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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Impact of M-solar flare-induced solar proton event on mesospheric Na layer over Utah (41.8 degrees N,112 degrees W)
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Impact of M-solar flare-induced solar proton event on mesospheric Na layer over Utah (41.8 degrees N,112 degrees W)

机译:M-Solar Flare诱导的Solar Proton事件对犹他州的Mesompheric Na层的影响(41.8度,112°W)

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The influence of solar proton event, induced by M-solar flare, on the mesospheric sodium layer is studied over a midlatitude location Utah(41.8 degrees N, 112 degrees W) during 19 July 2012. The variation in sodium concentration (cm(-3)) is examined with temperature and atomic oxygen concentration obtained from NRLMSISE-00 empirical model. In the vicinity of peak sodium concentration, the temperature shows a strong negative correlation with sodium concentration, atomic oxygen concentration shows a positive correlation with sodium concentration. An enhancement in sodium concentration is observed during the solar proton event with highest concentration at the time of maximum proton flux. The altitude of peak sodium concentration shows a downward movement with lowest altitude corresponding to the time of maximum proton flux. However, the altitude of peak sodium concentration is found in the altitude region of 85-90 km throughout the solar proton event.
机译:M-Solar Flare诱导的太阳能质子事件的影响在2012年7月19日的中间位置定位(41.8度,112摄氏度)的中间位置定位。钠浓度的变化(cm(-3 )通过温度和由NRLMSISE-00实证模型获得的温度和原子氧浓度检查。 在钠钠浓度附近,温度显示出与钠浓度的强负相关,原子氧浓度显示与钠浓度的正相关。 在最大质子通量时的最高浓度的太阳能质子事件期间观察到钠浓度的增强。 峰值钠浓度的高度显示出与最大质子通量的时间相对应的最低高度的向下运动。 然而,在整个太阳能质子事件中,在85-90km的高度区域发现高钠浓度的高度。

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