The Crossing of Cold Front and the Night f0F2
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摘要: 本文利用1968—1975年“寒潮年鉴”和乌鲁木齐、长春两站电离层f0F2资料,讨论了寒潮过境对夜电离层的影响.对个别样本的统计分析,特别是以地面气温最低日为标准日的叠加周期分析,均说明寒潮过境时夜间f0F2有下降趋势,平均说,在标准日下降最大,而后恢复.下降的百分值在太阳活动低年比高年大,乌鲁木齐站则比长春站大.这一下降的可能原因,是寒潮中激流带底部风切不稳定性产生的重力波向上传至电离层高度,对电子浓度分布影响的积累效应.此初步设想能定性说明统计分析中的一些基本特性.Abstract: The effects of the cold fronts upon the night f0F2 are found out by using the records from the cold fronts years book and ionosonds measurements of Wulumuqi and Changchun. From the statistical analyses of large number samples from 1968 to 1975 and the superposed epoch analyses with the day of the minimum temperature during the processes as the key day, it is shown that the f0F2 tends to decrease when a could front passes across. The maximum decrease is at the key day in the superposed epoch analyses. The pereentage values of the decreases are 4%-8%. It is larger in solar low-activity years, and the variation is also larger in Wulumuqi than in Changchun, x2-and U-test have been used to demonstrate the significance of the respose. The effects are probably caused by the gravity waves from the Jet-stream?generated Kelvin-Helm-holtz Instability within the cold front area. Gravity waves may propagate upward and produce the up-down oscillation in ionosphere. The integrated decrease of the f0F2 and the difference between the high and low activity years can be interpreted by his mechanism as well as the station-to-station difference.
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