摘要
本省今年自入秋以来,气候亢旱,雨泽稀少;粮价曾一度高涨,人心惶惑,望雩者致为殷切。顾今岁秋季雨量,虽非绝对过低,较谐前光绪二十八年及民国二十一年等大旱时代,已迥不相同,然若考之於近数年,与夫在四季雨量上之分配,则减逊良多,此实属昭彰难讳之事实。作者为明瞭其原因,不揣譾陋,试为探讨,讹误难免,尚幸方家指正之!
The Autumn drought of Sian,Shensi in 1936 was caused by the interplay of the following meteorological factors:1.The Siberian High covered North China,remained stationary and stable.2.The cyclones of the Yangtze type A were weak ond shallow.Most of them traveiled in a northeast direction and did not pass Sian as they should do.3,The cyclones of the Yangtze type B were very few in fhis year.
出处
《气象学报》
1937年第1期39-42,共4页
Acta Meteorologica Sinica
