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首页> 外文期刊>Journal of atmospheric and solar-terrestrial physics >Planetary wave-type oscillations in the ionosphere and their relationship to mesospheric/lower thermospheric and geomagnetic disturbances at Wuhan (30.6 degrees N, 114.5 degrees E)
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Planetary wave-type oscillations in the ionosphere and their relationship to mesospheric/lower thermospheric and geomagnetic disturbances at Wuhan (30.6 degrees N, 114.5 degrees E)

机译:武汉地区(北纬30.6度,东经114.5度)电离层中的行星波型振荡及其与中层/低层热层和地磁干扰的关系

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摘要

Using wind, ionospheric and geomagnetic intensity data observed simultaneously at Wuhan (30.6 degrees N, 114.5 degrees E) in 2002 and 2003, planetary wave type oscillations (PWTO) in the ionosphere and their relationship with oscillations in the mesosphere/lower thermosphere (MLT) and geomagnetic intensity have been investigated. Two cases of 2- and 5-day oscillations in the ionosphere are analyzed to distinguish MLT drivers and geomagnetic drivers. The geomagnetic oscillations are the most important drivers for the PWTO with dominant periods of 5-, 10-, 13.5-day. But the planetary waves in MLT winds are the main drivers for the quasi-2-day oscillations in the ionosphere. The correlation coefficient of the occurrence rates of the 2-day oscillation in winds and in ionospheric f(0)F(2) is 0.82 for the data from February to November. The oscillations in the geomagnetic intensity can drive 30-50% of 5-, 10- and 13.5-day PWTO events in the ionosphere. If we evaluate all of the possible events driven by geomagnetic oscillations, more than 70% of the events have a relationship with geomagnetic oscillations with 5- and 10-day periods. The 39.7 h PWTO in ionospheric plasma frequencies observed from day 161 to 166 in 2002, are generated by an upward propagating wave with period 43.8 h. Two events of 6-day oscillations in the ionosphere observed during May to July in 2003, have different drivers. The first one is probably generated by 5.4-day upward propagating waves in MLT winds, but enhanced during a moderate geomagnetic storm. The second one is generated by the geomagnetic oscillations during a strong geomagnetic storm. (c) 2005 Elsevier Ltd. All rights reserved.
机译:利用2002年和2003年在武汉(北纬30.6度,东经114.5度)同时观测到的风,电离层和地磁强度数据,电离层中的行星波型振荡(PWTO)及其与中层/下热层(MLT)振荡的关系已经研究了地磁强度。分析了电离层中2天和5天振荡的两种情况,以区分MLT驱动器和地磁驱动器。地磁振荡是PWTO的最重要驱动因素,主导周期为5、10、13.5天。但是MLT风中的行星波是电离层准两天振荡的主要驱动力。对于2月至11月的数据,在风中和电离层中2天振荡的发生率的相关系数f(0)F(2)为0.82。地磁强度的振荡可以驱动电离层中5、10和13.5天PWTO事件的30-50%。如果我们评估由地磁振荡驱动的所有可能事件,则超过70%的事件与5天和10天周期的地磁振荡有关。从2002年的第161天到166天,电离层等离子体频率中的39.7 h PWTO是由向上传播的波(周期为43.8 h)产生的。 2003年5月至7月观察到的两个电离层6天振荡事件具有不同的驱动力。第一个可能是由MLT风中的5.4天向上传播波产生的,但在中等地磁风暴中会增强。第二个是由强地磁风暴期间的地磁振荡产生的。 (c)2005 Elsevier Ltd.保留所有权利。

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