From 6f1a6aa9edfbe46096a8816d93afa5345a7e25f8 Mon Sep 17 00:00:00 2001 From: Dmitriy Logashenko Date: Mon, 14 Aug 2023 16:03:04 +0300 Subject: [PATCH] Cosmetics in the Doxygen docu: DOIs in the references, LaTeX syntax corrections. --- .../spatial_disc/disc_util/conv_shape_interface.h | 8 ++++---- 1 file changed, 4 insertions(+), 4 deletions(-) diff --git a/ugbase/lib_disc/spatial_disc/disc_util/conv_shape_interface.h b/ugbase/lib_disc/spatial_disc/disc_util/conv_shape_interface.h index cd4a701cb..4c5f0a92b 100644 --- a/ugbase/lib_disc/spatial_disc/disc_util/conv_shape_interface.h +++ b/ugbase/lib_disc/spatial_disc/disc_util/conv_shape_interface.h @@ -52,9 +52,9 @@ namespace ug{ *
  • P. Frolkovic, H. De Schepper, Numerical Modelling of Convection Dominated * Transport Coupled with Density Driven Flow in Porous Media. * Advances in Water Resources 24 (1): 63–72, 2000, DOI: 10.1016/S0309-1708(00)00025-7
    • - *
  • K. W. Morton, D. F. Mayers, Numerical Solution of Partial Differential - * Equations, Cambridge University Press, 1994
    • - *
  • R. J. Le Veque, Numerical Methods for Conservation Laws, Birkhäuser, 1990
    • + *
  • K. W. Morton, D. Mayers, Numerical Solution of Partial Differential Equations: + * An Introduction (2nd ed.), Cambridge: Cambridge University Press, 2005, DOI: 10.1017/CBO9780511812248
    • + *
  • R. J. LeVeque, Numerical Methods for Conservation Laws (2nd ed.), Springer Basel AG, 1992, DOI: 10.1007/978-3-0348-8629-1
    • * * Convection shapes is one of possible implementations of upwind methods, * in which the upwind is considered as a special kind of interpolation of degrees @@ -78,7 +78,7 @@ namespace ug{ * through a subcontrol volume face with the integration point \f$ip\f$ is * \f[ \sum_{s=1}^{n_s} \phi_s (ip) \, c_s, \f] * where \f$\phi_s (ip)\f$ are the values of the \f$n_s\f$ ``convection shapes'' - * at \f$ip\f$, whereas $c_s$ are the degrees of freedom of \f$c\f$ corresponding + * at \f$ip\f$, whereas \f$c_s\f$ are the degrees of freedom of \f$c\f$ corresponding * to the shapes. * * Although the convection shapes for every upwind method are based on the