Learmonth - Type III bursts Daily summary from 20100211 2220 to 20100212 1101 (YYYYMMDD hhmm UT) date start-end time # of bursts (YYYYMMDD) (hhmm UT) 20100212 0046 - 0047 1 20100212 0049 - 0050 3 20100212 0053 - 0054 4 20100212 0055 - 0056 2 20100212 0112 - 0112 1 20100212 0116 - 0116 1 20100212 0118 - 0118 1 20100212 0211 - 0211 1 20100212 0215 - 0215 2 20100212 0216 - 0216 1 20100212 0402 - 0402 1 20100212 0454 - 0454 1 20100212 0509 - 0509 1 20100212 0546 - 0547 2 20100212 0552 - 0552 1 20100212 0554 - 0556 5 20100212 0606 - 0608 3 20100212 0611 - 0611 1 20100212 0612 - 0613 2 20100212 0632 - 0632 1 20100212 0633 - 0633 1 20100212 0642 - 0643 4 20100212 0645 - 0648 8 20100212 0654 - 0654 1 20100212 0657 - 0657 1 20100212 0713 - 0713 1 20100212 0717 - 0718 2 20100212 0720 - 0726 14 20100212 0735 - 0735 1 20100212 0920 - 0920 2 20100212 0922 - 0922 1 20100212 0937 - 0937 1 20100212 0940 - 0942 10 20100212 0943 - 0943 1 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 20100211 2000 to 20100212 0760 (YYYYMMDD hhmm UT) date start-end time # of bursts (YYYYMMDD) (hhmm UT) 20100211 2106 - 2106 1 20100211 2223 - 2223 1 20100212 0049 - 0050 2 20100212 0053 - 0054 5 20100212 0055 - 0056 2 20100212 0116 - 0116 1 20100212 0118 - 0118 1 20100212 0215 - 0215 1 20100212 0402 - 0402 1 20100212 0454 - 0454 1 20100212 0508 - 0508 1 20100212 0551 - 0552 3 20100212 0554 - 0556 5 20100212 0560 - 0560 1 20100212 0606 - 0608 4 20100212 0611 - 0613 5 20100212 0620 - 0621 2 20100212 0622 - 0622 1 20100212 0627 - 0627 1 20100212 0630 - 0631 3 20100212 0633 - 0634 2 20100212 0635 - 0635 2 20100212 0642 - 0643 3 20100212 0644 - 0644 1 20100212 0645 - 0646 5 20100212 0647 - 0647 1 20100212 0649 - 0650 2 20100212 0654 - 0656 5 20100212 0660 - 0660 2 20100212 0702 - 0702 1 20100212 0715 - 0715 1 20100212 0717 - 0717 1 20100212 0720 - 0720 1 20100212 0721 - 0726 15 20100212 0732 - 0732 1 The results are preliminary. Type-III-like signals can be produced by local lightnings and/or machinery interference.