\begin{table}%t4 %\centering \par \caption{\label{table4} 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 (\cite{jen1}), McNaught \& Asher (\cite{asmc3}) and Vaubaillon (\cite{vaub}) are presented in bold (see Sect.~\ref{comp_2002}).} \begin{tabular}{cccccr} \hline\hline \multicolumn{1}{c}{duration} & \multicolumn{3}{c}{time [UT]} & \multicolumn{1}{c}{$L_{\odot}$} & \multicolumn{1}{c}{30-min} \\ \multicolumn{1}{c}{} & \multicolumn{1}{c}{day} & \multicolumn{1}{c}{hour} & \multicolumn{1}{c}{min} & \multicolumn{1}{c}{J2000.0} & \multicolumn{1}{c}{shower rate} \\ \hline $T <0.4 $~s & 19 & 0 & 45 & $236^{\circ}\!\!.46$ & 35.48 \\ & \bf{19} &\bf{4} &\bf{15} & $236^{\circ}\!\!.61$ & \bf{162.75} \\ & \bf{19} & \bf{6} & \bf{45} & $236^{\circ}\!\!.71$ & \bf{69.58} \\ & \bf{19} &\bf{10} & \bf{45} & $236^{\circ}\!\!.88$ & \bf{100.66} \\ \hline $T\geq 0.4$~s & 19 & 3 & 45 & $236^{\circ}\!\!.59$ & 175.63 \\ & \bf{19} & \bf{4} & \bf{15} & $236^{\circ}\!\!.61$ & \bf{297.98} \\ & 19 & 4 & 45 & $236^{\circ}\!\!.63$ & 130.50 \\ & \bf{19}& \bf{6} & \bf{15} & $236^{\circ}\!\!.69$ & \bf{84.88} \\ & \bf{19} &\bf{10} & \bf{45} & $236^{\circ}\!\!.88$ & \bf{46.39} \\ \hline $T\geq 1.0$~s & 19 & 3 & 45 & $236^{\circ}\!\!.59$ & 137.25 \\ & \bf{19} &\bf{4} & \bf{15} & $236^{\circ}\!\!.61$ & \bf{243.02} \\ & 19 & 4 & 45 & $236^{\circ}\!\!.63$ & 101.53 \\ & \bf{19} & \bf{6} & \bf{15} & $236^{\circ}\!\!.69$ & \bf{72.08} \\ & \bf{19} & \bf{10}& \bf{45} & $236^{\circ}\!\!.88$ & \bf{16.07} \\ \hline $T\geq 10.0$~s& \bf{19} &\bf{4} &\bf{15} & $236^{\circ}\!\!.61$ & \bf{75.02} \\ & \bf{19} &\bf{6} &\bf{15} & $236^{\circ}\!\!.69$ & \bf{36.35} \\ \hline \end{tabular} \end{table}