Learmonth - Type III bursts
             Daily summary
from 20110327 2239 to 20110328 1024  (YYYYMMDD hhmm UT)
 
   date     start-end time  # of bursts
(YYYYMMDD)     (hhmm UT)
  20110327    2325 - 2325          1
  20110327    2341 - 2342          2
  20110328    0022 - 0023          3
  20110328    0029 - 0030          3
  20110328    0037 - 0037          2
  20110328    0050 - 0050          1
  20110328    0120 - 0122          6
  20110328    0129 - 0129          1
  20110328    0240 - 0240          1
  20110328    0305 - 0305          2
  20110328    0319 - 0319          1
  20110328    0344 - 0349          15
  20110328    0355 - 0355          2
  20110328    0401 - 0401          1
  20110328    0404 - 0404          1
  20110328    0427 - 0427          1
  20110328    0431 - 0431          1
  20110328    0434 - 0435          3
  20110328    0443 - 0443          1
  20110328    0446 - 0447          2
  20110328    0601 - 0602          2
  20110328    0612 - 0613          3
  20110328    0619 - 0621          7
  20110328    0624 - 0624          1
  20110328    0627 - 0627          2
  20110328    0807 - 0807          1
  20110328    0831 - 0832          2
 
 
The results are preliminary.
Type-III-like signals can be produced by local lightnings
and/or machinery interference.
 
 
        Culgoora - Type III bursts
             Daily summary
from 20110327 2000 to 20110328 0760  (YYYYMMDD hhmm UT)
 
   date     start-end time  # of bursts
(YYYYMMDD)     (hhmm UT)
  20110327    2225 - 2225          1
  20110328    0022 - 0023          3
  20110328    0029 - 0031          4
  20110328    0119 - 0119          1
  20110328    0121 - 0121          3
  20110328    0126 - 0126          1
  20110328    0305 - 0305          1
  20110328    0347 - 0348          3
  20110328    0355 - 0355          2
  20110328    0404 - 0404          1
  20110328    0446 - 0446          1
  20110328    0602 - 0602          1
  20110328    0613 - 0613          1
  20110328    0619 - 0620          3
  20110328    0639 - 0639          1
 
 
The results are preliminary.
Type-III-like signals can be produced by local lightnings
and/or machinery interference.