Department of Civil and Environmental Engineering, Washington State University, Pullman, WA, USA.
Key Laboratory for Semi-Arid Climate Change of the Ministry of Education, College of Atmospheric Sciences, Lanzhou University, Lanzhou, China.
Nat Commun. 2020 Apr 3;11(1):1665. doi: 10.1038/s41467-020-15515-2.
Drylands cover 41% of Earth's surface and are the largest source of interannual variability in the global carbon sink. Drylands are projected to experience accelerated expansion over the next century, but the implications of this expansion on variability in gross primary production (GPP) remain elusive. Here we show that by 2100 total dryland GPP will increase by 12 ± 3% relative to the 2000-2014 baseline. Because drylands will largely expand into formerly productive ecosystems, this increase in dryland GPP may not increase global GPP. Further, GPP per unit dryland area will decrease as degradation of historical drylands outpaces the higher GPP of expanded drylands. Dryland expansion and climate-induced conversions among sub-humid, semi-arid, arid, and hyper-arid subtypes will lead to substantial changes in regional and subtype contributions to global dryland GPP variability. Our results highlight the vulnerability of dryland subtypes to more frequent and severe climate extremes and suggest that regional variations will require different mitigation strategies.
旱地覆盖了地球表面的 41%,是全球碳汇中年际变化最大的来源。预计在下个世纪,旱地将加速扩张,但这种扩张对总初级生产力(GPP)变化的影响仍不清楚。在这里,我们表明,到 2100 年,相对于 2000-2014 年的基线,旱地的总 GPP 将增加 12±3%。由于旱地将主要扩张到以前生产力较高的生态系统,因此旱地 GPP 的增加可能不会增加全球 GPP。此外,随着历史旱地的退化超过扩张旱地的更高 GPP,旱地每单位面积的 GPP 将减少。亚湿润、半干旱、干旱和超干旱亚型之间的气候诱导转换将导致旱地对全球旱地 GPP 变化的区域和亚型贡献发生重大变化。我们的研究结果突出了旱地亚型对更频繁和更严重气候极端事件的脆弱性,并表明区域变化将需要不同的缓解策略。