TY - JOUR
T1 - Substructures with luminosity modulation and horizontal oscillation in pulsating patch
T2 - Principal component analysis application to pulsating aurora
AU - Nishiyama, Takanori
AU - Miyoshi, Yoshizumi
AU - Katoh, Yuto
AU - Sakanoi, Takeshi
AU - Kataoka, Ryuho
AU - Okano, Shoichi
N1 - Funding Information:
We thank Dr. Donald L. Hampton, B. Lawson, K. Abnett, and all the staff of the Poker Flat Research Range for their helpful support during the observations. A. Otomo has supported us when we were making our ground-based observations at the Poker Flat Research Range in 2011-2012, and the authors appreciate her cooperation in this study. This work was carried out with funding from Grants-in-Aid for Japan Society for the Promotion of Science (JSPS) Fellows (K1232151) and Grants-in-Aid for Scientific Research (25302006, 15H05815, and 15H05747) from the Ministry of Education, Science, Sports, Technology, and Culture of Japan. This study was also supported by the joint research program of the Institute for Space-Earth Environmental Research, Nagoya University and the Global COE program Global Education and Research Center for Earth and Planetary Dynamics of Tohoku University. The production of this paper was supported by an NIPRpublication subsidy. The IMF and solar wind data were obtained from the GSFC/SPDF OMNIWeb interface at http://omniweb.gsfc.nasa.gov/. The Dst and AE indices were provided by the World Data Center for Geomagnetism (WDC-C2) at Kyoto University. Ground-based magnetometer data were provided by the Geophysical Institute Magnetometer Array operated by the Geophysical Institute, University of Alaska, and they are available through the open data repository at UC Berkeley at http://themis.ssl.Berkeley.edu/ index.shtml. Aurora data were obtained from the EMCCD camera, all-sky camera, and photometer at the Poker Flat Research Range and are stored at the following address: http://polaris.nipr.ac.jp/?nishiyama/ tmp/PFRR/.
Publisher Copyright:
©2016. American Geophysical Union. All Rights Reserved.
PY - 2016/3/1
Y1 - 2016/3/1
N2 - We observed a mesoscale aurora (100 km × 100 km) with patchy structure and equatorward propagation at Poker Flat Research Range on 1 December 2011. Fast Fourier transform (FFT) analysis revealed that this pulsating patch clearly exhibited temporal variations that can be categorized into two types: on-off pulsation (7.8-10 s) with large amplitudes and luminosity modulations excited during on phase with a frequency of about 3.0 Hz. In addition, we applied principal component analysis (PCA) to time series image data of the pulsating aurora for the first time. Time coefficients were estimated by PCA for the whole patch and the substructures were consistent with those obtained from the FFT analysis, and therefore, we concluded that PCA is capable of decomposing several structures that have different coherent spatiotemporal characteristics. Another new insight in this study is that the rapid variations were highly localized; they were excited in only the substructures embedded in the whole structure. Moreover, the whole patch propagated equatorward because of E × B drift of cold plasma, while the substructures did not show such systematic propagation but rather forward-backward oscillations. The horizontal scale of the substructures was estimated to be no smaller than 410 km at the magnetic equator, which is comparable to that of the wave packet structure of a whistler mode chorus perpendicular to the field line. We suggest that the apparent horizontal oscillation of the substructures is associated with field-aligned propagations of the whistler mode chorus in a duct.
AB - We observed a mesoscale aurora (100 km × 100 km) with patchy structure and equatorward propagation at Poker Flat Research Range on 1 December 2011. Fast Fourier transform (FFT) analysis revealed that this pulsating patch clearly exhibited temporal variations that can be categorized into two types: on-off pulsation (7.8-10 s) with large amplitudes and luminosity modulations excited during on phase with a frequency of about 3.0 Hz. In addition, we applied principal component analysis (PCA) to time series image data of the pulsating aurora for the first time. Time coefficients were estimated by PCA for the whole patch and the substructures were consistent with those obtained from the FFT analysis, and therefore, we concluded that PCA is capable of decomposing several structures that have different coherent spatiotemporal characteristics. Another new insight in this study is that the rapid variations were highly localized; they were excited in only the substructures embedded in the whole structure. Moreover, the whole patch propagated equatorward because of E × B drift of cold plasma, while the substructures did not show such systematic propagation but rather forward-backward oscillations. The horizontal scale of the substructures was estimated to be no smaller than 410 km at the magnetic equator, which is comparable to that of the wave packet structure of a whistler mode chorus perpendicular to the field line. We suggest that the apparent horizontal oscillation of the substructures is associated with field-aligned propagations of the whistler mode chorus in a duct.
KW - ground-based observations
KW - pulsating aurora
KW - small-scale aurora
KW - wave-particle interactions
KW - whistler mode chorus
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U2 - 10.1002/2015JA022288
DO - 10.1002/2015JA022288
M3 - Article
AN - SCOPUS:84961572721
SN - 2169-9380
VL - 121
SP - 2360
EP - 2373
JO - Journal of Geophysical Research: Space Physics
JF - Journal of Geophysical Research: Space Physics
IS - 3
ER -