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首页> 外文期刊>Journal of atmospheric and solar-terrestrial physics >Near-continual ground-based nighttime observations of thermospheric neutral winds and temperatures over equatorial Brazil from 2009 to 2012
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Near-continual ground-based nighttime observations of thermospheric neutral winds and temperatures over equatorial Brazil from 2009 to 2012

机译:2009年至2012年近赤道巴西近地层的热层中性风和温度的夜间观测

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摘要

We present measurements of thermospheric neutral winds and temperatures measured by two Fabry-Perot interferometers (FPIs) operating in northeastern Brazil, in the equatorial region, over the period of September 2009 through June 2012. The FPIs observe the Doppler shift and broadening of the nighttime 630.0-nm emission originating at altitudes of approximately 240km. The temperatures indicate a strong dependence on solar flux conditions, as captured by the F_(10.7) index, which ranged from ~72 to 175 solar flux units over the duration of the study. The signature of the midnight temperature maximum is seen in the data, recurring each year during the local summer months (October through February). Throughout the year, the thermospheric zonal winds show an initial increase in eastward flow after sunset followed by a reduction in the midnight and early morning hours. This reduction in the zonal flow is most rapid in the local summer months. The thermospheric meridional winds show the expected signature of trans-equatorial flow from the summer to winter hemisphere. Superposed on this during the local summer months is a time of equatorward flow during the mid-evening period, 22-23LT, which is likely a manifestation of the semi-diurnal thermal tidal wave moving upward into the lower thermosphere region from below. The thermospheric neutral winds do not show as much of a dependence on the solar flux as the thermospheric neutral temperatures do, at least for the range of fluxes covered during the study period.
机译:我们介绍了在2009年9月至2012年6月期间在巴西东北部赤道地区运行的两台Fabry-Perot干涉仪(FPI)测得的热圈中性风和温度。这些FPI观测到多普勒频移和夜间范围扩大从约240 km的高度发出630.0 nm的光。温度表明强烈依赖于太阳通量条件,如F_(10.7)指数所记录的那样,在整个研究过程中,温度范围约为72至175个太阳通量单位。在数据中可以看到午夜最高温度的特征,每年夏季局部月份(10月至2月)都会重复出现。全年,热层带风显示出日落之后东风的最初增加,随后的午夜和清晨时间减少。在当地夏季,这种地带流量的减少最快。从夏季到冬季半球,热圈子午风显示出跨赤道流的预期特征。在当地夏季月份中,这是一个叠加的过程,在中午期间是赤道流时间22-23 LT,这很可能是半日热潮汐从下方向上移动到较低热层区域的一种表现。至少在研究期内,热球中性风对太阳通量的依赖性不如热球中性温度高。

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