Other
Scientific paper
Dec 2004
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004agufmsm22a..02w&link_type=abstract
American Geophysical Union, Fall Meeting 2004, abstract #SM22A-02
Other
7871 Waves And Instabilities, 7894 Instruments And Techniques, 7899 General Or Miscellaneous, 6964 Radio Wave Propagation, 6984 Waves In Plasma
Scientific paper
Whistler-like events between 60 to 100 Hz have been detected in the ELF station operated by NCKU-ISUAL team at the Lulin Observatory, Taiwan (120o52'E, 23o28' N, 2862m high) from August 20, 2003 to July 29, 2004. The most distinguished feature is the frequency descent in the frequency-time spectrograms, resembling terrestrial whistlers. Other features of the ELF events include(a) a long event duration up to 2 minutes, (b) a daytime diurnal maximum occurring around 10 am, (c) a dominant magnetic field polarization in the north-south direction with strength at a few to tens of pT, and (d) no detection of vertical electric fields...etc. For the past 20 years, similar events were only reported twice, one at the auroral latitude (Heacock, 1974) and the other at the mid-latitude (Sentman and Ehring, 1994). Possible source mechanisms have been discussed are (a) magenetosheath lion roars propagating along the TEM-mode waveguide in the earth-ionosphere cavity, and (b) hiss detected in the equator. Lightning-generated whistlers are not favored in previous studies because of being unable to interpret the observed long dispersions with the electron density environment but all the mechanisms remain open questions. References Heacock, R.R., Whistler-like pulsation events in the frequency range 20-200Hz, Geophys. Res. Lett., 2, 77, 1974. Sentman, D. D., D. A. Ehring, Midlatitude detection of ELF whistlers. J. Geophys. Res., 99, 2183, 1994.
Hsu Rue-Ron
Lee Lillian
Su Haibin
Wang Kai
Wang Yadong
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