The flux variability of Markarian 501 in very high energy gamma rays

Citation
J. Quinn et al., The flux variability of Markarian 501 in very high energy gamma rays, ASTROPHYS J, 518(2), 1999, pp. 693-698
Citations number
26
Categorie Soggetti
Space Sciences
Journal title
ASTROPHYSICAL JOURNAL
ISSN journal
0004637X → ACNP
Volume
518
Issue
2
Year of publication
1999
Part
1
Pages
693 - 698
Database
ISI
SICI code
0004-637X(19990620)518:2<693:TFVOM5>2.0.ZU;2-L
Abstract
The BL Lacertae object Markarian 501 was identified as a source of gamma-ra y emission at the Whipple Observatory in 1995 March. Here we present a flux variability analysis on several timescales of the 233 hr data set accumula ted over 213 nights (from March 1995 to July 1998) with the Whipple Observa tory 10 m atmospheric Cerenkov imaging telescope. In 1995, with the excepti on of a single night, the flux from Markarian 501 was constant on daily and monthly timescales and had an average flux of only 10% that of the Crab Ne bula, making it the weakest very high energy source detected to date. In 19 96, the average flux was approximately twice the 1995 flux and showed signi ficant month-to-month variability. No significant day-scale variations were detected. The average gamma-ray flux above similar to 350 GeV in the 1997 observing season rose to 1.4 times that of the Crab Nebula-14 times the 199 5 discovery level-allowing a search for variability on timescales shorter t han 1 day. Significant hour-scale variability was present in the 1997 data, with the shortest, observed on MJD 50,607, having a doubling time of simil ar to 2 hr. In 1998 the average emission level decreased considerably from that of 1997 (to similar to 20% of the Crab Nebula flux), but two significa nt flaring events were observed. Thus the emission from Markarian 501 shows large amplitude and rapid flux variability at very high energies, as does Markarian 421. It also shows large mean flux level variations on year-to-ye ar timescales, behavior that has not been seen from Markarian 421 so far.