...
首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Correction to 'Unified PCN and PCS indices: Method of calculation,physical sense, and dependence on the IMF azimuthal physical sense, and dependence on the IMF azimuthal
【24h】

Correction to 'Unified PCN and PCS indices: Method of calculation,physical sense, and dependence on the IMF azimuthal physical sense, and dependence on the IMF azimuthal

机译:修正“统一PCN和pc指数:方法计算的物理意义,和依赖国际货币基金组织物理意义上,方位和依赖在IMF方位

获取原文
获取原文并翻译 | 示例
           

摘要

In the paper "Unified PCN and PCS indices: Methodof calculation, physical sense, and dependence on the IMFazimuthal and northward components" by Oleg Troshichevet al. (Journal of Geophysical Research, 111, A05208,doi:10.1029/2005JA011402, 2006), two errors should benoticed. One appears in equation (1). Here the D and Hcomponents have been interchanged in the formula. Thecorrect version is Of = SH sin -y SD cosy.(1) We have carefully checked to verify that the erroneousformula has not been used in the programs used to handlethe magnetic data. Thus the error is a typo withoutconsequences for the data processing and the results reported in the paper. However, the correction is importantin order to avoid inadvertent use of the erroneous equation.[2] The second error appears in the name of the magneticcomponent displayed in Figure 1. Figure 1 is used toillustrate the method for determination of the quiet levelin evaluation of the magnetic deviations. Figure 1 actuallydisplays the D (not the H) component of the magnetic fieldmeasured at Vostok station in June 2002. Figure 1 is usedonly for illustration, and the corresponding plot of the Hcomponent is very similar. Thus the typo has no conse-quences and is considered to be of minor importance.Janzhura and Troshichev [2008] use the same figure withthe same typo.
机译:摘要“统一PCN和pc指数:方法计算,物理意义,依赖IMFazimuthal继续向北而行组件”由奥列格Troshichevet。(《地球物理研究,111,应注意的错误。(1)。在这里,D和Hcomponents互换的公式。是= SH sin - y SD舒适。(1)我们已经仔细吗检查验证erroneousformula用于handlethe未使用的项目磁数据。数据处理和withoutconsequences在报纸上报道的结果。修正角色来避免无意的使用错误的方程。[2]第二个错误出现在的名称magneticcomponent显示在图1。toillustrate方法用于测定安静的levelin磁的评价偏差。的磁fieldmeasured H)组件2002年6月Vostok站。插图,和相应的块Hcomponent非常相似。没有conse-quences,被认为是次要的的重要性。相同的图与相同的错误。

著录项

相似文献

  • 外文文献
  • 中文文献
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