Victor U. Chukwuma , Bolarinwa J. Adekoya , Eugene O. Onori , Oluwafunmilayo O. Ometan , Aghogho Ogwala
{"title":"强烈地磁风暴期间太阳风结构的全球相对地球有效性:以三明治结构CME驱动的强烈地磁风暴为例","authors":"Victor U. Chukwuma , Bolarinwa J. Adekoya , Eugene O. Onori , Oluwafunmilayo O. Ometan , Aghogho Ogwala","doi":"10.1016/j.asr.2025.02.013","DOIUrl":null,"url":null,"abstract":"<div><div>An investigation was undertaken of ionospheric responses during the geomagnetic storm of Oct 13, 2016, regarding the observed configuration of sheath I-magnetic cloud-sheath II sandwich structure of the CME along the equatorial-, low-, and mid-latitude ionosphere along 96–145<sup>o</sup>E meridian lines. The aim of the study was to primarily reveal the global relative geo-effectiveness of the solar wind structures and elucidate the dominant storm-time driving mechanism that accounts for the ionospheric responses during the different phases of the storm.</div><div>Our results indicate that the occurrence of positive storms at some of the stations with intense depletion of the <span><math><mrow><mrow><mo>[</mo><mi>O</mi><mo>]</mo></mrow><mo>/</mo><msub><mrow><mo>[</mo><mi>N</mi></mrow><mn>2</mn></msub><mrow><mo>]</mo></mrow></mrow></math></span> ratio during the recovery phase while pointing to the efficacy of plasma exchange between the plasmasphere and the ionosphere draws attention to the fact that ionospheric response is a phenomenon that is possibly due to the complex interplay among the different drivers; it is often difficult to distinguish one driving force from another based on observations alone.</div><div>Our results also show that sheath I, though hemispherically geoeffective lacked global geo-effectiveness. The sheath II, with a global geo-effectiveness of 54.01 %, is more geoeffective than the magnetic cloud which has a geoeffective of 45.99 %. The comparatively higher geo-effectiveness of Sheath II is plausibly due to increased solar wind pressure. <span><span>Boudouridis et al. (2005)</span></span> have shown that southward IMF conditions combined with increased high solar wind pressure lead to enhanced coupling between the solar wind and the terrestrial magnetosphere which significantly increases the geo-effectiveness of the solar wind. Furthermore, the non-geo-effectiveness of Sheath I is plausibly a result of the fact that the period of the spatiotemporal location of Sheath I when the solar wind pressure was high <span><math><mrow><mo>(</mo><mn>6.83</mn><mi>n</mi><mi>P</mi><mi>a</mi><mo>≤</mo><mi>P</mi><mi>s</mi><mi>w</mi><mo>≤</mo><mn>10.23</mn><mi>n</mi><mi>P</mi><mi>a</mi><mo>)</mo></mrow></math></span> the stations along 96–145<sup>o</sup>E meridian lines were on the dayside. And the increased solar wind dynamic pressure during the spatiotemporal location of Sheath II possibly contributed to the observed polarity differences with the magnetic cloud producing interhemispheric positive storms, and Sheath II producing negative interhemispheric negative storms.</div></div>","PeriodicalId":50850,"journal":{"name":"Advances in Space Research","volume":"75 8","pages":"Pages 6431-6453"},"PeriodicalIF":2.8000,"publicationDate":"2025-02-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"On global relative geo-effectiveness of solar wind structures during an intense geomagnetic storm: A case study of an intense geomagnetic storm driven by sandwich-structured CME\",\"authors\":\"Victor U. Chukwuma , Bolarinwa J. Adekoya , Eugene O. Onori , Oluwafunmilayo O. Ometan , Aghogho Ogwala\",\"doi\":\"10.1016/j.asr.2025.02.013\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>An investigation was undertaken of ionospheric responses during the geomagnetic storm of Oct 13, 2016, regarding the observed configuration of sheath I-magnetic cloud-sheath II sandwich structure of the CME along the equatorial-, low-, and mid-latitude ionosphere along 96–145<sup>o</sup>E meridian lines. The aim of the study was to primarily reveal the global relative geo-effectiveness of the solar wind structures and elucidate the dominant storm-time driving mechanism that accounts for the ionospheric responses during the different phases of the storm.</div><div>Our results indicate that the occurrence of positive storms at some of the stations with intense depletion of the <span><math><mrow><mrow><mo>[</mo><mi>O</mi><mo>]</mo></mrow><mo>/</mo><msub><mrow><mo>[</mo><mi>N</mi></mrow><mn>2</mn></msub><mrow><mo>]</mo></mrow></mrow></math></span> ratio during the recovery phase while pointing to the efficacy of plasma exchange between the plasmasphere and the ionosphere draws attention to the fact that ionospheric response is a phenomenon that is possibly due to the complex interplay among the different drivers; it is often difficult to distinguish one driving force from another based on observations alone.