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Validation of SABER temperature measurements using ground-based instruments

机译:使用基于地面的仪器验证Saber温度测量

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The sounding of the atmosphere using broadband emission radiometry (SABER) instrument is one of four instruments mounted on the thermosphere ionosphere mesosphere energetics and dynamics (TIMED) satellite. SABER sounds the MLTI (the mesosphere and lower thermosphere/ionosphere) region of the earth's atmosphere by measuring infrared limb emission. The instrument measures accurate values of atmospheric limb radiance that are ground processed to retrieve temperature, ozone, water vapor, carbon dioxide, and key parameters describing the energetics of the high atmosphere. SABER results are being used to study the chemistry and dynamics of the mesosphere and the effects on the atmosphere due to major solar storm events. The temperature data from SABER measurements is plotted against temperature measurements collected from several ground based instruments for the purpose of verifying the SABER data. These ground based instruments are located all over the world, including e.g. Boulder, Colorado; Mauna Loa, Hawaii; and parts of Russia. The ground based instruments used for validation of SABER temperatures have already undergone scrutiny and error analyses, and are used as a benchmark to validate data collected from SABER. Furthermore, nitric oxide measurements collected during is period of heightened solar activity is used to create global plots to illustrate the changing atmosphere as the Sun's radiation interacts with the Earth's atmosphere. These solar activity global plots illustrate the effects on the atmosphere as a result of solar flares, solar storms, and other solar activities.
机译:使用宽带发射辐射率(Saber)仪器的气氛探测是安装在热圈电离层Mese圈层能量和动力学(定时)卫星上安装的四种仪器之一。通过测量红外线肢体排放,Saber声称地球氛围的MLTI(介质圈和较低的热圈/电离层)区域。仪器测量准确的大气肢体辐射值,该辐射被加工以检索温度,臭氧,水蒸气,二氧化碳和描述高气氛的能量学的关键参数。 SABER结果用于研究介质圈的化学和动力学以及由于主要的太阳风暴事件为大气的影响。来自Sabre测量的温度数据被绘制,以验证Sabre数据的若干地基仪器收集的温度测量。这些基于地面的仪器位于全球各地,包括例如:博尔德,科罗拉多;夏威夷Mauna Loa;和俄罗斯的一部分。用于验证Sabre温度的基于地面的仪器已经经历了审查和错误分析,并用作验证从Saber收集的数据的基准。此外,在高度的太阳能活动期间收集的一氧化氮测量用于创建全球地块,以说明随着太阳的辐射与地球大气相互作用的变化气氛。这些太阳能活动全球地块由于太阳能耀斑,太阳风暴和其他太阳能活动而说明了对大气的影响。

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