ÿþAuxiliary Material for Paper 2012gl053168
A high-resolution model of field-aligned currents through empirical orthogonal
functions analysis (MFACE)
Maosheng He and Joachim Vogt
School of Engineering and Science, Jacobs University Bremen,
Bremen, Germany
Hermann Luhr
Deutsches GeoForschungsZentrum Potsdam,
Potsdam, Germany
Eugen Sorbalo
School of Engineering and Science, Jacobs University Bremen,
Bremen, Germany
Adrian Blagau
School of Engineering and Science, Jacobs University Bremen,
Bremen, Germany
Institute for Space Sciences,
Bucharest-Magurele, Romania
Guan Le
Heliophysics Science Division, NASA Goddard Space Flight Center,
Greenbelt, Maryland, USA
Gang Lu
High Altitude Observatory, NCAR,
Boulder, Colorado, USA
He, M., J. Vogt, H. Luhr, E. Sorbalo, A. Blagau, G. Le, and G. Lu (2012), A
high-resolution model of field-aligned currents through empirical orthogonal
functions analysis (MFACE), Geophys. Res. Lett., 39, L18105,
doi:10.1029/2012GL053168.
Introduction
This electronic supplement contains tables of MFACE coefficients for both
the Northern and Southern hemisphere, and an additional figure presenting
polar distributions of FACs at March Equinox. To unify the driving
condition, MFACE is built with 30 minutes lag to solar winds driving,
despite the FAC density (~20 minutes) responds quicker than FAC latitude
dependence (~35-40 minutes) as indicated by Figure 2b.
The current density jz (in units of mu Am-2) in the direction of
geomagnetic field could be calculated through the following steps, for a
given driving set of Geomagnetic Latitude (MLat), Geomagnetic Local Time
(MLT), Day of Year (DoY), IMF clock angle ¸IMF in GSM, IMF component in
GSM y-z plane Bt (in units of nT), IMF magnitude B (in units of nT),
solar wind speed (in units of km/s) and AE index,.
1) Determination of latitude of Auroral Current Centre (ACC) MLatACC and
the score sj,
MLatACC=Sigma_alpha_ACC*termAi*termBi
sj=Sigma_alpha_sj*termAi*termBi, j=1,2,...,12
Here, termAi and termBi are functions of . The specific functions are
given in the first and second columns of the table contained in Tables S1
and S3. alpha's are coefficients presented in Tables S2 and S4.
2) Calculation of jmean(dMLat) and EOFi(dMLat) through the discrete
functions listed in Tables S1 and S3. Here, dMLat is the latitude with
respect to the reference point of ACC, dMLat=MLat-MLatACC.
EOFs are basis functions determined from the profiles in such a way that
the EOF1 accounts for the largest possible variance, and each succeeding
EOF in turn accounts for maximum variance possible under the constraint
that it be orthogonal to the preceding EOFs. Only the first twelve EOFs
are provided here, since they are the least set that accounts for more
than 95% variance.
3) Estimation of current density,
jz=jmean+Sigma_si*EOFi
Users could cut off the model at lower order than 12, because the
variance captured by the regression decreases rapidly with EOF order, as
shown in Figure 2a.
1. 2012gl053168-ts01.xls
Table S1. EOFs for the Northern Hemisphere.
1.1 Column "dMLat", the latitude with respect to Auroral Current Centre.
1.2 Column "jmean", average FAC density of all profiles.
1.3 Columns "EOF1" ,...,"EOF12", the first twelve EOFs.
2. 2012gl053168-ts02.xls
Table S2. Coefficients for the Northern Hemisphere.
2.1 Column "termA", the first factor termAi .
2.2 Column "termB", the second factor termBi.
2.3 Column "MLat_ACC", alpha_ACC, coefficients for MLatACC.
2.4 Columns "s_1" ,..., "s_j",..., "s_12",
alpha_s1,...,alpha_sj,...,alpha_s12, coefficients for s1,...,sj,..., s12.
3. 2012gl053168-ts03.xls
Table S3. Same as Table S1 but for the Southern Hemisphere.
4. 2012gl053168-ts04.xls
Table S4. Same as Table S2 but for the Southern Hemisphere.
5. 2012gl053168-fs01.pdf
Figure S1. Polar distribution of FACs at March Equinox for Northern
(left) and Southern (right) Hemispheres, arranged by IMF clock angle. Bt
equals 5nT for all patterns except equals 0nT for the central plots for
each hemisphere. In each panel, numbers in corners show the maximum
density (bottom corners, in units of mu Am-2) and hemispherical integrated
density (top corners, in units of MA), for both the downward (right
corners) and the upward current (left corners). Maximum upward and
downward current peaks are marked by crosses.