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首页> 外文期刊>Journal of atmospheric and solar-terrestrial physics >Quiet-condition hmF2, NmF2, and B-0 variations at Jicamarca and comparison with IRI-2001during solar maximum
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Quiet-condition hmF2, NmF2, and B-0 variations at Jicamarca and comparison with IRI-2001during solar maximum

机译:Jicamarca的安静条件hmF2,NmF2和B-0变化以及与太阳最大期间IRI-2001的比较

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We use the measurements of the Jicamarca digisonde to examine the variations in F2 layer peak electron density (NmF2), its height (hmF2), and the F2 layer thickness parameter (B-0) near the dip equator. The hourly ionograms during geomagnetic quiet-conditions for a 12-month period close to the maximum solar activity, April 1999-March 2000, are used to calculate the monthly averages of these parameters, for each month. The averages are compared with the International Reference Ionosphere (IRI)-2001 model values. The results show that the higher hmF2 values during daytime, associated with the upward velocity, are mainly responsible for the greater values of NmF2 and B-0; while the nighttime lower hmF2, related to the downward velocity, are responsible for the smaller NmF2 and B-0. For daytime, hmF2 and NmF2 are correlated with the solar activity in the equinoctial and summer months. The hmF2 and B-0 peaks at sunset with an associated sharp decrease in NmF2 are presented in the equinoctial and summer months, but not in the winter months. Comparison of the measured hmF2 values with the International Radio Consultative Committee (CCIR) maps used in IRI-2001 (IRI-CCIR) reveals an IRI overestimate in hmF2 during daytime. The most significant discrepancy is that the IRI-CCIR does not model the post-sunset peak in hmF2. For the NmF2 comparison, the values obtained from both the CCIR and URSI maps are generally close to the observed values. For the B-0 comparison, the highest discrepancy between the observation and the Gulyaeva option (IRI-Gulyaeva) is the location of the annual maximum for the daytime values, also the winter daytime predictions are too low. Additionally, the significant negative difference between the observation and the B-0-table option (IRI-B-0-table) provides a slightly better prediction, except for 0400-1000 LT when the model significantly overestimates. The post-sunset peak in B-0 at some months is predicted by neither the IRI-Gulyaeva nor the IRI-B-0-table options. (C) 2006 Elsevier Ltd. All rights reserved.
机译:我们使用Jicamarca digisonde的测量结果来检查F2层峰值电子密度(NmF2),其高度(hmF2)以及倾角赤道附近的F2层厚度参数(B-0)的变化。在接近最大太阳活动(1999年4月至2000年3月)的12个月地磁安静条件下的每小时离子图用于计算每个月这些参数的月平均值。将平均值与国际参考电离层(IRI)-2001模型值进行比较。结果表明,白天较高的hmF2值与上升的速度有关,主要是NmF2和B-0的值较大的原因。而与下降速度有关的夜间较低的hmF2则是较小的NmF2和B-0的原因。在白天,hmF2和NmF2与在等分和夏季月份的太阳活动相关。在等分和夏季月份出现hmF2和B-0峰,而NmF2随之急剧下降,而在冬季月份则不出现。将测得的hmF2值与IRI-2001中使用的国际无线电咨询委员会(CCIR)图表(IRI-CCIR)进行比较,发现白天hmF2中的IRI高估了。最显着的差异是IRI-CCIR并未对hmF2中的日落后峰值进行建模。对于NmF2比较,从CCIR和URSI图获得的值通常接近观察值。对于B-0比较,观测值与Gulyaeva选项(IRI-Gulyaeva)之间的最大差异是白天值的年度最大值所在,而且冬季白天的预测值也太低。此外,观测值和B-0表选项(IRI-B-0表)之间的显着负差提供了更好的预测,但模型显着高估时为0400-1000 LT。 IRI-Gulyaeva或IRI-B-0-table选项均未预测B-0日落后的峰值。 (C)2006 Elsevier Ltd.保留所有权利。

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