Mlynczak Martin G, Knipp Delores J, Hunt Linda A, Gaebler John, Matsuo Tomoko, Kilcommons Liam M, Young Cindy L
NASA Langley Research Center, Hampton, VA, USA.
Aerospace Engineering Sciences Department, University of Colorado Boulder, Boulder, CO, USA.
Space Weather. 2018 Apr;16(4):363-375. doi: 10.1002/2017SW001757.
Infrared radiative cooling by nitric oxide (NO) and carbon dioxide (CO) modulates the thermosphere's density and thermal response to geomagnetic storms. Satellite tracking and collision avoidance planning require accurate density forecasts during these events. Over the past several years, failed density forecasts have been tied to the onset of rapid and significant cooling due to production of NO and its associated radiative cooling via emission of infrared radiation at 5.3 μm. These results have been diagnosed, after the fact, through analyses of measurements of infrared cooling made by the Sounding of the Atmosphere using Broadband Emission Radiometry instrument now in orbit over 16 years on the National Aeronautics and Space Administration Thermosphere, Ionosphere, Mesosphere Energetics and Dynamics satellite. Radiative cooling rates for NO and CO have been further shown to be directly correlated with composition and exospheric temperature changes during geomagnetic storms. These results strongly suggest that a network of smallsats observing the infrared radiative cooling of the thermosphere could serve as space weather sentinels. These sentinels would observe and provide radiative cooling rate data in real time to generate nowcasts of density and aerodynamic drag on space vehicles. Currently, radiative cooling is not directly considered in operational space weather forecast models. In addition, recent research has shown that different geomagnetic storm types generate substantially different infrared radiative response, and hence, substantially different thermospheric density response. The ability to identify these storms, and to measure and predict the Earth's response to them, should enable substantial improvement in thermospheric density forecasts.
一氧化氮(NO)和二氧化碳(CO)引起的红外辐射冷却调节了热层的密度以及对地磁暴的热响应。在这些事件期间,卫星跟踪和碰撞避免规划需要准确的密度预测。在过去几年中,密度预测失败与由于NO的产生及其通过5.3μm红外辐射发射所伴随的辐射冷却导致的快速且显著的冷却开始有关。这些结果事后通过对使用宽带发射辐射测量仪进行的大气探测所做的红外冷却测量分析得以诊断,该仪器已在国家航空航天局的热层、电离层、中间层能量学和动力学卫星上运行了16年。NO和CO的辐射冷却率进一步显示与地磁暴期间的成分和外层温度变化直接相关。这些结果强烈表明,一个观测热层红外辐射冷却的小卫星网络可以充当空间天气哨兵。这些哨兵将实时观测并提供辐射冷却率数据,以生成对航天器密度和气动阻力的临近预报。目前,业务空间天气预报模型中并未直接考虑辐射冷却。此外,最近的研究表明,不同类型的地磁暴会产生截然不同的红外辐射响应,因此也会产生截然不同的热层密度响应。识别这些风暴以及测量和预测地球对它们的响应的能力,应该能够大幅改进热层密度预测。