130 3101 840 1950 2006 1228 1200 0 2006 1228 2300 0 16 5 4 0 0 0 0 0 KRECH 2 3101 Header record, version 1. KINST 3 840 JULIA, Jicamarca, Lima, Peru KINDAT 4 1950 KINDAT definition below IBYRE 5 2006 Beginning year IBDTE 6 1228 Beginning month and day IBHME 7 1200 Beginning UT hour, min. IBCSE 8 0 Beginning centisecond IEYRE 9 2006 Ending year IEDTE 10 1228 Ending month and day IEHME 11 2300 Ending UT hour, min. IECSE 12 0 Ending centisecond LPROL 13 16 Length of prologue in accompanying data JPAR 14 5 Number of single-valued parameters MPAR 15 4 Number of multiple-valued parameters NROW 16 1 Number of entries for each multiple-valued entry C NROW may vary from the above in data records C KODS contains the single-valued parameters. KODS( 1) 17 153 Reference geod latitude (N hemi=pos) 1.E-02 deg KODS( 2) 18 156 Reference geodetic longitude 1.E-02 deg KODS( 3) 19 60 Integration time for these data 1.E+00 s KODS( 4) 20 110 Altitude (height) 1.E+00 km KODS( 5) 21 -110 Error in altitude (height) 1.E+00 km C KODM contains the multiple-valued parameters. KODM( 1) 26 1252 Direction 5 Ion velocity (perp north) 1.E-02 m/s KODM( 2) 27 -1252 Error parameter in 1252 1.E-02 m/s KODM( 3) 28 1241 Direction 4 Ion velocity (perp east) 1.E-01 m/s KODM( 4) 29 -1241 Error parameter in 1241 1.E-01 m/s C Missing parameters are assigned a value -32767 C Parameters which overflow the given format are assigned a value 32767 C.............................................................................. CKINDAT=1950 for the F-region ExB, perp N(upward and perp E, ion drifts C from the 150-km echoes measured by the 50 MHz JULIA radar C.............................................................................. C C These data are proxy measurements of F-region ExB ion drifts derived from C the 150-km echoes measured with the Jicamarca (11.95 S, 76.87 W; 520 m alt) C Unattended Long-Term studies of the Ionosphere and Atmosphere (JULIA) C system. On day 359 of 2001 at the ground, the apex magnetic lat,lon were C (0.58,-5.12) deg. The magnetic inclination and declination angles were C 1.145 deg and 0.367 deg. The magnetic local time at 0 UT is ~1835 MLT. C C Jicamarca is the site of a 50 MHz incoherent scatter radar (ISR, kinst=10) C in operation since the 1960s. The JULIA system is a coherent scatter radar C (kinst=840) that uses two low-power 50 MHz transmitters which are phased C together to excite the transmission antennas as a single unit. The JULIA C system was intended for uninterrupted observations of ionospheric and C atmospheric irregularities. JULIA shares the antenna, receiving system, C processing, etc. with the ISR, but uses different transmitters. The C coherent and incoherent scatter radar transmitters can operate at the same C time for intercomparisons (e.g. Chau and Woodman, 2004]. C C The JULIA data are divided into 3 categories based on their altitude range C and local time of occurrance. Observations of the E region electrojet (EEJ) C are made between altitudes of 85 and 140 km in the morning and evening. The C equatorial spread F (ESF) region irregularities are sampled between 95 and C more than 850 km at night. For the valley region and so-called "150 kilo- C meter" echoes, altitudes bewtween 130 and 180 km are sampled during the day. C The present 150-km echoes are averages between 140 and 170 km. C C JULIA ionospheric irregularity data have been collected beginning in August C 1996. Signal-to-noise ratios are shown as intensities. Horizontal zonal C drifts are deduced with radar intererometry. Vertical drifts refer to C Doppler phase speeds where positive values imply upward phase propagation C in the EEJ and ESF modes. C C Echoes from 150-km irregularities were first observed in the early 1960's C over Jicamarca using the ISR [Balsley, 