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深厚大气边界层演变与湍流运动、沙尘滞空的研究 被引量:3

Research on the Development of the Deep Atmospheric Boundary Layer, Turbulent Motion, and Dust Stagnation
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摘要 大气边界层是地球表面与大气之间水热、动量、能量和痕量气体等物质交换和输送的重要通道,在天气和气候的演变过程中有着重要作用。深厚大气边界层现象和特征、形成机理以及天气气候效应是大气边界层研究领域的热点问题,也是科学难题。着眼于对天气和气候高敏感、高影响的极端气候区和特殊地理区域,回顾梳理了深厚大气边界层的观测事实,归纳总结了不同地区深厚大气边界层的成因和影响因素,描述深厚大气边界层演变过程中独特的湍流运动图像,解析探讨了深厚大气边界层演变与沙尘滞空之间的关联。最后,提出了深厚大气边界层的未来研究关注重点和实现突破的4个关键科学问题,以期为更加系统地开展深厚大气边界层研究提供参考依据。 The atmospheric boundary layer connects the land surface to the atmosphere through the turbulent exchange of heat,momentum,and trace gases.In addition,it plays an important role in the formation and evolution of weather and climate.The characteristics and formation mechanisms of the deep atmospheric boundary layer have been key focus areas in atmospheric boundary layer research.Focusing on extremely arid regions and special geographical locations,the observational facts and influencing factors of the deep atmospheric boundary layer were reviewed and summarized.Furthermore,a physical description of turbulent motion in the development of the deep atmospheric boundary layer was provided.Using the Taklimakan Desert as an example,the effects of the interactions between the deep atmospheric boundary layer and dust stagnation on weather and climate were discussed.In order to provide a roadmap for future research,this study identified and outlined four key scientific problems related to deep atmospheric boundary layer research.
作者 张璐 李倩惠 孟露 张强 张宏昇 何清 赵天良 ZHANG Lu;LI Qianhui;MENG Lu;ZHANG Qiang;ZHANG Hongsheng;HE Qing;ZHAO Tianliang(Laboratory for Climate and Ocean-Atmosphere Studies,Department of Atmospheric and Oceanic Sciences,School of Physics,Peking University,Beijing 100871,China;Tianjin Key Laboratory for Oceanic Meteorology,Tianjin Meteorological Service Center,Tianjin 300074,China;Institute of Desert Meteorology,China Meteorological Administration,Urumqi/Taklimakan Desert Meteorology Field Experiment Station of China Meteorological Administration/National Observation and Research Station of Desert Meteorology,Taklimakan Desert of Xinjiang/Xinjiang Key Laboratory of Desert Meteorology and Sandstorm,Urumqi 830002,China;Institute of Arid Meteorology,China Meteorological Administration/Key Laboratory of Arid Climatic Change and Reducing Disaster of Gansu Province/Key Open Laboratory of Arid Climatic Change and Disaster Reduction of China Meteorological Administration,Lanzhou 730020,China;Gansu Meteorological Bureau,Lanzhou 730020,China;School of Atmospheric Physics,Nanjing University of Information Science&Technology,Nanjing 210044,China)
出处 《地球科学进展》 CAS CSCD 北大核心 2022年第10期991-1004,共14页 Advances in Earth Science
基金 国家自然科学基金项目“化学天气数值预报系统中大气成分与大气宏微观动力、热力和云过程的双向反馈机制与影响研究”(编号:42090031)和“青藏高原夏季热源‘北扩’与塔里木盆地‘滞空’沙尘气溶胶辐射加热的关联及对区域降水变异的影响”(编号:4203000543)资助
关键词 深厚大气边界层 陆—气相互作用 湍流运动图像 干旱地区 青藏高原 Deep atmospheric boundary layer Land-atmosphere interaction Turbulent characteristics Arid regions Tibetan Plateau
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