TITLE: GCN GRB OBSERVATION REPORT NUMBER: 3343 SUBJECT: Renewal of SGR 1806-20 activity DATE: 05/05/03 15:18:35 GMT FROM: Valentin Pal'shin at Ioffe Inst S. Golenetskii, R.Aptekar, E. Mazets, V. Pal'shin, D. Frederiks on behalf of Konus-Wind and Helicon/Coronas-F teams, and T. Cline on behalf of the Konus-Wind team, and A. Rau, A. von Kienlin, G. Lichti on behalf of the INTEGRAL SPI-ACS GRB team report: On May 2 Konus-Wind detected two SGR-like bursts in the trigger mode. The first one triggered Konus-Wind at 5376.421 s UT (01:29:36.421). It was also detected by INTEGRAL SPI-ACS. Because the burst was soft, the SPI-ACS response is very weak, and precise triangulation of this burst is not possible. We conservatively estimated that the time delay was 3.6 +/- 0.4 s which is consistent with the expected time delay for SGR 1806-20 (=3.651 s). Additionaly, the Konus ecliptic latitude response indicates that the burst source is near the ecliptic plane, so we believe that this burst originated from SGR 1806-20. The burst is unusually long with a duration of ~4.5 s, but relatively weak. As observed by Konus-Wind, the burst had a fluence ~2.0x10^-5 erg/cm2, and a peak flux ~6x10^-6 erg/cm2 s (both in 20-200 keV range). The time-integrated spectrum of the burst is well fitted by the OTTB spectral model: dN/dE ~ E^{-1} exp(-E/kT) with kT = 18 +/- 1 keV, which is typical for this SGR. The second burst triggered Konus-Wind at 18502.741 s UT (05:08:22.741). As observed by Konus-Wind, it had a duration ~1 s, a fluence ~4.5x10^-6 erg/cm2, a peak flux ~3.7x10^-6 erg/cm2 s (both in 20-200 keV range). Another two SGR-like bursts (soft and short) were observed by Konus-Wind in the background mode at 5021 s UT (01:23:41) and 16740 s UT (04:39:00) (also on May 2). The last burst was also detected by Helicon-Corronas-F in the background mode. The estimated time delay is consistent with SGR 1806-20 position. The Konus ecliptic latitude response indicates that the source of all these bursts is near the ecliptic plane, so we suppose, that they are also originated from SGR 1806-20.