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Ionospheric response to the 2009 sudden stratospheric warming over the equatorial, low, and middle latitudes in the South American sector

机译:电离层对2009年南美赤道,低纬度和中纬度地区平流层突然变暖的反应

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摘要

The present study investigates the ionospheric total electron content (TEC) and F-layer response in the Southern Hemisphere equatorial, low, and middle latitudes due to major sudden stratospheric warming (SSW) event, which took place during January–February 2009 in the Northern Hemisphere. In this study, using 17 ground-based dual frequency GPS stations and two ionosonde stations spanning latitudes from 2.8°N to 53.8°S, longitudes from 36.7°W to 67.8°W over the South American sector, it is observed that the ionosphere was significantly disturbed by the SSW event from the equator to the midlatitudes. During day of year 26 and 27 at 14:00 UT, the TEC was two times larger than that observed during average quiet days. The vertical TEC at all 17 GPS and two ionosonde stations shows significant deviations lasting for several days after the SSWtemperature peak. Using one GPS station located at Rio Grande (53.8°S, 67.8°W, midlatitude South America sector), it is reported for the first time that the midlatitude in the Southern Hemisphere was disturbed by the SSW event in the Northern Hemisphere.
机译:本研究调查了由于2009年1月至2月在北半球发生的重大平流层突然变暖(SSW)事件导致的南半球赤道,低纬和中纬度电离层总电子含量(TEC)和F层响应半球。在这项研究中,使用了17个地面双频GPS站和两个电离探空仪站,它们跨过南美地区,纬度从2.8°N到53.8°S,经度从36.7°W到67.8°W,观察到电离层是从赤道到中纬度的SSW事件极大地干扰了该事件。在世界标准时间26和27的14:00时,TEC值是平均安静日观测到的值的两倍。在SSW温度峰值之后,所有17个GPS站和两个离子探空仪站的垂直TEC都显示出明显的偏差,并持续了几天。据报道,这是第一次使用位于里奥格兰德州(53.8°S,67.8°W,南纬中纬度地区)的GPS站,南半球的中纬度受到北半球SSW事件的干扰。

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