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Comparisons of thermospheric wind and temperature measurements in equatorial Brazil to Whole Atmosphere Model Predictions

机译:赤道巴西的热层风和温度测量与整个大气模型预测的比较

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The results from the Whole Atmosphere Model (WAM) at 240km are compared with measurements of equatorial thermospheric winds and temperatures acquired by nearly continual nighttime Fabry-Perot interferometer (FPI) measurements made in northeastern Brazil from September 2009 to August 2012. These comparisons show generally good agreement for the zonal winds with only slight differences seen in regard to the early morning period. For the evening period of 21-23 LT the observed meridional winds differed from the WAM predictions in two respects. First, while the flow direction was generally correct, the speeds of observed cross-hemispheric flow from the summer to the winter hemisphere were generally somewhat greater by 25 to 35ms~(-1) than the predicted speeds from WAM. In contrast, the observed meridional winds are found to be weaker than the WAM results for winter months for all three years. Second, although the observations and predictions both show similar timing and amplitude for a 3-h period of northward flow in September and October, the observations indicate a shift in the timing of this flow of about 1h, from ~22 LT in September and October to ~21 LT in December. The WAM predictions show a systematic shift in phase from 21-00 LT in September to 18-21 LT in December. Regarding temperature, the WAM predictions show a midnight temperature maximum (MTM) with a peak amplitude of 50-65K, in agreement with the observations. However, the WAM results also show a systematic shift in timing of the MTM occurrence, with the MTM peak seen at ~22 LT in summer and at 00 LT in winter. In contrast, the FPI monthly climatology data show the timing of the MTM peak to be 00±0.5 LT for all months except winter, when the MTM peak is not clearly evident.
机译:将2009年9月至2012年8月在巴西东北部进行的近乎连续的夜间Fabry-Perot干涉仪(FPI)测量获得的赤道热球风和温度测量结果与240 km的整体大气模型(WAM)的结果进行了比较。与纬向风有很好的一致性,与清晨相比只有很小的差异。在21-23 LT的傍晚,观测到的子午风在两个方面与WAM的预测不同。首先,虽然流动方向总体上是正确的,但从夏季到冬季半球的跨半球流动速度通常比WAM的预测速度大25至35ms〜(-1)。相反,在整个三年中,观测到的子午风均弱于冬季的WAM结果。其次,尽管观测和预测都显示了在9月和10月的北流3小时内相似的时间和振幅,但观测结果表明,该流的时间从9月和10月的约22 LT偏移了约1 h。到12月的〜21 LT。 WAM预测显示阶段性系统转移,从9月的21-00 LT到12月的18-21 LT。关于温度,WAM预测显示午夜最高温度(MTM),其峰值幅度为50-65K,与观察结果一致。但是,WAM结果也显示了MTM发生时间的系统性变化,MTM高峰在夏季约22 LT,冬季在00 LT。相比之下,FPI月度气候数据显示MTM高峰时间不明显,除冬季外,所有月份MTM高峰的时间均为00±0.5 LT。

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