Xiao Qingnong. 1994: DISTORTION AND OCCLUSION OF COLD FRONTS UNDER THE INFLUENCES OF OROGRAPHY. Acta Meteorologica Sinica, (4): 414-423. DOI: 10.11676/qxxb1994.051
Citation: Xiao Qingnong. 1994: DISTORTION AND OCCLUSION OF COLD FRONTS UNDER THE INFLUENCES OF OROGRAPHY. Acta Meteorologica Sinica, (4): 414-423. DOI: 10.11676/qxxb1994.051

DISTORTION AND OCCLUSION OF COLD FRONTS UNDER THE INFLUENCES OF OROGRAPHY

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  • Received Date: July 13, 1992
  • Revised Date: October 03, 1992
  • Published Date: February 19, 2013
  • Following classical theory, a two-layer frontal model is designed. It assumes that frontal surface is the zero-order discontinuty of density. In this paper, the model is used to study orographically distorted and occluded fronts. It is indicated that the distortion and occlusion of cold fronts are different under different conditions of orography. Frontal intensity has also influences on the distortion and occlusion. Some rules are revealed and compared with observations. In addition, we have analysed the vertical structure of cold front above mountain and found that frontal surface may be bulged under the influence of orography when it climes the mountain. The bulge of frontal surface is just like the bore which is pointed out by Lone(1972) when he analvsed fluid over obstacles.
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