On the Warm Front on the 24-25th Sept. 1935

[摘要] On the 24-25th Sept. 1935 the warm front was observed in the KwantÔ distric_??_and brough_??_ there the heavy rainfall. (See T. Ootani and K. Sone's paper). In this paper the present authors have investigated on the characteristic features of the line of discontinuity which was caused at the warm front. It was found that the line of discontinuity marched to NW-wards to the KwantÔ district from the SE-ern sea with a velocity about 3-4m/sec and went up generally the river Tone forming a wedge-like line.The inclination of the surface of discontinuity was found to be about 40'.

[学科分类] 大气科学