1964]. The echoes are called C 150-km because they are observed between the altitudes of 140 and 170 km. C These echoes occurr only during the daytime and show very little seasonal C dependence. The 150-km echoes have been observed at Jicamarca with the ISR C on a campaign basis [e. g., Kudeki and Fawcett, 1993]. Sucessful low power C observations of 150-km echoes have been performed since 2001 with the JULIA C radar using two different antenna beam configurations (a single vertical C beam, and an east-west beam pair). Using the vertical beam, only the C vertical ion Doppler velocities are obtained, while using the east-west C beam position both the vertical and zonal ion velocities are measured. In C the latter case, two beams are used at the same time using diffent antenna C sections. C C An important finding from the study of these 150-km echoes is that the C daytime vertical Doppler velocities of the 150-km irregularities averaged C over the altitudinal region of the irregularities were in excellent C agreement with the mean F region (200-500 km) ISR vertical drifts [Chau and C Woodman, 2004]. Vertical is perpendicular north at the magnetic equator C where the B field is horizontally directed from the south to the north. C The zonal ion Doppler velocities from the east-west JULIA beam are in C reasonable agreement with the ISR zonal ion velocities. Although 150-km C echoes have been observed and studied for many years, the physical C mechanism which causes them is still unknown. This JULIA database of C representative zonal and vertical (perpendicular north) ion drifts could C contribute in providing very precise proxy measurements of F region drifts C using less powerful and more economical radar. C C For more information, consult the following references: C C Balsley, B. B. (1964), Evidence of a stratified echoing region at 150 C kilometers in the vecinity of the magnetic equator during daylight hours, C J. Geophys. Res. Lett., 24, 2941-2944. C Chau, J. L. and R. F. Woodman, (2004), Daytime vertical and zonal velocities C from 150-km echoes: Their relevance to F-region dynamics, Geophys. Res. C Lett., 31, doi:10.1029/2004GL020800. C Kudeki, E. and C. D. Fawcett, (1993), High resolution observations of 150 Km C echoes at Jicamarca, Geophys. Res. Lett., 20, 1987-1990. C C.............................................................................. C ACKNOWLEDGEMENTS: C The Jicamarca Radio Observatory is a facility of the Instituto C Geofisico del Peru operated with support from the NSF Cooperative C Agreement ATM-0432565 through Cornell University. C.............................................................................. C Further questions and comments should be addressed to: C C Jorge L. Chau C Radio Observatorio de Jicamarca C Instituto Geofisico del Peru C Apartado 13-0207 C Lima, Peru C Phone: (51)-1-3172313 Fax: (51)-1-3172312 C E-mail: jchau@jro.igp.gob.pe C CANALYST Henry Pinedo C Radio Observatorio de Jicamarca C Instituto Geofisico del Peru C E-mail: hpinedo@jro.igp.gob.pe C C Web URL: C http://jro.igp.gob.pe C CANDATE Thu May 7 21:45:21 EDT 2009 5 1101 840 1950 2006 1228 1200 0 2006 1228 1205 0 16 5 4 1 153 156 60 110 -110 -1195 -7687 300 155 15 1252 -1252 1241 -1241 -32767-32767-32767-32767 5 1101 840 1950 2006 1228 1205 0 2006 1228 1210 0 16 5 4 1 153 156 60 110 -110 -1195 -7687 300 155 15 1252 -1252 1241 -1241 -32767-32767-32767-32767 5 1101 840 1950 2006 1228 1210 0 2006 1228 1215 0 16 5 4 1 153 156 60 110 -110 -1195 -7687 300 155 15 1252 -1252 1241 -1241 -32767-32767-32767-32767 5 1101 840 1950 2006 1228 1215 0 2006 1228 1220 0 16 5 4 1 153 156 60 110 -110 -1195 -7687 300 155 15 1252 -1252 1241 -1241 -32767-32767-32767-32767 5 1101 840 1950 2006 1228 1220 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