</div><div>Our results also show that sheath I, though hemispherically geoeffective lacked global geo-effectiveness. The sheath II, with a global geo-effectiveness of 54.01 %, is more geoeffective than the magnetic cloud which has a geoeffective of 45.99 %. The comparatively higher geo-effectiveness of Sheath II is plausibly due to increased solar wind pressure. <span><span>Boudouridis et al. (2005)</span></span> have shown that southward IMF conditions combined with increased high solar wind pressure lead to enhanced coupling between the solar wind and the terrestrial magnetosphere which significantly increases the geo-effectiveness of the solar wind. Furthermore, the non-geo-effectiveness of Sheath I is plausibly a result of the fact that the period of the spatiotemporal location of Sheath I when the solar wind pressure was high <span><math><mrow><mo>(</mo><mn>6.83</mn><mi>n</mi><mi>P</mi><mi>a</mi><mo>≤</mo><mi>P</mi><mi>s</mi><mi>w</mi><mo>≤</mo><mn>10.23</mn><mi>n</mi><mi>P</mi><mi>a</mi><mo>)</mo></mrow></math></span> the stations along 96–145<sup>o</sup>E meridian lines were on the dayside. And the increased solar wind dynamic pressure during the spatiotemporal location of Sheath II possibly contributed to the observed polarity differences with the magnetic cloud producing interhemispheric positive storms, and Sheath II producing negative interhemispheric negative storms.</div></div>\",\"PeriodicalId\":50850,\"journal\":{\"name\":\"Advances in Space Research\",\"volume\":\"75 8\",\"pages\":\"Pages 6431-6453\"},\"PeriodicalIF\":2.8000,\"publicationDate\":\"2025-02-13\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Advances in Space Research\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0273117725001322\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"ASTRONOMY & ASTROPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Advances in Space Research","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0273117725001322","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ASTRONOMY & ASTROPHYSICS","Score":null,"Total":0}
On global relative geo-effectiveness of solar wind structures during an intense geomagnetic storm: A case study of an intense geomagnetic storm driven by sandwich-structured CME
An investigation was undertaken of ionospheric responses during the geomagnetic storm of Oct 13, 2016, regarding the observed configuration of sheath I-magnetic cloud-sheath II sandwich structure of the CME along the equatorial-, low-, and mid-latitude ionosphere along 96–145oE meridian lines. The aim of the study was to primarily reveal the global relative geo-effectiveness of the solar wind structures and elucidate the dominant storm-time driving mechanism that accounts for the ionospheric responses during the different phases of the storm.
Our results indicate that the occurrence of positive storms at some of the stations with intense depletion of the ratio during the recovery phase while pointing to the efficacy of plasma exchange between the plasmasphere and the ionosphere draws attention to the fact that ionospheric response is a phenomenon that is possibly due to the complex interplay among the different drivers; it is often difficult to distinguish one driving force from another based on observations alone.
Our results also show that sheath I, though hemispherically geoeffective lacked global geo-effectiveness. The sheath II, with a global geo-effectiveness of 54.01 %, is more geoeffective than the magnetic cloud which has a geoeffective of 45.99 %. The comparatively higher geo-effectiveness of Sheath II is plausibly due to increased solar wind pressure. Boudouridis et al. (2005) have shown that southward IMF conditions combined with increased high solar wind pressure lead to enhanced coupling between the solar wind and the terrestrial magnetosphere which significantly increases the geo-effectiveness of the solar wind. Furthermore, the non-geo-effectiveness of Sheath I is plausibly a result of the fact that the period of the spatiotemporal location of Sheath I when the solar wind pressure was high the stations along 96–145oE meridian lines were on the dayside. And the increased solar wind dynamic pressure during the spatiotemporal location of Sheath II possibly contributed to the observed polarity differences with the magnetic cloud producing interhemispheric positive storms, and Sheath II producing negative interhemispheric negative storms.
期刊介绍:
The COSPAR publication Advances in Space Research (ASR) is an open journal covering all areas of space research including: space studies of the Earth''s surface, meteorology, climate, the Earth-Moon system, planets and small bodies of the solar system, upper atmospheres, ionospheres and magnetospheres of the Earth and planets including reference atmospheres, space plasmas in the solar system, astrophysics from space, materials sciences in space, fundamental physics in space, space debris, space weather, Earth observations of space phenomena, etc.
NB: Please note that manuscripts related to life sciences as related to space are no more accepted for submission to Advances in Space Research. Such manuscripts should now be submitted to the new COSPAR Journal Life Sciences in Space Research (LSSR).
All submissions are reviewed by two scientists in the field. COSPAR is an interdisciplinary scientific organization concerned with the progress of space research on an international scale. Operating under the rules of ICSU, COSPAR ignores political considerations and considers all questions solely from the scientific viewpoint.