极区电离层NmF2观测与国际参考电离层对比研究OA北大核心CSTPCD
Comparison of polar region ionospheric NmF2 observations with the Interna-tional Reference Ionosphere
利用南北极极隙区与极光带纬度 3 个台站对电离层F2 层峰值电子密度(NmF2)长达 1 个太阳活动周的观测数据,对国际参考电离层 IRI-2016 模型在极区的适用性进行系统的定量研究.结果表明,在极光带纬度的北极Tromsø站,IRI预测与观测符合最好,大部分季节相对误差在 40%以内,在太阳活动高年略好于太阳活动低年.在极隙区纬度的南极中山站和Longyearbyen站,IRI预测精度在太阳活动低年高于太阳活动高年.在中山站和北极Longyearbyen站仅个别月份相对误差在 20%以内,大部分月份相对误差超过 40%,冬季相对误差接近 100%,特别是Longyearbyen站,在太阳活动高年冬季相对误差超过 100%.从季节上看,3个台站都是冬季符合最差,夏季符合最好.IRI-2016 模型对极区电离层进行预测时,难以如实反映极区等离子体对流和能量粒子沉降等极区特有的物理过程对极区电离层NmF2 的影响.
This article systematically and quantitatively explores the applicability of the International Reference Iono-sphere IRI-2016 model in polar regions,using observation data of the ionospheric F2-layer peak electron density(NmF2)acquired one solar cycle at three stations within the polar cusp region and the latitude of the aurora belt.The results showed good consistency between the IRI-2016 predictions and observation at the auroral latitude Tromsø Station,with relative errors less than 40%in most seasons.The accuracy of IRI-2016 prediction was marginally higher during solar maximum years than during solar minimum years at Tromsø,conversely it was higher during solar minimum years than during solar maximum years at the Zhongshan and Longyearbyen stations.At Zhongshan and Longyearbyen stations,the relative error is less than 20%in only a few months,more than 40%in most months,and is almost 100%in winter.Especially at Longyearbyen Station,the relative error is more than 100%in winter during solar maximum years.Overall consistency between observations and IRI-2016 prediction perform was low-est in winter,and highest in summer at all three stations.Plasma convection strongly influences NmF2 and particle precipitation in the polar regions,but the IRI-2016 model could not accurately reproduce these physical processes.
徐盛;李培豪;廖小倩;刘瑞源;陈相材
郑州轻工业大学计算机与通信工程学院,河南 郑州 450000自然资源部极地科学重点实验室,中国极地研究中心(中国极地研究所),上海 200136
极区电离层国际参考电离层IRI-2016模型F2层峰值电子密度(NmF2)
polar ionosphereInternational Reference Ionosphere IRI-2016 modelF2 layer peak electron density(NmF2)
《极地研究》 2024 (001)
26-36 / 11
国家自然科学基金项目(41804155,42130210,42120104003)和上海市科技创新行动计划(21DZ1206100)资助
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