@@ -20,8 +20,8 @@ In the latter case, the [`ViscousFormulationLocalDG`](@ref) scheme is recommende
2020struct ViscousFormulationBassiRebay1 end
2121
2222"""
23- flux_parabolic(u_ll, u_rr, gradient_or_divergence, mesh, equations,
24- parabolic_scheme::ViscousFormulationBassiRebay1)
23+ flux_parabolic(u_ll, u_rr, gradient_or_divergence, mesh, equations,
24+ parabolic_scheme::ViscousFormulationBassiRebay1)
2525
2626This computes the classical BR1 flux. Since the interface flux for both the
2727DG gradient and DG divergence under BR1 are identical, this function does
@@ -66,11 +66,11 @@ Cockburn and Dong proved that this scheme is still stable despite the zero penal
6666ViscousFormulationLocalDG () = ViscousFormulationLocalDG (nothing )
6767
6868"""
69- flux_parabolic(u_ll, u_rr, ::Gradient, mesh::TreeMesh, equations,
70- parabolic_scheme::ViscousFormulationLocalDG)
69+ flux_parabolic(u_ll, u_rr, ::Gradient, mesh::TreeMesh, equations,
70+ parabolic_scheme::ViscousFormulationLocalDG)
7171
72- flux_parabolic(u_ll, u_rr, ::Divergence, mesh::TreeMesh, equations,
73- parabolic_scheme::ViscousFormulationLocalDG)
72+ flux_parabolic(u_ll, u_rr, ::Divergence, mesh::TreeMesh, equations,
73+ parabolic_scheme::ViscousFormulationLocalDG)
7474
7575These fluxes computes the gradient and divergence interface fluxes for the
7676local DG method. The local DG method uses an "upwind/downwind" flux for the
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