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投稿时间:2008-03-17 修订日期:2008-07-19
投稿时间:2008-03-17 修订日期:2008-07-19
中文摘要: 根据1987年、2006年秦皇岛沿海出现的三次海市蜃楼景观资料,统计分析了海市蜃楼景象发
生时、发生前的天气形势、地面气压场、单站部分气象要素特征、GPS水汽探测资料等。结
果表明:海市蜃楼一般出现在高空槽后,强冷空气刚刚过后十分稳定的地面高压前部。沿海
地区,当近地面风很弱,气温急剧下降、湿度明显减少,700hPa温度露点差T-Td≥6
℃,饱和湿空气层处于不稳定状态向稳定干空气状态转化时,海市蜃楼景观出现的几率较大
。
Abstract:Three mirages which took place in 1987 and 2006 were selected and some meteor
ological elements during and before the mirage, such as weather situation, surfa
ce pressure field, water vapor remotely sensed by GPS and local meteorological f
actors were analyzed. The result shows that the mirage usually occurs in the rea
r of upper trough. In the meantime, it is in the front of surface high pressure
as dry and cold air just passed by. In the coastal region, if there would be the
se circumstances, such as a light wind, sharp decrease of temperature , low humi
dity, and the dew point deference is not lower than 6℃ at 700hPa, the layer of
humid saturated air is in the transient state from an unstable condition to a st
able situation of dry air,the wonderful view of mirage would have a high prob
ability to take place.
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基金项目:“GPS水汽探测网业务应用系统开发”河北省气象局科技基金资金项目
作者 | 单位 |
陈连友 | 河北省秦皇岛市气象局, 066000 河北省生态环境重点实验室 |
张宝贵 | 河北省秦皇岛市气象局, 066000 河北省生态环境重点实验室 |
陈小雷 | 河北省生态环境重点实验室 河北省气象台 |
景华 | 河北省生态环境重点实验室 河北省气象台 |
周建馨 | 河北省秦皇岛市气象局, 066000 河北省生态环境重点实验室 |
徐静 | 河北省秦皇岛市气象局, 066000 河北省生态环境重点实验室 |
引用文本:
陈连友,张宝贵,陈小雷,景华,周建馨,徐静,2008.出现海市蜃楼的天气特征分析[J].气象,34(11):84-88.
Chen Lianyou,Zhang Baogui,Chen Xiaolei,Jing Hua,Zhou Jianxin,Xu Jing,2008.Analysis of Weather Characteristics for the Mirage[J].Meteor Mon,34(11):84-88.
陈连友,张宝贵,陈小雷,景华,周建馨,徐静,2008.出现海市蜃楼的天气特征分析[J].气象,34(11):84-88.
Chen Lianyou,Zhang Baogui,Chen Xiaolei,Jing Hua,Zhou Jianxin,Xu Jing,2008.Analysis of Weather Characteristics for the Mirage[J].Meteor Mon,34(11):84-88.