which mainly occurs in semi-arid ecosystems, explains 29% of the interannual variation in global NPP, despite its 16% contribution to total global NPP. More surprisingly, drought prone ecosystems in the Southern Hemisphere, which only account for 7% of the total global NPP, contribute to 33% of the interannual variation in global NPP. Our observations support the leading role of semi-arid ecosystems in interannual variability in global NPP and highlight the great impacts of long-term drought on the global carbon cycle.
机译:干旱是全球陆地净初级生产持续变化的主要驱动因素。然而,如何以及在多大程度上和在多大程度上和多大程度上影响全球NPP变异性尚不清楚。基于多时间尺度干旱指数Spei和基于卫星的年度全球陆地NPP数据集,我们在两个半球中观察到干旱和NPP之间的强大关系。在北半球,每年的NPP趋势是由19个月的干旱变化驱动,而在南半球的南半球是由16个月的干旱变化驱动的。尽管对全球全球NPP的贡献16%,但是主要发生在半干旱生态系统中的干旱占据的NPP,占全球NPP际变化的29%。更令人惊讶的是,南半球的干旱易发的生态系统,只占全球总NPP总数的7%,占全球NPP持续变化的33%。我们的观察支持半干旱生态系统在全球NPP中处于年间变异性的领先作用,并突出了长期干旱在全球碳循环中的巨大影响。

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