Department of Ecology, College of Urban and Environmental Science, and Key Laboratory for Earth Surface Processes of the Ministry of Education, Peking University, Beijing, 100871, China; State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing, 100093, China.
Glob Chang Biol. 2014 Jun;20(6):2019-30. doi: 10.1111/gcb.12512. Epub 2014 Jan 27.
Forests play an important role in regional and global carbon (C) cycles. With extensive afforestation and reforestation efforts over the last several decades, forests in East Asia have largely expanded, but the dynamics of their C stocks have not been fully assessed. We estimated biomass C stocks of the forests in all five East Asian countries (China, Japan, North Korea, South Korea, and Mongolia) between the 1970s and the 2000s, using the biomass expansion factor method and forest inventory data. Forest area and biomass C density in the whole region increased from 179.78 × 10(6) ha and 38.6 Mg C ha(-1) in the 1970s to 196.65 × 10(6) ha and 45.5 Mg C ha(-1) in the 2000s, respectively. The C stock increased from 6.9 Pg C to 8.9 Pg C, with an averaged sequestration rate of 66.9 Tg C yr(-1). Among the five countries, China and Japan were two major contributors to the total region's forest C sink, with respective contributions of 71.1% and 32.9%. In China, the areal expansion of forest land was a larger contributor to C sinks than increased biomass density for all forests (60.0% vs. 40.0%) and for planted forests (58.1% vs. 41.9%), while the latter contributed more than the former for natural forests (87.0% vs. 13.0%). In Japan, increased biomass density dominated the C sink for all (101.5%), planted (91.1%), and natural (123.8%) forests. Forests in South Korea also acted as a C sink, contributing 9.4% of the total region's sink because of increased forest growth (98.6%). Compared to these countries, the reduction in forest land in both North Korea and Mongolia caused a C loss at an average rate of 9.0 Tg C yr(-1), equal to 13.4% of the total region's C sink. Over the last four decades, the biomass C sequestration by East Asia's forests offset 5.8% of its contemporary fossil-fuel CO2 emissions.
森林在区域和全球碳(C)循环中发挥着重要作用。在过去几十年中,东亚地区进行了大规模的造林和再造林,森林面积大幅增加,但它们的碳储量动态尚未得到充分评估。我们使用生物量扩展因子法和森林清查数据,估算了 1970 年代至 2000 年代东亚五个国家(中国、日本、朝鲜、韩国和蒙古国)的森林生物量 C 储量。整个地区的森林面积和生物量 C 密度从 1970 年代的 179.78×10^6 公顷和 38.6 Mg C ha^-1 增加到 2000 年代的 196.65×10^6 公顷和 45.5 Mg C ha^-1。C 储量从 6.9 Pg C 增加到 8.9 Pg C,平均封存率为 66.9 Tg C yr^-1。在这五个国家中,中国和日本是该地区森林碳汇的两个主要贡献者,分别占总碳汇的 71.1%和 32.9%。在中国,所有森林(60.0%对 40.0%)和人工林(58.1%对 41.9%)的林地面积扩张是碳汇的较大贡献者,而生物量密度增加则贡献较小,而天然林则相反(87.0%对 13.0%)。在日本,所有(101.5%)、人工(91.1%)和天然(123.8%)森林的生物量密度增加都主导着碳汇。韩国的森林也是一个碳汇,由于森林生长增加,贡献了该地区总碳汇的 9.4%。与这些国家相比,朝鲜和蒙古的森林面积减少导致碳损失的平均速率为 9.0 Tg C yr^-1,相当于该地区总碳汇的 13.4%。在过去的四十年中,东亚森林的生物量 C 固存抵消了其当代化石燃料 CO2 排放的 5.8%。