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  5. Scaling Features of High-Latitude Geomagnetic Field Fluctuations at Swarm Altitude: Impact of IMF Orientation
 
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Scaling Features of High-Latitude Geomagnetic Field Fluctuations at Swarm Altitude: Impact of IMF Orientation

Author(s)
De Michelis, Paola  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia  
Consolini, Giuseppe  
INAF- Istituto di Astrofisica e Planetologia Spaziali  
Tozzi, Roberta  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia  
Marcucci, Maria Federica  
INAF- Istituto di Astrofisica e Planetologia Spaziali  
Language
English
Obiettivo Specifico
1A. Geomagnetismo e Paleomagnetismo
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Journal of Geophysical Research: Space Physics  
Issue/vol(year)
/122 (2017)
Pages (printed)
10548-10562
Date Issued
September 2017
DOI
10.1002/2017JA024156
URI
https://www.earth-prints.org/handle/2122/11695
Subjects
05.07. Space and Planetary sciences  
01.02. Ionosphere  
04.05. Geomagnetism  
Subjects

Turbulence

geomagnetic field

High-latitude

F-region

Abstract
This paper attempts to explore the statistical scaling features of high-latitude geomagnetic
field fluctuations at Swarm altitude. Data for this study are low-resolution (1 Hz) magnetic data recorded by
the vector field magnetometer on board Swarm A satellite over 1 year (from 15 April 2014 to 15 April 2015).
The first- and second-order structure function scaling exponents and the degree of intermittency of the
fluctuations of the intensity of the horizontal component of the magnetic field at high northern latitudes
have been evaluated for different interplanetary magnetic field orientations in the GSM Y-Z plane and
seasons. In the case of the first-order structure function scaling exponent, a comparison between the
average spatial distributions of the obtained values and the statistical convection patterns obtained using
a Super Dual Auroral Radar Network dynamic model (CS10 model) has been also considered. The obtained
results support the idea that the knowledge of the scaling features of the geomagnetic field fluctuations
can help in the characterization of the different ionospheric turbulence regimes of the medium crossed by
Swarm A satellite. This study shows that different turbulent regimes of the geomagnetic field fluctuations
exist in the regions characterized by a double-cell convection pattern and in those regions near the border
of the convective structures.
Type
article
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