Table 4: Positions of main activity peaks recorded in 2002. The instants of the maxima are determined with an error of 15 min. Our observations corresponding to the forecast of Jenniskens (2001), McNaught & Asher (2002) and Vaubaillon (2002) are presented in bold (see Sect. 5.3).
duration time [UT] $L_{\odot }$ 30-min
  day hour min J2000.0 shower rate
T <0.4 s 19 0 45 $236^{\circ}\!\!.46$ 35.48
  19 4 15 $236^{\circ}\!\!.61$ 162.75
  19 6 45 $236^{\circ}\!\!.71$ 69.58
  19 10 45 $236^{\circ}\!\!.88$ 100.66
$T \geq 0.4$ s 19 3 45 $236^{\circ}\!\!.59$ 175.63
  19 4 15 $236^{\circ}\!\!.61$ 297.98
  19 4 45 $236^{\circ}\!\!.63$ 130.50
  19 6 15 $236^{\circ}\!\!.69$ 84.88
  19 10 45 $236^{\circ}\!\!.88$ 46.39
$T\geq 1.0$ s 19 3 45 $236^{\circ}\!\!.59$ 137.25
  19 4 15 $236^{\circ}\!\!.61$ 243.02
  19 4 45 $236^{\circ}\!\!.63$ 101.53
  19 6 15 $236^{\circ}\!\!.69$ 72.08
  19 10 45 $236^{\circ}\!\!.88$ 16.07
$T\geq 10.0$ s 19 4 15 $236^{\circ}\!\!.61$ 75.02
  19 6 15 $236^{\circ}\!\!.69$ 36.35


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