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 inChinese science bulletin Vol. 59; no. 29-30; pp. 3877 - 3883
Main Authors Wang, Yuan, Du, Aimin, Chen, Gengxiong, Cao, Xin, Zhang, Ying, Li, Min, Liu, Xiaocan, Guo, Jianpeng
Format Journal Article
LanguageEnglish
Published Heidelberg Springer-Verlag 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.
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
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CitedBy_id crossref_primary_10_1051_swsc_2020077
crossref_primary_10_1029_2022JA030816
crossref_primary_10_11728_cjss2016_05_672
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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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fao
chongqing
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StartPage 3877
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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