Hu Cheng, Liu Huili, Zhang Yifan, Cui Yu, Sun Fan, Shi Xuejing, Zhang Junqing, Yang Yanrong, Zhang Leying, Qi Bing, Xiao Qitao, Hu Ning, Griffis Timothy J, Xiao Wei
College of Ecology and Environment, Joint Center for sustainable Forestry in Southern China, Nanjing Forestry University, Nanjing 210037, China; Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Key Laboratory of Ecosystem Carbon Source and Sink, China Meteorological Administration (ECSS-CMA), Nanjing University of Information Science & Technology, Nanjing 210044, China.
College of Ecology and Environment, Joint Center for sustainable Forestry in Southern China, Nanjing Forestry University, Nanjing 210037, China.
Sci Total Environ. 2025 Apr 25;974:178884. doi: 10.1016/j.scitotenv.2025.178884. Epub 2025 Mar 24.
After the initial prevention of COVID-19 in early 2020, China gradually lifted its control measures in the latter half of 2020, leading to a rebound in anthropogenic CO emissions. However, the emergence of a COVID-19 variant in late 2021, particularly in densely populated and economically developed areas, prompted the reimplementation of stringent confinement measures. Furthermore, with the policy shift towards achieving "herd immunity", China fully lifted pandemic control measures in December 2022, resulting in the unrestricted movement of residents and facilitating the widespread transmission of COVID-19 in the ensuing months. But to our knowledge, no studies have yet quantified the relative changes in CO emissions during these successive phases, representing a significant knowledge gap in understanding the impact of varying control measures on anthropogenic CO emissions at both city and regional scales. Consequently, we selected Hangzhou city and the Yangtze River Delta (YRD) region as our study area due to their status as economically developed and densely populated regions in China. In order to mitigate the influence of biological CO flux, we utilized wintertime atmospheric CO observations at two urban and rural sites, along with their gradient, across three years (December 2020-February 2023). We employed two distinct methods with the WRF-STILT model to quantify the relative changes in CO emissions. Our findings indicate that (1) atmospheric CO concentrations at both sites and their gradients in 2022 were significantly lower than those observed in 2020, with modeled simulations using consistent emissions suggesting that changes in emissions were the predominant factor rather than variations in atmospheric transport processes; (2) After applying the source region partition method, anthropogenic CO emissions during the winter of 2021 decreased to 69.8 % ± 1.6 % in Hangzhou city when compared with 2020, while emissions in the YRD region dropped to 92.5 % ± 6.2 %. In winter 2022, emissions in Hangzhou city decreased to 79.9 % ± 1.9 %, and YRD region decreased to 82.0 % ± 7.2 % relative to 2020, highlighting substantial spatial heterogeneity from the city to the regional scale; (3) notably, the observed decreases in CO emissions in both Hangzhou and the YRD were not reflected in prior inventories, which indicated an annual increase of 8 % for 2021 and 2022, suggesting that even the most recent inventories fail to account for the prolonged emission reduction effects occurring over the preceding three years.
在2020年初对新冠疫情进行初步防控之后,中国于2020年下半年逐步放松管控措施,导致人为碳排放出现反弹。然而,2021年末新冠病毒变异株出现,尤其在人口密集和经济发达地区,促使重新实施严格的封控措施。此外,随着政策转向实现“群体免疫”,中国于2022年12月全面解除疫情防控措施,居民得以自由流动,在随后几个月里促进了新冠病毒的广泛传播。但据我们所知,尚无研究对这些连续阶段碳排放的相对变化进行量化,这在理解不同管控措施对城市和区域尺度上人为碳排放的影响方面存在重大知识空白。因此,我们选择杭州市和长江三角洲(长三角)地区作为研究区域,因其在中国属于经济发达且人口密集的地区。为减轻生物碳通量的影响,我们利用了2020年12月至2023年2月三年间两个城乡站点的冬季大气一氧化碳观测数据及其梯度。我们使用WRF-STILT模型采用两种不同方法来量化碳排放的相对变化。我们的研究结果表明:(1)2022年两个站点的大气一氧化碳浓度及其梯度均显著低于2020年观测值,使用一致排放的模型模拟表明排放变化是主要因素,而非大气传输过程的变化;(2)应用源区划分方法后,与2020年相比,杭州市2021年冬季人为一氧化碳排放量降至69.8%±1.6%,而长三角地区排放量降至92.5%±6.2%。2022年冬季,杭州市排放量降至79.9%±1.9%,长三角地区降至82.0%±7.2%(相对于2020年),凸显了从城市到区域尺度上的显著空间异质性;(3)值得注意的是,杭州市和长三角地区观测到的一氧化碳排放量下降并未在先前的排放清单中体现,先前清单显示2021年和2022年排放量每年增长8%,这表明即使是最新的排放清单也未能考虑到此前三年长期存在的减排效应。