青藏高原地气相互作用过程及其天气气候效应数值模拟研究综述

A review of numerical simulation research on the interaction process between atmospheric and ground in the Qingzang plateau and its weather and climate effects

  • 摘要: 在全球气候变化和人类活动加剧的背景下,青藏高原作为“亚洲水塔”及“地球第三极”,其地气相互作用过程对区域和全球气候系统的调节作用愈加显著。数值模拟作为理解高原复杂气候过程的有效工具,在探索青藏高原地气系统的物理机制和天气气候效应方面发挥了不可替代的作用。系统综述了青藏高原地区4个主要地气相互作用过程的数值模拟研究进展,包括陆地-表层大气过程(边界层过程)、云降水物理过程、区域水分循环过程和平流层过程,重点探讨了这些过程在不同时间和空间尺度上的表现及其对区域天气系统、季风环流和全球气候的影响。最后,展望了未来的研究方向,提出需要通过提高数值模式的精度、优化参数化方案以及结合多源观测数据,以进一步揭示青藏高原在全球气候系统中的独特角色,并为应对气候变化的挑战提供科学依据。

     

    Abstract: In the context of global climate change and intensified human activities, the Qingzang plateau, known as the "Asian Water Tower" and the "Third Pole of the Earth", plays an increasingly significant role in regulating regional and global climate systems through its land-atmosphere interactions. Numerical simulations, as an effective tool for understanding the complex climatic processes on the plateau, have played an irreplaceable role in exploring the physical mechanisms behind the land-atmosphere systems on the Qingzang plateau and their weather and climate effects. This paper systematically reviews the research progresses of numerical simulations on four major land-atmosphere interaction processes on the Qingzang plateau, including land-surface-atmospheric processes (boundary layer processes), cloud precipitation physics processes, regional water cycle processes, and tropospheric processes, and focuses on discussing how these processes manifest at different temporal and spatial scales and their impacts on regional weather systems, monsoon circulations, and global climate. Finally, this paper outlines future research directions by proposing a need to enhance model accuracy, optimize parameterization schemes and integrate multiple observational data sources to further reveal the unique role of the Qingzang plateau in global climate system dynamics and provide scientific basis for addressing challenges posed by climate change.

     

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