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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Observation of TEC perturbation associated with mediumscale traveling ionospheric disturbance and possible seeding mechanism of atmospheric gravity wave at a Brazilian sector
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Observation of TEC perturbation associated with mediumscale traveling ionospheric disturbance and possible seeding mechanism of atmospheric gravity wave at a Brazilian sector

机译:TEC扰动与观察mediumscale电离层扰动和旅行可能的催化机制的大气重力波在一个巴西的部门

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摘要

In the present study, we document daytime total electron content (TEC) disturbances associated with medium-scale traveling ionospheric disturbances (MSTIDs), on few chosen geomagnetically quiet days over Southern Hemisphere of Brazilian longitude sector. These disturbances are derived from TEC data obtained using Global Navigation Satellite System (GNSS) receiver networks. From the keograms and cross-correlation maps, the TEC disturbances are identified as the MSTIDs that are propagating equatorward-eastward, having most of their average wavelengths longer in latitude than in longitude direction. These are the important outcomes of the present study which suggest that the daytime MSTIDs over Southern Hemisphere are similar to their counterparts in the Northern Hemisphere. Another important outcome is that the occurrence characteristics of these MSTIDs and that of atmospheric gravity wave (AGW) activities in the thermosphere are found to be similar on day-to-day basis. This suggests a possible connection between them, confirming the widely accepted AGW forcing mechanism for the generation of these daytime MSTIDs. The source of this AGW is investigated using the Geostationary Operational Environmental Satellite system (GOES) and Constellation Observing System forMeteorology, Ionosphere, and Climate satellite data. Finally, we provided evidences that AGWs are generated by convection activities from the tropospheric region.
机译:在目前的研究中,我们白天总文档电子(TEC)干扰相关的内容与中等规模的电离层旅行干扰(MSTIDs),在一些选择眼睛安静的天在南部南半球的巴西经度部门。干扰来自TEC数据获得使用全球导航卫星系统(GNSS)接收器网络。互相关地图、TEC干扰的MSTIDs传播equatorward-eastward,他们的大部分纬度的平均波长更长的时间比经度方向。本研究的结果表明白天MSTIDs在南半球类似于北方的同行半球。发生这些MSTIDs和特征大气重力波(索引)活动热大气层中发现类似的日常的基础。它们之间的联系,确认接受索引迫使生成的机制这些白天MSTIDs。使用同步调查运行环境卫星系统(是)和星座观测系统forMeteorology、电离层和气候卫星数据。是由对流活动的对流层的地区。

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