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生态学杂志 ›› 2026, Vol. 45 ›› Issue (2): 681-694.doi: 10.13292/j.1000-4890.202602.049

• 技术与方法 • 上一篇    下一篇

基于多模型耦合的京津冀城市群生态碳汇保护区划多情景模拟

赵欣瑶,肖睿珂,刘廷炜,王凯平,曹蕾,奚承彬,张云路*


  

  1. (北京林业大学园林学院, 北京 100083)

  • 出版日期:2026-02-10 发布日期:2026-08-01

Multi-scenario simulation of ecological carbon sink conservation zoning in Beijing-Tianjin-Hebei urban agglomeration based on multi-model coupling.

ZHAO Xinyao, XIAO Ruike, LIU Tingwei, WANG Kaiping, CAO Lei, XI Chengbin, ZHANG Yunlu*   

  1. (School of Landscape Architecture, Beijing Forestry University, Beijing 100083, China).

  • Online:2026-02-10 Published:2026-08-01

摘要: 气候变化已成为制约社会经济可持续发展的重要因素,而在城市群应对未来气候变化的生态碳汇保护区划领域仍存在研究空白。本研究提出了一个耦合斑块级土地利用变化模拟(PLUS)模型、生态过程(CASA)模型和Zonation模型的综合框架。以京津冀城市群为研究对象,基于CMIP6提供的3种气候变化情景——SSP126(低排放可持续发展路径)、SSP245(中等排放路径)和SSP585(高排放高碳发展路径)动态模拟城市群尺度的土地利用变化和生态空间碳汇效能演变特征,进而确定生态碳汇核心保护区的空间范围。结果表明:(1)至2030年,生态优先的SSP126情景并非最优路径,高碳排放的SSP585情景下尽管生态空间面积有所缩减,但部分单元碳汇平均值较高,成为近期较优发展路径;(2)近期与远期最优发展情景存在差异,2060年最优路径为SSP245,而SSP585情景下生态碳汇总量降至最低,主要由于持续高温和生态空间破碎化加剧导致植被生产力显著下降;(3)SSP126、SSP245和SSP585情景下确定的核心保护区面积分别为85014、84832和84834 km2,保护区的空间异质性主要源于气候变化与人类活动的交互作用,如气候变暖促进燕山东北部植被生长,而高强度开发导致南部山区和西北农牧交错带生态退化。总体而言,该框架为平衡生态碳汇保护与社会经济发展提出了更精准的保护区划路径和更科学的动态调控措施,为京津冀地区及其他类似城市群在气候变化背景下的可持续发展提供了有益参考。

关键词: 气候变化, 多情景模拟, 多模型耦合, 土地利用变化, 净初级生产力, 保护区

Abstract: Although climate change has become a significant constraint on sustainable socioeconomic development, there remains a research gap in the planning of ecological carbon sink reserve for urban agglomerations in response to climate change. We proposed an integrated framework coupling the Patch-level Land Use Simulation (PLUS) model, the Carnegie-Ames-Stanford Approach (CASA) model, and the Zonation model. Using the Beijing-Tianjin-Hebei urban agglomeration as a case study, based on three climate change scenarios-SSP126 (low-emission sustainable development pathway), SSP245 (medium-emission pathway), and SSP585 (high-emission and high-carbon development pathway)-provided by CMIP6, we applied this framework to simulate the variations of land use change and ecological carbon sink capacity at the urban agglomeration scale, and identified the spatial extent of core ecological carbon sink reserve. The results showed that: (1) By 2030, the ecologically prioritized SSP126 scenario is not the optimal path. Although the ecological space area is reduced under the highcarbon emission SSP585 scenario, the higher average carbon sink values in certain units make it a comparatively better development pathway in the near term. (2) The optimal development pathways differ between the short-term and long-term. By 2060, the optimal pathway is SSP245, while the total ecological carbon sink under SSP585 decreases to the lowest level, due to sustained high temperatures and intensified fragmentation of ecological space leading to a significant decline in vegetation productivity. (3) The core conservation areas will delineate under the SSP126, SSP245, and SSP585 scenarios cover areas of 85014, 84832, and 84834 km2, respectively. The spatial heterogeneity of these conservation areas mainly stems from the interaction between climate change and human activities. For example, warming promotes vegetation growth in the northeastern Yanshan region, whereas high-intensity development leads to ecological degradation in the southern mountainous areas and the northwestern farming-pastoral ecotone. In summary, this framework provides more precise conservation zoning pathways and scientifically grounded dynamic regulatory measures for balancing ecological carbon sink reserve with socio-economic development. It offers a valuable reference for the sustainable development of the Beijing-Tianjin-Hebei region and other similar urban agglomerations in the context of climate change.


Key words: climate change, multi-scenario simulation, multi-model coupling, land use/cover change, net primary production, conservation zone