{"title":"日食对东南亚地区共轭点F2层峰值电子密度的影响","authors":"Nimit Insakun, N. Wichaipanich, K. Hozumi","doi":"10.1109/ICITEED.2019.8930004","DOIUrl":null,"url":null,"abstract":"In this paper, the effect of March 9, 2016 solar eclipse on the F2 layer peak electron density (NmF2) at conjugate points in Southeast Asia is presented. NmF2 is calculated from the F2 layer critical frequency (foF2) that is manually scaled from three ionosonde stations in Southeast Asia region. Two ionosonde stations are in Thailand, namely Chiang Mai $(18.76^{\\circ} N, 98.93^{\\circ} E$, Dip $12.7^{\\circ} N)$ and Chumphon $(10.72^{\\circ} N, 99.38^{\\circ}$E, Dip $3.2^{\\circ} N)$. One station is in Indonesia, namely Kototabang $(0.2^{\\circ}\\mathrm{S}, 100.32^{\\circ}$E, Dip $10.1^{\\circ} S)$. These ionosonde stations are located at conjugate points in Southeast Asia. The daily interquartile range (every 15 minutes) of NmF2 data from 4$^{th}$ March to 15$^{th}$ March 2016 were analyzed the NmF2 variations during before and after the solar eclipse day on 9$^{th}$ March 2016. Besides, the monthly median, the upper boundary and lower boundary of NmF2 compared with the observed ones were used for analyzing the anomalous variations. The results of this study indicate that the NmF2 value increases during 2 days before and after the eclipse day while it decreases on solar eclipse day for all 3 stations.","PeriodicalId":6598,"journal":{"name":"2019 11th International Conference on Information Technology and Electrical Engineering (ICITEE)","volume":"9 1","pages":"1-5"},"PeriodicalIF":0.0000,"publicationDate":"2019-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"9 March 2016 Solar Eclipse Effects F2 Layer Peak Electron Density at Conjugate Points over Southeast Asia Region\",\"authors\":\"Nimit Insakun, N. Wichaipanich, K. Hozumi\",\"doi\":\"10.1109/ICITEED.2019.8930004\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"In this paper, the effect of March 9, 2016 solar eclipse on the F2 layer peak electron density (NmF2) at conjugate points in Southeast Asia is presented. NmF2 is calculated from the F2 layer critical frequency (foF2) that is manually scaled from three ionosonde stations in Southeast Asia region. Two ionosonde stations are in Thailand, namely Chiang Mai $(18.76^{\\\\circ} N, 98.93^{\\\\circ} E$, Dip $12.7^{\\\\circ} N)$ and Chumphon $(10.72^{\\\\circ} N, 99.38^{\\\\circ}$E, Dip $3.2^{\\\\circ} N)$. One station is in Indonesia, namely Kototabang $(0.2^{\\\\circ}\\\\mathrm{S}, 100.32^{\\\\circ}$E, Dip $10.1^{\\\\circ} S)$. These ionosonde stations are located at conjugate points in Southeast Asia. The daily interquartile range (every 15 minutes) of NmF2 data from 4$^{th}$ March to 15$^{th}$ March 2016 were analyzed the NmF2 variations during before and after the solar eclipse day on 9$^{th}$ March 2016. Besides, the monthly median, the upper boundary and lower boundary of NmF2 compared with the observed ones were used for analyzing the anomalous variations. The results of this study indicate that the NmF2 value increases during 2 days before and after the eclipse day while it decreases on solar eclipse day for all 3 stations.\",\"PeriodicalId\":6598,\"journal\":{\"name\":\"2019 11th International Conference on Information Technology and Electrical Engineering (ICITEE)\",\"volume\":\"9 1\",\"pages\":\"1-5\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2019-10-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"2019 11th International Conference on Information Technology and Electrical Engineering (ICITEE)\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1109/ICITEED.2019.8930004\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"2019 11th International Conference on Information Technology and Electrical Engineering (ICITEE)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/ICITEED.2019.8930004","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1
摘要
本文研究了2016年3月9日日食对东南亚共轭点F2层峰值电子密度(NmF2)的影响。NmF2是根据F2层临界频率(foF2)计算的,foF2是由东南亚地区三个电离层探空站人工缩放的。泰国有两个离子探空站,分别是清迈$(18.76^{\circ} N, 98.93^{\circ} E$, Dip $12.7^{\circ} N)$和春丰$(10.72^{\circ} N, 99.38^{\circ}$E, Dip $3.2^{\circ} N)$。一个站在印度尼西亚,即Kototabang $(0.2^{\circ}\ mathm {S}, 100.32^{\circ}$E, Dip $10.1^{\circ} S)$。这些电离层探空站位于东南亚的共轭点。利用2016年3月4日至15日NmF2数据的日四分位数差(每15分钟)分析2016年3月9日日食前后NmF2的变化。此外,利用NmF2的月中位数、上下限与观测值的比较分析了NmF2的异常变化。研究结果表明,3个台站的NmF2值在日食前后2 d内均呈上升趋势,而在日食当天则呈下降趋势。
9 March 2016 Solar Eclipse Effects F2 Layer Peak Electron Density at Conjugate Points over Southeast Asia Region
In this paper, the effect of March 9, 2016 solar eclipse on the F2 layer peak electron density (NmF2) at conjugate points in Southeast Asia is presented. NmF2 is calculated from the F2 layer critical frequency (foF2) that is manually scaled from three ionosonde stations in Southeast Asia region. Two ionosonde stations are in Thailand, namely Chiang Mai $(18.76^{\circ} N, 98.93^{\circ} E$, Dip $12.7^{\circ} N)$ and Chumphon $(10.72^{\circ} N, 99.38^{\circ}$E, Dip $3.2^{\circ} N)$. One station is in Indonesia, namely Kototabang $(0.2^{\circ}\mathrm{S}, 100.32^{\circ}$E, Dip $10.1^{\circ} S)$. These ionosonde stations are located at conjugate points in Southeast Asia. The daily interquartile range (every 15 minutes) of NmF2 data from 4$^{th}$ March to 15$^{th}$ March 2016 were analyzed the NmF2 variations during before and after the solar eclipse day on 9$^{th}$ March 2016. Besides, the monthly median, the upper boundary and lower boundary of NmF2 compared with the observed ones were used for analyzing the anomalous variations. The results of this study indicate that the NmF2 value increases during 2 days before and after the eclipse day while it decreases on solar eclipse day for all 3 stations.