李国庆, Robin Kung, Richard L. Pfeffer. 1993: 旋转流体物理实验中见到的大气环流特征. 气象学报, (4): 405-413. DOI: 10.11676/qxxb1993.051
引用本文: 李国庆, Robin Kung, Richard L. Pfeffer. 1993: 旋转流体物理实验中见到的大气环流特征. 气象学报, (4): 405-413. DOI: 10.11676/qxxb1993.051
Li Guoqing, Robin Kung, Richard L. Pfeffer. 1993: THE ATMOSPHERIC CIRCULATION FEATURES SEEN IN THE ROTATING FLUID PHYSICS EXPERIMENTS. Acta Meteorologica Sinica, (4): 405-413. DOI: 10.11676/qxxb1993.051
Citation: Li Guoqing, Robin Kung, Richard L. Pfeffer. 1993: THE ATMOSPHERIC CIRCULATION FEATURES SEEN IN THE ROTATING FLUID PHYSICS EXPERIMENTS. Acta Meteorologica Sinica, (4): 405-413. DOI: 10.11676/qxxb1993.051

旋转流体物理实验中见到的大气环流特征

THE ATMOSPHERIC CIRCULATION FEATURES SEEN IN THE ROTATING FLUID PHYSICS EXPERIMENTS

  • 摘要: 在合适的实验参数下(热力Rossby数ROT=0.1,Taylor数Ta=2.2×107),在旋转斜压流中,大尺度地形强迫造成低频振荡以及大气环流中的"阻塞"流型。这是由于地形强迫造成的准静止波与行进波的相互作用及共振引起的。地形把波数单一的流动变成多波数的流动。地形强迫使波数减少。

     

    Abstract: Under suitable imposed experimental parameters,near thermal Rossbv number ROT=0.1,and Taylor number Ta=2.2×107,the large-scale topography forcing produces low-frequency oscillation in the flow and rather long-lived flow pattern resembling blocking in the atmospheric circulation.The ‘blocking' phenomenon is caused by interaction and resonance of travelling waves and the quasi-stationary waves formed by topography forcing.The large-scale topography transforms wavenumber-homogeneous flows into mufti-wavenumber flows,and the topography-forced flows possess less wavenumber.

     

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