首页> 美国卫生研究院文献>Scientific Reports >Longitudinal variations in thermospheric parameters under summer noontime conditions inferred from ionospheric observations: A comparison with empirical models
【2h】

Longitudinal variations in thermospheric parameters under summer noontime conditions inferred from ionospheric observations: A comparison with empirical models

机译:根据电离层观测结果推断的夏季中午条件下热层参数的纵向变化:与经验模型的比较

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

Longitudinal variations in the thermospheric neutral composition ([O] and [N2]) and exospheric temperature Tex have been inferred from June monthly median noontime foF1 and foF2 observations at mid-latitudes to check for consistency with empirical MSIS models. In general, a similarity in longitudinal variations has been demonstrated, and this is interesting, as similar variations were obtained with very different methods and different data sources. Both inferred and MSISE-00 modelled height-integrated O/N2 ratios are comparable to TIMED/GUVI observations only under solar minimum conditions but differ substantially under high solar activity. The retrieved height-integrated O/N2 ratio longitudinal variations are small (∼15%) in comparison to the observed NmF2 variations under high solar activity. The height-integrated O/N2 ratio cannot be incorporated into the F2-layer formation mechanism; therefore, such observations cannot be used for any quantitative interpretation of NmF2 variations.
机译:从中纬度6月每月中午foF1和foF2观测值中推断出热层中性成分([O]和[N2])和大气层温度Tex的纵向变化,以检验与经验MSIS模型的一致性。通常,已经证明了纵向变化的相似性,这很有趣,因为使用非常不同的方法和不同的数据源可以获得相似的变化。推断的和MSISE-00建模的高度积分O / N2比值仅在太阳最低条件下才可与TIMED / GUVI观测值相提并论,但在太阳活动较高时却大不相同。与在高太阳活动下观察到的NmF2变化相比,所获得的高度积分O / N2比纵向变化小(约15%)。高度积分的O / N2比不能纳入F2层的形成机理;因此,这种观察不能用于NmF2变异的任何定量解释。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

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