Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, 11A, Datun Road, Chaoyang District, Beijing, 100101, China.
University of Chinese Academy of Sciences, 19A Yuquan Road, Shijingshan District, Beijing, 100049, China.
Sci Rep. 2018 Jan 11;8(1):493. doi: 10.1038/s41598-017-18798-6.
Variations in forest net primary productivity (NPP) reflects the combined effects of key climate variables on ecosystem structure and function, especially on the carbon cycle. We performed risk analysis indicated by the magnitude of future negative anomalies in NPP in comparison with the natural interannual variability to investigate the impact of future climatic projections on forests in China. Results from the multi-model ensemble showed that climate change risk of decreases in forest NPP would be more significant in higher emission scenario in China. Under relatively low emission scenarios, the total area of risk was predicted to decline, while for RCP8.5, it was predicted to first decrease and then increase after the middle of 21st century. The rapid temperature increases predicted under the RCP8.5 scenario would be probably unfavorable for forest vegetation growth in the long term. High-level risk area was likely to increase except RCP2.6. The percentage area at high risk was predicted to increase from 5.39% (2021-2050) to 27.62% (2071-2099) under RCP8.5. Climate change risk to forests was mostly concentrated in southern subtropical and tropical regions, generally significant under high emission scenario of RCP8.5, which was mainly attributed to the intensified dryness in south China.
森林净初级生产力(NPP)的变化反映了关键气候变量对生态系统结构和功能的综合影响,尤其是对碳循环的影响。我们进行了风险分析,根据未来 NPP 与自然年际变异性相比的负异常幅度,研究了未来气候预测对中国森林的影响。多模式集合的结果表明,在中国较高排放情景下,森林 NPP 减少的气候变化风险将更为显著。在相对较低的排放情景下,预计风险总面积将会下降,而在 RCP8.5 情景下,预计到 21 世纪中叶后会先下降后上升。RCP8.5 情景下预测的快速升温可能对森林植被的长期生长不利。除 RCP2.6 外,高风险区可能会增加。高风险区的比例预计将从 RCP8.5 情景下的 5.39%(2021-2050 年)增加到 27.62%(2071-2099 年)。森林面临的气候变化风险主要集中在亚热带和热带南部地区,在 RCP8.5 高排放情景下通常较为显著,这主要归因于中国南方的干旱加剧。