Dear Colleagues, The following article is accepted for publication as IBVS No. 5128. (Relayed by Kunjaya et al.) --- \documentstyle[twoside,epsf]{article} \input{ibvs2.sty} \begin{document} \IBVShead{xxxx}{xx May 2001} \IBVStitle {Superhump in November 2000 Superoutburst of TY Piscium} \IBVSauth{C.~Kunjaya$^{1,2}$,K.~Kinugasa$^1$,R.~Ishioka$^3$, T.~Kato$^3$,H.~Iwamatsu$^3$, M.~Uemura$^3$} \vskip 5mm \IBVSinst{Gunma Astronomical Observatory, Takayama, Agatsuma, Gunma 377-0702, JAPAN, e-mail: kinugasa@astron.pref.gunma.jp} \IBVSinst{Dept. of Astronomy, Institut Teknologi Bandung, Ganesa 10, Bandung 40132, Indonesia, e-mail: kunjaya@as.itb.ac.id} \IBVSinst{Dept. of Astronomy, Kyoto University, Kyoto 606-8502, Japan, e-mail: ishioka@kusastro.kyoto-u.ac.jp, tkato@kusastro.kyoto-u.ac.jp, iwamatsu@kusastro.kyoto-u.ac.jp, uemura@kusastro.kyoto-u.ac.jp} \IBVSobj{TY Psc} \IBVStyp{cataclysmic} \IBVSkey{dwarf novae -- photometry} \begintext The SU UMa type dwarf nova TY Psc was found in bright state on 28 Nov 2000 by J. Ripero (vsnet-campaign 545 : http://vsnet.kusastro.kyoto-u.ac.jp/vsnet/Mail/vsnet-campaign/msg00545.html and vsnet-superoutburst 66 : http://vsnet.kusastro.kyoto-u.ac.jp/vsnet/Mail/vsnet-superoutburst/ msg00066.html). It was then observed photometrically using small telescopes equipped with V filter, which resembles Johnson V filter and cooled CCD camera in three sites: \begin{enumerate} \item Kyoto University on October 30, 2000, using 25 cm Schmidt Cassegrain, with ST-7 CCD camera. \item Ouda Station, Kyoto University, on November 1, 2000, using 60 cm Cassegrain with PixelVision camera (SITe SI004AB, Cryo Tiger-cooled) and Rc filter. \item Gunma Astronomical Observatory on November 3, 2000, using 25 cm Newtonian with cooled Bitran 11 CCD camera and V filter. \end{enumerate} The exposure time was 30 seconds in Kyoto and Ouda, and around 25 to 40 seconds in GAO observation depending on the altitude of the object. Ouda data was reduced using IRAF APPHOT package. To correct for the read out noise, the object frames was subtracted by bias frames and for flat fielding we used twilight frames. GAO and Kyoto data was reduced by Java$^{TM}$-based aperture photometry package developed by one of the author (TK). The read out and thermal noise was removed by dark frame subtraction and flat fielding was done using twilight frames. Due to unstable weather condition, some of the Kyoto and Ouda data has to be rejected. The criterion for the rejection was one of the following condition, (1) the count of the comparison star drop to less than 25\% of the average count or (2) the count is more than 25\% of average count but dropped suddenly more than 25\% of those in the previous frame. Figure 1 showed the resulting light curve, the ordinate is the magnitude of the star relative to a comparison star. The comparison star used for differential photometry in Ouda data is 12.36 mag star GSC 2296.1010, GAO and Kyoto data is a 12.49 mag star GSC 2296.1213. \IBVSfig{8cm}{fig1.ps}{Light curves of TY Psc obtained at (a) Kyoto, (b) Ouda, and (c) Gunma.} The trend of the data from each site was removed using straight-line fitting. The three sets of data was then combined to form one data set. Similar trend removal procedure was applied once again to the combined data to remove the influence of observational environment difference. The final combined and corrected data was then analyzed using Phase Dispersion Minimization method (Stellingwerf, 1978), which was implemented into PDMWIN 3.0 computer program wrote by Widjaja (1996). The resulting $\theta$ diagram is presented in figure 2. \IBVSfig{8cm}{fig2.ps}{$\theta$ diagram of the period analysis of the combined data} >From figure 2 we can estimate the most probable period, that is about 102 minutes. To get a more precise period determination we took part of the figure 2 that is the valley around 102 minutes period and fit it to a parabolic curve. The minimum of the parabola occurs at the trial period 0.0708 day or 101.9 minute. Using this value we construct the folded light curve and presented in figure 3. This graph shows a usual superhump light curve, that is steeper brightening followed by shallower dimming. \IBVSfig{8cm}{fig3.ps}{Folded curve of the combined data} We used full width half maximum of the deepest valley of the $\theta$ diagram as the error of the period determination. Then the estimated error of the superhump period found is 0.4 minutes. In this work we could confirm and refine previous superhump period estimation of TY Psc quoted by Szkody and Feinswog (1988). Despite unfavorable weather in two observation site, the period determination was relatively accurate. This is the consequence of long time covering (4 days) so that slight change in trial period will cause significant difference in $\theta$ (see figure 2). Therefore long time covering is recommended for accurate determination of superhump period, provided there is no phase change between observations. Recalling the 98.4 minutes orbital period found by Thorstensen et al. (1996), this superhump period is 3.6\% longer than the orbital period which is quite normal for SU UMa type dwarf novae. \medskip \begin{references} Stelingwerf, R.F., 1978, {\it ApJ}, {\bf 224}, 953 Szkody, P., Feinswog L., 1988, {\it ApJ}, {\bf 334}, 422 Thorstensen, J.R., Patterson, J.O., Shambrook A., Thomas, G., 1996, {\it PASP}, {\bf 108}, 73 Widjaja, A., 1996, http://vsnet.kusastro.kyoto-u.ac.jp/vsnet/ \end{references} \IBVSefigure{fig1.ps} \IBVSefigure{fig2.ps} \IBVSefigure{fig3.ps} \end{document}