  We analyze H-alpha observations of the recurrent nova T CrB obtained during
the last decade. For the first time the H-alpha emission profile is analyzed
after subtraction of the red giant contribution. Based on our new radial
velocity measurements of the H-alpha emission line we estimate the component
masses of T CrB. It is found that the hot component is most likely a massive
white dwarf. We estimate the inclination and the component masses to be i~67
deg, Mwd = 1.37 +/-0.13 Msun and Msec=1.12 +/-0.23 Msun, respectively. The
radial velocity of the central dip in the H-alpha profile changes nearly in
phase with that of the red giant's absorption lines. This suggests that the dip
is most likely produced by absorption in the giant's wind.
  Our observations cover an interval when the H-alpha and the U-band flux vary
by a factor of ~6, while the variability in B and V is much smaller. Based on
our observations, and archival ultraviolet and optical data we show that the
optical, ultraviolet and H-alpha fluxes strongly correlate. We argue that the
presence of an accretion disc can account for most of the observed properties
of T CrB.
