Favorable lunar conditions accompanied the maximum of the
  2001 Quadrantid meteor shower. Peak activity was expected
  near 12h UT on January 3, corresponding to a solar longitude
  of lambda=283.16°.
  Observers were satisfied by good Quadrantid rates in the UT
  afternoon and evening hours of January 3, 2001. Radio forward-
  scatter observations as reported by Hiroshi Ogawa, Japan,
  showed increased Quadratid activity until 20h UT on January 3,
  compared with the background activity of December 30-January 1.
  Geometrical effects of radiant direction changes will play
  a significant role though. 
  The highest ZHR value is found for 13h30m UT on January 3
  or a solar longitude of lambda=283.24° (J2000.0). The
  ZHR of about 130 is a typical value for the Quadrantids,
  but the number of reports for the peak period is very small
  whence conclusions are tentative. The peak time may easily
  shift by one hour to either side once a more comprehensive
  dataset is available.
----------------------------------------------------- Date Time (UT) Sollong nObs nIND nQUA ZHR +/- ----------------------------------------------------- Jan 02 2300 282.63 2 2 17 13 9 Jan 03 0230 282.78 5 3 40 26 4 Jan 03 0510 282.89 13 5 109 17 3 Jan 03 0740 283.00 9 5 98 56 6 Jan 03 0940 283.08 10 8 192 61 4 Jan 03 1120 283.15 6 4 90 68 7 Jan 03 1330 283.24 3 2 33 131 23 Jan 03 1500 283.31 4 3 53 118 16 Jan 03 1720 283.41 5 3 76 82 9 Jan 03 1910 283.48 10 5 217 95 6 Jan 03 2110 283.57 5 4 98 79 8 Jan 04 0400 283.86 2 1 19 16 4 -----------------------------------------------------
  Solar longitudes refer to equinox J2000.0. nObs is the number
  of individual observing periods, nIND is the number of individual
  observers providing them, nQUA is the number of Quadrantids
  seen. The radiant position was assumed at alpha=230, delta=+49,
  the population index used was r=2.1. The expectation value of the
  ZHR,
ZHR = (1 + sum nQUA) / sum(Teff/C),
was used for the averages here, where Teff is the effective
  observing time and C is the total correction composed of limiting
  magnitude, clouds, and zenith correction. Times are rounded to
  the nearest 10 minutes. 
  We are very grateful to the following 23 observers who sent
  their reports to the Visual Commission or to the various
  mailing lists in time for this first activity overview:
  
  ANDBI Birger Andresen (Norway), MEIMA Marcel Meima (UK),
  BIVNI Nicolas Biver (USA), NICTE Ted A. Nichols II (USA),
  BURWI Wlliam Burton (USA), PUNNI Nilesh Puntambekar (India),
  DAVMA Mark Davis (USA), RENJU Jurgen Rendtel (Germany),
  GLIGE George W. Gliba (USA), SPAGE George Spalding (UK),
  GODSH Shelagh Godwin (UK), STOWE Wes Stone (USA),
  HALWA Wayne T. Hally (USA), TAIRI Richard Taibi (USA),
  HASTA Takema Hashimoto (Japan), TUKAR Arnold Tukkers (the Netherlands),
  HOSDA Dave Hostetter (USA), UCHSH Shigeo Uchiyama (Japan),
  JOHCA Carl Johannink (Germany), YOUKI Kim S. Youmans (USA),
  LINMI Mike Linnolt (USA), ZHUJI Jin Zhu (China) and
  MCBAL Alastair McBeath (UK).
 
                         
                         
 
                 
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