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辽宁风暴潮灾害分析
引用本文:王斌飞,翟晴飞,敖,雪等.辽宁风暴潮灾害分析[J].安徽农业科学,2014(6):1765-1768,1835.
作者姓名:王斌飞  翟晴飞    雪等
作者单位:[1]辽宁省盘锦市气象局,辽宁盘锦124010 [2]辽宁省人工影响天气办公室,辽宁沈阳110166 [3]沈阳区域气候中心,辽宁沈阳110166
摘    要:根据1884~2012年辽宁省沿海地区气象站观测资料,结合辽宁沿海地区的地理环境,对该地区的风暴潮特征及灾害进行分析。结果表明,风暴潮在辽宁各地出现次数及灾害损失程度由于地理位置不同而存在差异,辽东湾风暴潮强度小于黄海北部海岸,浅水区的风暴潮强度明显大于深水区风暴潮;风暴潮减水机率多于增水,但增减水量值差异不大,偏南大风引起增水,偏北大风引起减水。

关 键 词:风暴潮特征  时空分布  增水特征  致灾因素  防御  辽宁

Analysis of Storm Surge Disasters in Liaoning
Institution:WANG Bin-fei,ZHAI Qing-fei( 1.Panjin Meteorological Service, Panjin, Liaoning 124010; 2.Liaoning Weather Modification Office,Shenyang, Liaoning 110166;)
Abstract:According to coastal weather station data in Liaoning Province during 1884-2012,combined with the geographical environment in Liaoning coastal area,the characteristics of storm surge and disaster in this area were analyzed.It was found that there are differences in the frequency and extent of storm surge disaster losses in Liaoning due to the different geographical position,Liaodong Bay storm surge intensity is less than the northern Yellow Sea coast.The storm surge strength in shallow water was significantly greater than it in the deep water.The water decelerate probability more than the increases probability of storm surge,but changes in the value of water is insignificant,southerly winds cause increase,northerly winds cause reduction.
Keywords:Storm surge characteristics  Spatial and temporal distribution  Water increasing features  Formative factors  Defense  Liaoning
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