{"title":"高纬度地区F2电离层的正常状态","authors":"A. Belehaki , G. Moraitis , I. Tsagouri","doi":"10.1016/S1464-1917(01)00004-6","DOIUrl":null,"url":null,"abstract":"<div><p>The use of monthly median values to determine the normal level of the undisturbed F2 layer, leads often to inconsistent results regarding the type of ionospheric disturbance and quietness as well. Recently Belehaki (2000) proposed an hourly local ionospheric index <em>f<sub>n</sub>F2</em> to define the normal level of the F2 layer at middle latitudes. In this paper we apply the <em>f<sub>n</sub>F2</em> index to observations from a high latitude station, where geomagnetic activity strongly influence the temporal and spatial behaviour of the ionospheric layers, for investigating and testing the usefulness of the <em>f<sub>n</sub>F2</em> index on a planetary scale. From the analysis that follows, it was revealed that during intervals of low magnetospheric activity, <em>f<sub>n</sub>F2</em> index shows a very good fit to the observed <em>f<sub>o</sub>F2</em> parameter, comparing to the monthly median <em>f<sub>o</sub>F2</em> behaviour. On the other hand, enhanced magnetospheric activity does not affect the <em>f<sub>n</sub>F2</em> index, which daily variation is a function of the sunspot number itself. In summary, the <em>f<sub>n</sub>F2</em> index can be used as a measure of the undisturbed F2 layer at middle and high latitudes as well, caution though is needed in the definition of the quiet magnetospheric intervals, which for the needs of this work it was approached as a function of the <em>aa</em>-index for middle latitudes, whereas the <em>AE</em>-index was used for auroral latitudes.</p></div>","PeriodicalId":101026,"journal":{"name":"Physics and Chemistry of the Earth, Part C: Solar, Terrestrial & Planetary Science","volume":"26 5","pages":"Pages 309-313"},"PeriodicalIF":0.0000,"publicationDate":"2001-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/S1464-1917(01)00004-6","citationCount":"3","resultStr":"{\"title\":\"The normal state of the F2 ionospheric layer at high latitudes\",\"authors\":\"A. Belehaki , G. Moraitis , I. Tsagouri\",\"doi\":\"10.1016/S1464-1917(01)00004-6\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>The use of monthly median values to determine the normal level of the undisturbed F2 layer, leads often to inconsistent results regarding the type of ionospheric disturbance and quietness as well. Recently Belehaki (2000) proposed an hourly local ionospheric index <em>f<sub>n</sub>F2</em> to define the normal level of the F2 layer at middle latitudes. In this paper we apply the <em>f<sub>n</sub>F2</em> index to observations from a high latitude station, where geomagnetic activity strongly influence the temporal and spatial behaviour of the ionospheric layers, for investigating and testing the usefulness of the <em>f<sub>n</sub>F2</em> index on a planetary scale. From the analysis that follows, it was revealed that during intervals of low magnetospheric activity, <em>f<sub>n</sub>F2</em> index shows a very good fit to the observed <em>f<sub>o</sub>F2</em> parameter, comparing to the monthly median <em>f<sub>o</sub>F2</em> behaviour. On the other hand, enhanced magnetospheric activity does not affect the <em>f<sub>n</sub>F2</em> index, which daily variation is a function of the sunspot number itself. In summary, the <em>f<sub>n</sub>F2</em> index can be used as a measure of the undisturbed F2 layer at middle and high latitudes as well, caution though is needed in the definition of the quiet magnetospheric intervals, which for the needs of this work it was approached as a function of the <em>aa</em>-index for middle latitudes, whereas the <em>AE</em>-index was used for auroral latitudes.</p></div>\",\"PeriodicalId\":101026,\"journal\":{\"name\":\"Physics and Chemistry of the Earth, Part C: Solar, Terrestrial & Planetary Science\",\"volume\":\"26 5\",\"pages\":\"Pages 309-313\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2001-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/S1464-1917(01)00004-6\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Physics and Chemistry of the Earth, Part C: Solar, Terrestrial & Planetary Science\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S1464191701000046\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Physics and Chemistry of the Earth, Part C: Solar, Terrestrial & Planetary Science","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1464191701000046","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
The normal state of the F2 ionospheric layer at high latitudes
The use of monthly median values to determine the normal level of the undisturbed F2 layer, leads often to inconsistent results regarding the type of ionospheric disturbance and quietness as well. Recently Belehaki (2000) proposed an hourly local ionospheric index fnF2 to define the normal level of the F2 layer at middle latitudes. In this paper we apply the fnF2 index to observations from a high latitude station, where geomagnetic activity strongly influence the temporal and spatial behaviour of the ionospheric layers, for investigating and testing the usefulness of the fnF2 index on a planetary scale. From the analysis that follows, it was revealed that during intervals of low magnetospheric activity, fnF2 index shows a very good fit to the observed foF2 parameter, comparing to the monthly median foF2 behaviour. On the other hand, enhanced magnetospheric activity does not affect the fnF2 index, which daily variation is a function of the sunspot number itself. In summary, the fnF2 index can be used as a measure of the undisturbed F2 layer at middle and high latitudes as well, caution though is needed in the definition of the quiet magnetospheric intervals, which for the needs of this work it was approached as a function of the aa-index for middle latitudes, whereas the AE-index was used for auroral latitudes.