首页> 美国政府科技报告 >Measurement of the Characteristics of TIDs Using Small and Regional Networks of GPS Receivers during the Campaign of 17-30 July of 2008.
【24h】

Measurement of the Characteristics of TIDs Using Small and Regional Networks of GPS Receivers during the Campaign of 17-30 July of 2008.

机译:2008年7月17日至30日运动期间利用Gps接收机小区域网络测量TID特征。

获取原文

摘要

This scientific report presents the results of a dedicated experiment that was conducted within the framework of the Low-latitude ionospheric Sensor Network (LISN) observatory to measure the characteristics of medium-scale (hundreds of km) Traveling Ionospheric Disturbances (TIDs) as they transit through the low-latitude ionosphere. A small array of 3 GPS receivers separated by 4-5 km placed in a triangular configuration was installed near Huancayo in Peru possessing several characteristics of a radiointerferometer. During the campaign days, 17 30 July 2008, TIDs were observed daily. On July 20, 2008 between 22 and 24UT several TIDs moved across the small array of GPS receivers with a velocity near 130 m/s, were directed northward and had wavelengths close to 450 km. Other GPS receivers that were operating hundreds of km away from Huancayo show also similar TEC traces and provide a phase velocity equal to 150 m/s. This value was measured using the GPS at Piura, Cuzco and Huancayo. Based on this positive result, we conclude that small and/or regional arrays of GPS receivers can be used at low latitudes to study the role that gravity waves may have on seeding plasma bubbles. 1. Introduction Traveling ionospheric disturbances (TIDs) are the ionospheric manifestation of neutral density oscillations called atmospheric gravity waves (AGWs or GWs). AGWs originate in the troposphere or stratosphere, and often propagate to F- region heights, where they induce oscillations in the plasma density via ion- neutral coupling. When AGW winds drive plasma along magnetic field lines via ion-neutral collisions, classical TIDs result (1 3). However, at night the electrodynamics are favorable to the production of nonclassical or electrodynamic TIDs, such that vertical movement of the F-layer results (4 6). TIDs that reach F-region altitudes are divided into two classes: mediumscale (MSTIDs) and large-scale (LSTIDs).MSTIDs primarily originate from.

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号