气候变化研究进展

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气候模式分辨率提升对东边界上升流系统模拟的影响

李卓然1,杜天时2,王胜鹏2,徐源3,荆钊2,4   

  1. 1 中国气象局气象发展与规划院,北京 100081;
    2 崂山实验室,青岛 266100;
    3 中国气象局国家气候中心,北京 100081;
    4 中国海洋大学深海圈层与地球系统前沿科学中心,青岛 266100
  • 收稿日期:2026-03-23 修回日期:2026-05-29 出版日期:2026-08-26 发布日期:2026-08-26
  • 通讯作者: 王胜鹏
  • 基金资助:
    国家自然科学基金项目;国家博士后创新人才支持计划资助;中国气象局气候预测研究重点开放实验室开放课题;中国气象局气候资源经济转化重点开放实验室开放研究课题题

Impacts of increased climate model resolution on eastern boundary upwelling systems simulations

LI Zhuo-Ran1, DU Tian-Shi2, WANG Sheng-Peng2, XU Yuan3, JING Zhao2, 4   

  1. 1 CMA Institute for Development and Programme Design, Beijing 100081, China;
    2 Laoshan Laboratory, Qingdao 266100, China;
    3 National Climate Centre, China Meteorological Administration, Beijing 100081, China; 4 Frontiers Science Center for Deep Ocean Multispheres and Earth System, Ocean University of China, Qingdao 266100, China
  • Received:2026-03-23 Revised:2026-05-29 Online:2026-08-26 Published:2026-08-26
  • Contact: Shengpeng Wang

摘要: 东边界上升流区域作为全球海洋中生产力最高的区域之一,在维持海洋生态系统稳定和支撑渔业资源方面发挥着至关重要的作用。然而,传统低分辨率气候模式在该区域的模拟中存在显著偏差,限制了对上升流过程及其未来变化的可靠评估。本研究利用CMIP6高分辨率模式比较计划中的多组高、低分辨率气候模式数据,系统评估了空间分辨率提升对全球四大东边界上升流系统模拟性能的改善作用,并深入解析了动力与热力指标在历史模拟和未来预估中的表征差异。结果表明,低分辨率模式普遍低估东边界上升流强度,而提高空间分辨率,尤其是海洋模式分辨率,可显著降低模拟偏差。分辨率提升可有效改进由埃克曼输运主导的上升流过程模拟,但对于地转输运贡献的再现能力仍显不足,与此同时,高分辨率模式在上升流热力指标模拟上亦表现出明显优势。未来情景预估显示,不同东边界上升流系统对全球变暖的响应存在显著区域差异,且分辨率提升并未明显降低各模式之间的预估离散度。总体而言,提高模式分辨率能够有效改善东边界上升流系统平均态模拟能力,但其未来变化趋势的预估仍存在较大不确定性,内在动力机制有待进一步探究。

关键词: 东边界上升流, 气候模式分辨率, CMIP6, 埃克曼输运, 地转输运

Abstract: As one of the most productive regions in the global ocean, eastern boundary upwelling systems (EBUSs) play a crucial role in maintaining marine ecosystems and supporting global fisheries. However, traditional low-resolution climate models exhibit substantial biases in these regions, limiting reliable assessments of upwelling processes and their future changes. Using simulations from the CMIP6 High-Resolution Model Inter-comparison Project (HighResMIP), this study evaluates the extent to which increased spatial resolution improves the simulation of the four major EBUSs worldwide and examines the differences between dynamical and thermal indicators for characterizing upwelling in both historical simulations and future projections. The results show that low-resolution models generally underestimate the strength of coastal upwelling, whereas increasing spatial resolution?particularly the ocean model resolution?significantly reduces these biases. Higher resolution effectively improves the simulation of Ekman-driven upwelling processes, although the representation of geostrophic transport remains challenging. Meanwhile, high-resolution models also demonstrate clear improvements in reproducing thermally based upwelling indicators. Future projections indicate pronounced regional differences in the response of EBUSs to global warming, while increased model resolution does not substantially reduce the spread among model projections. Overall, increasing model resolution significantly improves the representation of the mean state of EBUSs, but considerable uncertainties remain in their future projections, and the underlying dynamical mechanisms require further investigation.

Key words: Eastern boundary upwelling systems (EBUSs), Climate model resolution, Coupled Model Intercomparison Project Phase 6 (CMIP6), Ekman transport, Geostrophic transport

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