Published March 1986 | Version v1
Journal article

Solar-terrestrial disturbances of June-September 1982, 4

  • 1. Radio Research Lab., Koganei, Tokyo (Japan)

Description

A new 50-MHz Doppler radar with a mini-computer for real-time data processing and radar control was installed at Syowa Station, Antarctica in February 1982. Severe geomagnetic disturbances occurred at about 00 h UT, 14 July 1982. Then the magnetic H component decrease of about 4200 nT was observed at Syowa Station, and that of about 630 nT was observed at Kakioka Magnetic Observatory in the midlatitude. 50-MHz backscatter echoes were received on 13 - 14 July 1982 during a substorm growth phase, so the rough estimates of the Doppler velocity during this period were obtained. In this paper the Doppler spectra are discussed on the following three stages: SSC onset, substorm main phase and recovery phase. On the hypothesis of spatially homogeneous plasma flow, we determined a large-scale electric field by combining the drift velocities along the radar beams. It appeared that the E region electric field was larger than 30 mV/m in the main phase of this substorm. (author)

Additional details

Additional titles

Subtitle (English)
Ionospheric disturbances, 13: aurora observation using the Syowa Station 50-MHz Doppler radar

Publishing Information

Journal Title
J. Radio Res. Lab. (Tokyo)
Journal Volume
33
Journal Issue
special issue no.1
Series
J. Radio Res. Lab. (Tokyo).
Journal Page Range
269-277
ISSN
0033-8001
CODEN
JRRLA

INIS

Country of Publication
Japan
Country of Input or Organization
Japan
INIS RN
18068722
Subject category
S58: GEOSCIENCES;
Resource subtype / Literary indicator
Numerical Data
Descriptors DEI
AURORAE; DOPPLER EFFECT; EXPERIMENTAL DATA; MAGNETIC FIELDS; MAGNETIC STORMS; MEASURING INSTRUMENTS; MEASURING METHODS; MHZ RANGE; RADAR; SPECTRA; SUDDEN IONOSPHERIC DISTURBANCE; VELOCITY
Descriptors DEC
DATA; DISTURBANCES; FREQUENCY RANGE; INFORMATION; IONOSPHERIC STORMS; NUMERICAL DATA; RANGE FINDERS