School of Geographical Sciences, University of Bristol, Bristol, UK.
Faculty of Environment, Science and Economy, University of Exeter, Exeter, UK.
Nature. 2023 Mar;615(7952):436-442. doi: 10.1038/s41586-022-05679-w. Epub 2023 Mar 15.
The globally important carbon sink of intact, old-growth tropical humid forests is declining because of climate change, deforestation and degradation from fire and logging. Recovering tropical secondary and degraded forests now cover about 10% of the tropical forest area, but how much carbon they accumulate remains uncertain. Here we quantify the aboveground carbon (AGC) sink of recovering forests across three main continuous tropical humid regions: the Amazon, Borneo and Central Africa. On the basis of satellite data products, our analysis encompasses the heterogeneous spatial and temporal patterns of growth in degraded and secondary forests, influenced by key environmental and anthropogenic drivers. In the first 20 years of recovery, regrowth rates in Borneo were up to 45% and 58% higher than in Central Africa and the Amazon, respectively. This is due to variables such as temperature, water deficit and disturbance regimes. We find that regrowing degraded and secondary forests accumulated 107 Tg C year (90-130 Tg C year) between 1984 and 2018, counterbalancing 26% (21-34%) of carbon emissions from humid tropical forest loss during the same period. Protecting old-growth forests is therefore a priority. Furthermore, we estimate that conserving recovering degraded and secondary forests can have a feasible future carbon sink potential of 53 Tg C year (44-62 Tg C year) across the main tropical regions studied.
由于气候变化、森林砍伐和火灾退化,未受干扰的古老热带雨林这一全球重要的碳汇正在减少。目前,热带次生林和退化林的恢复面积约占热带森林面积的 10%,但它们能积累多少碳仍不确定。在这里,我们量化了三个主要连续热带湿润地区(亚马逊、婆罗洲和中非)恢复森林的地上碳(AGC)汇。基于卫星数据产品,我们的分析包括受关键环境和人为驱动因素影响的退化和次生林的异质时空增长模式。在恢复的头 20 年,婆罗洲的再生速率比中非和亚马逊分别高出 45%和 58%。这是由于温度、水分亏缺和干扰等变量的影响。我们发现,在 1984 年至 2018 年期间,退化和次生林的再生过程中积累了 107 太克碳/年(90-130 太克碳/年),抵消了同期湿润热带森林损失所产生的 26%(21-34%)的碳排放。因此,保护古老森林是当务之急。此外,我们估计,在主要热带地区,保护退化和次生林的恢复可以实现未来 53 太克碳/年(44-62 太克碳/年)的可行碳汇潜力。