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冬季环流与赤峰地区夏季旱涝
General Circulation in Winter and Drought and Flood over Chifeng Inner Mongolia in Summer
【摘要】 夏季旱涝与冬季环流关系密切。亚洲地区冬季纬向环流异常偏强 ,经向环流偏弱 ,同时 1月的极涡所在纬度 (简称极涡纬度 )偏南时 ,极易造成赤峰地区夏季洪涝 ;相反 ,纬向环流偏弱 ,经向环流偏强 ,同时 1月份的极涡纬度异常偏北时 ,极易造成赤峰地区夏季干旱。据此 ,把冬季环流进行分型 ,预测赤峰地区夏季旱涝
【Abstract】 Winter circulation and summer drought and flood is closely related.When the longitudinal circulation in winter is unusually strong the meridianal circulation is weaker.Meanwhile,when the north pole ovrtex tends to the south in January flood and drought would be caused easily in Chifeng area in summer.
- 【文献出处】 气象 ,Meteorological Monthly , 编辑部邮箱 ,2001年11期
- 【分类号】P434
- 【被引频次】9
- 【下载频次】51