王冰, 林修栋, 王娜, 郭敏, 冷冰. 一次持续性降雪过程中系统性降雪与冷流降雪的分析[J]. 云南大学学报(自然科学版), 2011, 33(S2): 379-382.
引用本文: 王冰, 林修栋, 王娜, 郭敏, 冷冰. 一次持续性降雪过程中系统性降雪与冷流降雪的分析[J]. 云南大学学报(自然科学版), 2011, 33(S2): 379-382.
An analysis of systematic snowfall and cold flow snowfall in theprocess of continuous snow[J]. Journal of Yunnan University: Natural Sciences Edition, 2011, 33(S2): 379-382.
Citation: An analysis of systematic snowfall and cold flow snowfall in theprocess of continuous snow[J]. Journal of Yunnan University: Natural Sciences Edition, 2011, 33(S2): 379-382.

一次持续性降雪过程中系统性降雪与冷流降雪的分析

An analysis of systematic snowfall and cold flow snowfall in theprocess of continuous snow

  • 摘要: 通过分析2010年1月初烟台地区的1次持续性降雪天气过程,将前期的系统性降雪和后期的冷流降雪分别进行总结,同时运用风廓线资料对过程进行分析,结果认为黄河气旋东移和较强冷平流南下是造成降雪的主要影响因子,风速的强弱对整个降雪过程有着直接的影响.通过分别对其影响机制以及作用因子进行总结,进一步地了解烟台地区的降雪成因,以期更好地服务于社会,减少各类损失.

     

    Abstract: It is analyzed the process of continuous snow,which is combined with pre-systematic snow and cold flow snowfall later,occurred in Yantai,early January,2010,and the data of wind profiler for process analysis,as well.It is concluded that the eastward shift of the Yellow River cyclone and strong cold advection is the main impact factors on causing snowfall.The extend of wind speed does a direct impact on snow.The mechanism and the factors of snow occurred on Yantai,is summaried to further understand the causes of snow in the area,to better serve the community and reduce the loss.

     

/

返回文章
返回