  We compare phenomenological results from 3+1d quasiparticle anisotropic
hydrodynamics (aHydroQP) with experimental data collected in RHIC 200 GeV Au-Au
collisions. We present comparisons of identified particle spectra in different
centrality clases, charged particle multiplicity versus pseudorapidity,
identified particle multiplicity versus centrality across a wide range of
particle species, identified particle elliptic flow versus transverse momentum,
and charged particle elliptic flow as a function of transverse momentum and
rapidity. We use the same aHydroQP and hadronic production/feed down codes that
were used previously to describe LHC 2.76 TeV data. The aHydroQP hydrodynamic
model includes the effects of both shear and bulk viscosities in addition to an
infinite number of transport coefficients computed self-consistently in the
relaxation time approximation. To convert to the final state hadrons, we use
anisotropic Cooper-Frye freeze-out performed on a fixed-energy-density
hypersurface and compute the production/feed down using a customized version of
Therminator 2. We find good agreement with many heavy-ion collision observables
using only smooth Glauber initial conditions parameterized by an initial
central temperature of T_0 = 455 MeV, a constant shear viscosity to entropy
density ratio eta/s= 0.179, and a switching (freeze-out) temperature of
T_FO=130 MeV.
