干旱气象 ›› 2025, Vol. 43 ›› Issue (2): 207-220.

• 论文 • 上一篇    下一篇

气候过渡区不同生态系统多陆面因子-大气耦合特征

何 杭,杨泽粟,邬钰嫣
  

  1. 成都信息工程大学大气科学学院,高原大气与环境四川省重点实验室,四川 成都 610225
  • 出版日期:2025-04-30 发布日期:2025-05-13
  • 作者简介:何杭(1999—),男,硕士研究生,主要从事陆-气相互作用研究。E-mail:hehangabc@163. com。

Characterization of multi-land surface factor-atmosphere coupling in different ecosystems in the climate transition zones

HE Hang, YANG Zesu, WU Yuyan
  

  1. College of Atmospheric Sciences,Chengdu University of Information Technology,Plateau Atmospheric and
    Environment Key Laboratory of Sichuan Province,Chengdu 610225,China
  • Online:2025-04-30 Published:2025-05-13

摘要:

气候过渡区作为“陆-气耦合”热点地区,当前研究多集中于该区域陆-气耦合时空分布及水热条件的影响,缺乏对多因子协同作用及不同生态系统耦合度差异的研究。本文基于站点观测资料,聚焦陆面水、热、生因子与地表通量的耦合关系,对比分析不同生态系统之间单因子和多因子陆-气耦合度差异,评估各陆面因子对耦合度的贡献。结果表明,单因子耦合中,稀疏植被的潜热与叶面积指
数耦合强度最强,农田的潜热与土壤温度耦合强度最强;草地、森林和农田的感热与土壤温度耦合最强。多因子耦合度明显优于单因子,多因子与潜热的耦合度在森林和稀疏植被有明显提升,与感热的耦合在稀疏植被明显增强。各因子对地表通量的贡献中,草地感热和潜热分别由热力和生态因子主导;稀疏植被潜热由水分、生态因子共同主导,感热由热力因子主导;农田和森林的潜热和感热由热力因子主导。干旱条件下,水分和生态因子对多数生态系统中潜热和感热的贡献增大。

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Abstract:

As a hot spot of “land-atmosphere coupling”, the current study focuses on the spatial and temporal distribution of land atmosphere coupling and the influence of hydrothermal conditions in the climate transition regions, but lacks the study on the synergistic effect of multi-factor and the difference in coupling degree among different ecosystems. Based on the station observation data, the paper focused on the coupling relationship between land surface water, thermal and ecological factors and surface fluxes, comparatively analyzed the differences in single-factor and multi-factor synergistic land-atmosphere coupling among different ecosystems, and assessed the contribution of each land surface factor to the coupling degree. The results show that in single-factor coupling, the coupling between latent heat flux and leaf area index is the strongest for sparse vegetation, and the coupling between latent heat flux and soil temperature is the strongest for farmland; the coupling between sensible heat flux and soil temperature is the strongest for grassland, forest and farmland. Multi-factor synergistic coupling is significantly better than that of single factor, and multi-factor synergistic coupling with latent heat flux is significantly enhanced in forest and sparse vegetation, and synergistic coupling with sensible heat flux is obviously enhanced in sparse vegetation. Among the contributions of each factor to the surface fluxes, in grassland system sensible and latent heat fluxes are dominated by thermal and ecological factors, respectively; in sparse vegetation system latent heat flux is codominated by the soil moisture factor and leaf area index, and sensible heat flux is dominated by the thermal factor; and latent heat and sensible heat fluxes are dominated by the thermal factor in farmland and forest system. Under drought conditions, the contributions of soil moisture and ecological factors to latent and sensible heat fluxes increase in most ecosystems.

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