资源环境科技发展态势分析平台

We report the first global, time-dependent simulation of the Mars upper atmospheric responses to a realistic solar flare event, an X8.2 eruption on 10 September 2017. The Mars Global Ionosphere-Thermosphere Model runs with realistically specified flare irradiance, giving results in reasonably good agreement with the Mars Atmosphere and Volatile EvolutioN spacecraft measurements. It is found that the ionized and neutral regimes of the upper atmosphere are significantly disturbed by the flare but react differently. The ionospheric electron density enhancement is concentrated below similar to 110-km altitude due to enhanced solar X-rays, closely following the time evolution of the flare. The neutral atmospheric perturbation increases with altitude and is important above similar to 150-km altitude, in association with atmospheric upwelling driven by solar extreme ultraviolet heating. It takes similar to 2.5 hr past the flare peak to reach the maximum disturbance and then additional similar to 10 hr to generally settle down to preflare levels.