摘要
对2005年12月发生在山东半岛北部威海地区的三次冷流暴雪过程进行了分析研究,用WRF模式进行了数值模拟。分析结果表明:三次冷流暴雪发生时低空850hPa层强冷平流与地面降水强度有较好的对应关系;低层和地面都是偏西北风流场,半岛地区呈气旋性弯曲;地面风场存在风向辐合,特殊的地形和海陆温差在北部沿海地区形成海岸锋,为冷流的发生提供了有利的触发机制;从垂直面的风场辐合辐散高度说明了冷流过程较其他降水过程有着明显的低空性。
Three cold airstream snowstorm processes happened in Dec. in 2005 have been analysed and simulated by WRF model. The results declare that : the cold airstream of 850hPa layer has good relationship with ground precipitation intensity in three cases; there are mainly NW wind fields on ground and at low level, which makes cyclonic curve on peninsula; wind convergence on ground and seashore front caused by special land and sea-land temperature difference provide burst mechanism for cold airstream course ; the height of wind divergence on vertical plane emphasizes the low level characteristic of cold airstream precipatition.
出处
《气象科学》
CSCD
北大核心
2008年第4期395-401,共7页
Journal of the Meteorological Sciences
基金
山东省"山东半岛冷流天气形成机理的模式研究"重点课题
关键词
山东半岛
冷流
海温
海岸锋
Shandong peninsula Cold airstream SST Seashore front