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A quantitative deconstruction of the morphology of high-latitude ionospheric convection

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A quantitative deconstruction of the morphology of high-latitude ionospheric convection. / Grocott, A.; Milan, S. E.; Imber, S. M. et al.
In: Journal of Geophysical Research, Vol. 117, No. A5, 05317, 17.05.2012.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Grocott, A, Milan, SE, Imber, SM, Lester, M & Yeoman, TK 2012, 'A quantitative deconstruction of the morphology of high-latitude ionospheric convection', Journal of Geophysical Research, vol. 117, no. A5, 05317. https://doi.org/10.1029/2012JA017580

APA

Grocott, A., Milan, S. E., Imber, S. M., Lester, M., & Yeoman, T. K. (2012). A quantitative deconstruction of the morphology of high-latitude ionospheric convection. Journal of Geophysical Research, 117(A5), Article 05317. https://doi.org/10.1029/2012JA017580

Vancouver

Grocott A, Milan SE, Imber SM, Lester M, Yeoman TK. A quantitative deconstruction of the morphology of high-latitude ionospheric convection. Journal of Geophysical Research. 2012 May 17;117(A5):05317. doi: 10.1029/2012JA017580

Author

Grocott, A. ; Milan, S. E. ; Imber, S. M. et al. / A quantitative deconstruction of the morphology of high-latitude ionospheric convection. In: Journal of Geophysical Research. 2012 ; Vol. 117, No. A5.

Bibtex

@article{fbf26069f31c458b8ff06cd8ac8af75d,
title = "A quantitative deconstruction of the morphology of high-latitude ionospheric convection",
abstract = "We present an analysis of ionospheric convection data derived from velocity measurements made by the Super Dual Auroral Radar Network (SuperDARN). Our analysis uses an established technique for combining the network data to produce maps of large-scale convection by fitting a spherical harmonic expansion of the ionospheric electric potential to the radar measurements. We discuss how the basis functions of the spherical harmonic expansion describe different characteristic elements of the ionospheric convection pattern and show how their associated coefficients can be used to quantify the morphology of the convection, much like the total transpolar voltage is used to quantify its strength, in relation to upstream interplanetary magnetic field conditions and associated magnetospheric activity. We find that similar to 2/3 of the voltage associated with the typical convection pattern is described by a simple twin vortex basis function. The magnitude of the twin vortex is strongly dependent on IMF B-Z and the degree of its (typically westward) rotation is weakly dependent on IMF B-Y. The remaining similar to 1/3 of the total voltage is associated with deviations from the basic twin vortex pattern, introduced by the addition of other basis functions, such as IMF B-Y associated dusk-dawn asymmetries, nightside convection features associated with tail activity, and {"}reverse{"} high-latitude convection cells associated with intervals of IMF B-Z > 0.",
keywords = "INTERPLANETARY MAGNETIC-FIELD, DUAL LOBE RECONNECTION, HF RADAR OBSERVATIONS, STATISTICAL PATTERNS, SUPERDARN, SIGNATURES, TIME, FLOW, IMF",
author = "A. Grocott and Milan, {S. E.} and Imber, {S. M.} and M. Lester and Yeoman, {T. K.}",
note = "Copyright 2012 by the American Geophysical Union",
year = "2012",
month = may,
day = "17",
doi = "10.1029/2012JA017580",
language = "English",
volume = "117",
journal = "Journal of Geophysical Research",
issn = "0148-0227",
publisher = "American Geophysical Union",
number = "A5",

}

RIS

TY - JOUR

T1 - A quantitative deconstruction of the morphology of high-latitude ionospheric convection

AU - Grocott, A.

AU - Milan, S. E.

AU - Imber, S. M.

AU - Lester, M.

AU - Yeoman, T. K.

N1 - Copyright 2012 by the American Geophysical Union

PY - 2012/5/17

Y1 - 2012/5/17

N2 - We present an analysis of ionospheric convection data derived from velocity measurements made by the Super Dual Auroral Radar Network (SuperDARN). Our analysis uses an established technique for combining the network data to produce maps of large-scale convection by fitting a spherical harmonic expansion of the ionospheric electric potential to the radar measurements. We discuss how the basis functions of the spherical harmonic expansion describe different characteristic elements of the ionospheric convection pattern and show how their associated coefficients can be used to quantify the morphology of the convection, much like the total transpolar voltage is used to quantify its strength, in relation to upstream interplanetary magnetic field conditions and associated magnetospheric activity. We find that similar to 2/3 of the voltage associated with the typical convection pattern is described by a simple twin vortex basis function. The magnitude of the twin vortex is strongly dependent on IMF B-Z and the degree of its (typically westward) rotation is weakly dependent on IMF B-Y. The remaining similar to 1/3 of the total voltage is associated with deviations from the basic twin vortex pattern, introduced by the addition of other basis functions, such as IMF B-Y associated dusk-dawn asymmetries, nightside convection features associated with tail activity, and "reverse" high-latitude convection cells associated with intervals of IMF B-Z > 0.

AB - We present an analysis of ionospheric convection data derived from velocity measurements made by the Super Dual Auroral Radar Network (SuperDARN). Our analysis uses an established technique for combining the network data to produce maps of large-scale convection by fitting a spherical harmonic expansion of the ionospheric electric potential to the radar measurements. We discuss how the basis functions of the spherical harmonic expansion describe different characteristic elements of the ionospheric convection pattern and show how their associated coefficients can be used to quantify the morphology of the convection, much like the total transpolar voltage is used to quantify its strength, in relation to upstream interplanetary magnetic field conditions and associated magnetospheric activity. We find that similar to 2/3 of the voltage associated with the typical convection pattern is described by a simple twin vortex basis function. The magnitude of the twin vortex is strongly dependent on IMF B-Z and the degree of its (typically westward) rotation is weakly dependent on IMF B-Y. The remaining similar to 1/3 of the total voltage is associated with deviations from the basic twin vortex pattern, introduced by the addition of other basis functions, such as IMF B-Y associated dusk-dawn asymmetries, nightside convection features associated with tail activity, and "reverse" high-latitude convection cells associated with intervals of IMF B-Z > 0.

KW - INTERPLANETARY MAGNETIC-FIELD

KW - DUAL LOBE RECONNECTION

KW - HF RADAR OBSERVATIONS

KW - STATISTICAL PATTERNS

KW - SUPERDARN

KW - SIGNATURES

KW - TIME

KW - FLOW

KW - IMF

U2 - 10.1029/2012JA017580

DO - 10.1029/2012JA017580

M3 - Journal article

VL - 117

JO - Journal of Geophysical Research

JF - Journal of Geophysical Research

SN - 0148-0227

IS - A5

M1 - 05317

ER -