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A superposed epoch analysis of auroral evolution during substorms: local time of onset region

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A superposed epoch analysis of auroral evolution during substorms: local time of onset region. / Milan, S. E.; Grocott, A.; Hubert, B.
In: Journal of Geophysical Research, Vol. 115, No. A5, A00I04, 14.10.2010.

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Milan, S. E., Grocott, A., & Hubert, B. (2010). A superposed epoch analysis of auroral evolution during substorms: local time of onset region. Journal of Geophysical Research, 115(A5), Article A00I04. https://doi.org/10.1029/2010JA015663

Vancouver

Milan SE, Grocott A, Hubert B. A superposed epoch analysis of auroral evolution during substorms: local time of onset region. Journal of Geophysical Research. 2010 Oct 14;115(A5):A00I04. doi: 10.1029/2010JA015663

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Milan, S. E. ; Grocott, A. ; Hubert, B. / A superposed epoch analysis of auroral evolution during substorms : local time of onset region. In: Journal of Geophysical Research. 2010 ; Vol. 115, No. A5.

Bibtex

@article{41eda7d790aa47608ef2685096cafda4,
title = "A superposed epoch analysis of auroral evolution during substorms: local time of onset region",
abstract = "Previous workers have shown that the magnetic local time (MLT) of substorm onset depends on the prevailing east-west component of the interplanetary magnetic field (IMF). To investigate the influence of the onset MLT on the subsequent auroral response we perform a superposed epoch analysis of the auroral evolution during approximately 2000 substorms using observations from the FUV instrument on the Imager for Magnetopause-to-Aurora Global Exploration (IMAGE) spacecraft. We subdivide the substorms by onset latitude and onset local time before determining average auroral images before and after substorm onset, for both electron and proton aurorae. We find that during the growth phase there is preexisting auroral emission in the MLT sector of the subsequent onset. After onset the auroral bulge expands eastward and westward, but remains centered on the onset sector. Approximately 30 min after onset, during the substorm recovery phase, the peaks in electron and proton auroral emission move into the postnoon and prenoon sectors, respectively, reflecting the “average” auroral precipitation patterns determined by previous studies. Superposed epoch analysis of the interplanetary magnetic field for the substorms under study suggests that the BY component of the IMF must be biased toward positive or negative values for up to a day prior to onset for the onset MLT to be influenced.",
keywords = "substorms, aurora",
author = "Milan, {S. E.} and A. Grocott and B. Hubert",
note = "Copyright 2010 by the American Geophysical Union.",
year = "2010",
month = oct,
day = "14",
doi = "10.1029/2010JA015663",
language = "English",
volume = "115",
journal = "Journal of Geophysical Research",
issn = "0148-0227",
publisher = "American Geophysical Union",
number = "A5",

}

RIS

TY - JOUR

T1 - A superposed epoch analysis of auroral evolution during substorms

T2 - local time of onset region

AU - Milan, S. E.

AU - Grocott, A.

AU - Hubert, B.

N1 - Copyright 2010 by the American Geophysical Union.

PY - 2010/10/14

Y1 - 2010/10/14

N2 - Previous workers have shown that the magnetic local time (MLT) of substorm onset depends on the prevailing east-west component of the interplanetary magnetic field (IMF). To investigate the influence of the onset MLT on the subsequent auroral response we perform a superposed epoch analysis of the auroral evolution during approximately 2000 substorms using observations from the FUV instrument on the Imager for Magnetopause-to-Aurora Global Exploration (IMAGE) spacecraft. We subdivide the substorms by onset latitude and onset local time before determining average auroral images before and after substorm onset, for both electron and proton aurorae. We find that during the growth phase there is preexisting auroral emission in the MLT sector of the subsequent onset. After onset the auroral bulge expands eastward and westward, but remains centered on the onset sector. Approximately 30 min after onset, during the substorm recovery phase, the peaks in electron and proton auroral emission move into the postnoon and prenoon sectors, respectively, reflecting the “average” auroral precipitation patterns determined by previous studies. Superposed epoch analysis of the interplanetary magnetic field for the substorms under study suggests that the BY component of the IMF must be biased toward positive or negative values for up to a day prior to onset for the onset MLT to be influenced.

AB - Previous workers have shown that the magnetic local time (MLT) of substorm onset depends on the prevailing east-west component of the interplanetary magnetic field (IMF). To investigate the influence of the onset MLT on the subsequent auroral response we perform a superposed epoch analysis of the auroral evolution during approximately 2000 substorms using observations from the FUV instrument on the Imager for Magnetopause-to-Aurora Global Exploration (IMAGE) spacecraft. We subdivide the substorms by onset latitude and onset local time before determining average auroral images before and after substorm onset, for both electron and proton aurorae. We find that during the growth phase there is preexisting auroral emission in the MLT sector of the subsequent onset. After onset the auroral bulge expands eastward and westward, but remains centered on the onset sector. Approximately 30 min after onset, during the substorm recovery phase, the peaks in electron and proton auroral emission move into the postnoon and prenoon sectors, respectively, reflecting the “average” auroral precipitation patterns determined by previous studies. Superposed epoch analysis of the interplanetary magnetic field for the substorms under study suggests that the BY component of the IMF must be biased toward positive or negative values for up to a day prior to onset for the onset MLT to be influenced.

KW - substorms

KW - aurora

U2 - 10.1029/2010JA015663

DO - 10.1029/2010JA015663

M3 - Journal article

VL - 115

JO - Journal of Geophysical Research

JF - Journal of Geophysical Research

SN - 0148-0227

IS - A5

M1 - A00I04

ER -