Comparing the diurnal variations in the SuperMAG auroral electrojet indices SML and SMU
Diurnal variations of the SuperMAG auroral electrojet indices (SML and SMU) were examined for the period of 1980-2010, and the differences between SML and SMU were especially analyzed. The diurnal variation of SML with a maximum at around 1100 UT has a prenoon- postnoon asymmetry. At solstices, the...
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Published in | Chinese science bulletin Vol. 59; no. 29-30; pp. 3877 - 3883 |
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Main Authors | , , , , , , , |
Format | Journal Article |
Language | English |
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01.10.2014
Science China Press |
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Abstract | Diurnal variations of the SuperMAG auroral electrojet indices (SML and SMU) were examined for the period of 1980-2010, and the differences between SML and SMU were especially analyzed. The diurnal variation of SML with a maximum at around 1100 UT has a prenoon- postnoon asymmetry. At solstices, the diurnal variation of SML is much stronger than that at equinoxes. For the SMU, two maxima are recorded in the diurnal variation with the bigger one at 1700 UT and the smaller one at 0400 UT. The seasonal variations are not obvious in the UT variation characteristics of SMU although the intensity of SMU is changed remarkably season by season. For both SML and SMU, the contributing stations are located at higher geomagnetic latitude around 1600 UT and at lower geomagnetic latitude around 0400 UT. These results indicate that:(1) the SML is mostly controlled by the convection electric field. Its diurnal variation is mainly correlated with the equinoctial and R-M hypothesis; (2) the SMU is largely controlled by the ionospheric conductance. Its diurnal variation is tightly correlated with the solar radiation. |
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AbstractList | Diurnal variations of the SuperMAG auroral electrojet indices (SML and SMU) were examined for the period of 1980–2010, and the differences between SML and SMU were especially analyzed. The diurnal variation of SML with a maximum at around 1100 UT has a prenoon-postnoon asymmetry. At solstices, the diurnal variation of SML is much stronger than that at equinoxes. For the SMU, two maxima are recorded in the diurnal variation with the bigger one at 1700 UT and the smaller one at 0400 UT. The seasonal variations are not obvious in the UT variation characteristics of SMU although the intensity of SMU is changed remarkably season by season. For both SML and SMU, the contributing stations are located at higher geomagnetic latitude around 1600 UT and at lower geomagnetic latitude around 0400 UT. These results indicate that: (1) the SML is mostly controlled by the convection electric field. Its diurnal variation is mainly correlated with the equinoctial and R-M hypothesis; (2) the SMU is largely controlled by the ionospheric conductance. Its diurnal variation is tightly correlated with the solar radiation. Diurnal variations of the SuperMAG auroral electrojet indices (SML and SMU) were examined for the period of 1980-2010, and the differences between SML and SMU were especially analyzed. The diurnal variation of SML with a maximum at around 1100 UT has a prenoon- postnoon asymmetry. At solstices, the diurnal variation of SML is much stronger than that at equinoxes. For the SMU, two maxima are recorded in the diurnal variation with the bigger one at 1700 UT and the smaller one at 0400 UT. The seasonal variations are not obvious in the UT variation characteristics of SMU although the intensity of SMU is changed remarkably season by season. For both SML and SMU, the contributing stations are located at higher geomagnetic latitude around 1600 UT and at lower geomagnetic latitude around 0400 UT. These results indicate that:(1) the SML is mostly controlled by the convection electric field. Its diurnal variation is mainly correlated with the equinoctial and R-M hypothesis; (2) the SMU is largely controlled by the ionospheric conductance. Its diurnal variation is tightly correlated with the solar radiation. Diurnal variations of the SuperMAG auroral electrojet indices ( SML and SMU ) were examined for the period of 1980–2010, and the differences between SML and SMU were especially analyzed. The diurnal variation of SML with a maximum at around 1100 UT has a prenoon-postnoon asymmetry. At solstices, the diurnal variation of SML is much stronger than that at equinoxes. For the SMU , two maxima are recorded in the diurnal variation with the bigger one at 1700 UT and the smaller one at 0400 UT. The seasonal variations are not obvious in the UT variation characteristics of SMU although the intensity of SMU is changed remarkably season by season. For both SML and SMU , the contributing stations are located at higher geomagnetic latitude around 1600 UT and at lower geomagnetic latitude around 0400 UT. These results indicate that: (1) the SML is mostly controlled by the convection electric field. Its diurnal variation is mainly correlated with the equinoctial and R-M hypothesis; (2) the SMU is largely controlled by the ionospheric conductance. Its diurnal variation is tightly correlated with the solar radiation. |
