摘要
本文分析了１９９４年１２月１５～２２日河北兴隆折射率结构常数气球探测的主要结果。表明：兴隆冬季观测的湍流比昆明强，相干长度ｒＯ平均为６．４ｃｍ。不仅低层湍流较强，而且对流层顶附近有一较强湍流层。夜间垂直分布廓线可以用Ｈｕｆｎａｙｅｌ－Ｖａｌｌｅｙ模式来拟合。
Main observational results of the structure coefficient of the atmospheric refractive index C: are given. They were obtained by a balloon-borne instrument at Xinlong Station, Hebei province from December 15 to 22,1994. It shows that the turbulence at Xinlong Station is stronger than Kunming's. The average value of coherence length is 6.4 cm. Not only is there a strong turbulence within the boundary layer, but also in the tropopause region. The night-time data may be fitted by Hufnagel-Valley model.
出处
《量子电子学》
CSCD
1996年第4期385-390,共6页
基金
国家高技术863-308资助
