Variation and modeling of ultraviolet auroral oval boundaries associated with interplanetary and geomagnetic parameters
Variation and modeling of ultraviolet auroral oval boundaries associated with interplanetary and geomagnetic parameters
复制标题
与行星际和地磁参数相关的紫外线极光椭圆边界的变化和建模
DOI:
10.1002/2016sw001530
复制
发表时间:
2017-04
期刊:
影响因子:
--
通讯作者:
Yang Hui-Gen
中科院分区:
文献类型:
--
作者:
Hu Ze-Jun;Yang Qiu-Ju;Liang Ji-Min;Hu Hong-Qiao;Zhang Bei-Chen;Yang Hui-Gen
A large data set of auroral poleward/equatorward boundary, which are automatically identified from more than 60,000 images acquired by Polar ultraviolet imager, is used to study the variation of auroral boundaries associated with the interplanetary/geomagnetic environments and dynamic parameters of the magnetosphere. A total number of 3,805,000/1,215,000 points for poleward/equatorward boundary were identified from the data set. It is found that the poleward/equatorward boundaries show an equatorward movement with the increase of Kan‐Lee electric field. The poleward/equatorward boundaries in the nightside sector (1800–0600 magnetic local time (MLT)) show an equatorward motion with the increase of the value of IMF By and the north‐south electric field. The equatorward boundary (1800–0300 MLT) shows a quasi‐linear equatorward displacement with the increase of solar wind dynamic pressure and speed. The poleward boundary (excluding midday sector) and equatorward boundary expand equatorward with the increase of AE index. The auroral oval boundary model with input parameters of the three components of IMF, solar wind speed and density, and AE is developed by using multivariate regression method. Evaluation of the model shows that the mean absolute deviation of the model in every MLT sector is 1.3–2.1° magnetic latitude (MLAT) for the poleward boundary and 1.3–2.5° MLAT for the equatorward boundary, respectively, when input parameters are within valid value coverage (three components of IMF are each from −8 to +8 nT, and the values of solar wind speed and density, and AE are not more than 550 km/s, 20/cm−3, and 520 nT, respectively).
登录
查看更多内容
影响因子:
--
作者:
P. Newell;T. Sotirelis;K. Liou;C. Meng;F. Rich
通讯作者:
P. Newell;T. Sotirelis;K. Liou;C. Meng;F. Rich
影响因子:
--
作者:
M. Brittnacher;M. Fillingim;G. Parks;J. Spann
通讯作者:
M. Brittnacher;M. Fillingim;G. Parks;J. Spann
影响因子:
1.9
作者:
P. Boakes;S. Milan;G. Abel;M. Freeman;G. Chisham;B. Hubert;T. Sotirelis
通讯作者:
P. Boakes;S. Milan;G. Abel;M. Freeman;G. Chisham;B. Hubert;T. Sotirelis
影响因子:
2.8
作者:
Yang, Y. F.;Lu, J. Y.;Wang, J. -S.;Peng, Z.;Zhou, L.
通讯作者:
Zhou, L.
影响因子:
--
作者:
D. Hardy;W. J. Burke;M. Gussenhoven;N. Heinemann;E. Holeman
通讯作者:
D. Hardy;W. J. Burke;M. Gussenhoven;N. Heinemann;E. Holeman