Author | Li, Min Guo, Jianpeng Chen, Gengxiong Wang, Yuan Cao, Xin Zhang, Ying Liu, Xiaocan Du, Aimin |
AuthorAffiliation | Key Laboratory of Ionospheric Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China Beijing National Observatory of Space Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China University of Chinese Academy of Sciences,Beijing 100049, China Institute of Geophysics, China Earthquake Administration,Beijing 100081, China State Key Laboratory of Space Weather, Center for Space Science and Applied Research, Chinese Academy of Sciences, Beijing 100190, China |
Author_xml | – sequence: 1 fullname: Wang, Yuan – sequence: 2 fullname: Du, Aimin – sequence: 3 fullname: Chen, Gengxiong – sequence: 4 fullname: Cao, Xin – sequence: 5 fullname: Zhang, Ying – sequence: 6 fullname: Li, Min – sequence: 7 fullname: Liu, Xiaocan – sequence: 8 fullname: Guo, Jianpeng |
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CitedBy_id | crossref_primary_10_1051_swsc_2020077 crossref_primary_10_1029_2022JA030816 crossref_primary_10_11728_cjss2016_05_672 |
Cites_doi | 10.5303/JKAS.2003.36.spc1.093 10.1029/94JA02725 10.1029/2000GL012803 10.1029/2011JA016718 10.1016/S1364-6826(01)00093-1 10.1186/BF03351757 10.1029/2002JA009257 10.1029/97JA00577 10.1029/RG021i007p01647 10.1029/2011JA016779 10.1029/JA081i025p04546 10.1098/rsta.1959.0010 10.1029/2008JA013284 10.1029/2000JA000358 10.1007/978-94-010-1164-8 10.5194/angeo-28-1167-2010 10.1007/s00585-998-1573-9 10.1029/JA075i031p06073 10.1029/98JA01426 10.1016/j.asr.2012.07.034 10.1029/JZ071i003p00785 10.1029/2000JA000231 10.1038/381766a0 10.1029/2008GL033931 10.1029/JA078i001p00092 10.1029/96JA00142 10.1029/1999JA900439 10.1029/2012JA017845 10.1029/94GL00013-A 10.1029/2001JA000296 10.1029/2011JA016936 10.1093/mnras/73.1.52 10.1029/2002Gl015318 10.1029/1999JA900364 10.1029/2005JA011057 10.1029/2012JA017683 |
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Notes | Diurnal variations of the SuperMAG auroral electrojet indices (SML and SMU) were examined for the period of 1980-2010, and the differences between SML and SMU were especially analyzed. The diurnal variation of SML with a maximum at around 1100 UT has a prenoon- postnoon asymmetry. At solstices, the diurnal variation of SML is much stronger than that at equinoxes. For the SMU, two maxima are recorded in the diurnal variation with the bigger one at 1700 UT and the smaller one at 0400 UT. The seasonal variations are not obvious in the UT variation characteristics of SMU although the intensity of SMU is changed remarkably season by season. For both SML and SMU, the contributing stations are located at higher geomagnetic latitude around 1600 UT and at lower geomagnetic latitude around 0400 UT. These results indicate that:(1) the SML is mostly controlled by the convection electric field. Its diurnal variation is mainly correlated with the equinoctial and R-M hypothesis; (2) the SMU is largely controlled by the ionospheric conductance. Its diurnal variation is tightly correlated with the solar radiation. 11-1785/N Auroral electrojet ; SuperMAG Diurnal variation ; SML index ; SMU index http://dx.doi.org/10.1007/s11434-014-0451-y |
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Snippet | Diurnal variations of the SuperMAG auroral electrojet indices (SML and SMU) were examined for the period of 1980-2010, and the differences between SML and SMU... Diurnal variations of the SuperMAG auroral electrojet indices (SML and SMU) were examined for the period of 1980–2010, and the differences between SML and SMU... Diurnal variations of the SuperMAG auroral electrojet indices ( SML and SMU ) were examined for the period of 1980–2010, and the differences between SML and... |
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SubjectTerms | Chemistry/Food Science diurnal variation Earth Sciences electric field Engineering Humanities and Social Sciences latitude Life Sciences multidisciplinary Physics Science Science (multidisciplinary) seasonal variation SML SMU solar radiation UT变化 季节变化 日变化 昼夜变化 极光 电喷 |
Title | Comparing the diurnal variations in the SuperMAG auroral electrojet indices SML and SMU |
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