From d1275778dd1f212eee13e8aa2d1f3b40d9401751 Mon Sep 17 00:00:00 2001 From: Arpit Babbar Date: Fri, 22 Nov 2024 10:35:42 +0100 Subject: [PATCH] Fix spelling of Siddhartha Mishra --- src/equations/shallow_water_1d.jl | 12 ++++++------ src/equations/shallow_water_2d.jl | 4 ++-- 2 files changed, 8 insertions(+), 8 deletions(-) diff --git a/src/equations/shallow_water_1d.jl b/src/equations/shallow_water_1d.jl index 3c218eee9d9..29642470262 100644 --- a/src/equations/shallow_water_1d.jl +++ b/src/equations/shallow_water_1d.jl @@ -201,7 +201,7 @@ end Non-symmetric two-point volume flux discretizing the nonconservative (source) term that contains the gradient of the bottom topography [`ShallowWaterEquations1D`](@ref). -Gives entropy conservation and well-balancedness on both the volume and surface when combined with +Gives entropy conservation and well-balancedness on both the volume and surface when combined with [`flux_wintermeyer_etal`](@ref). Further details are available in the papers: @@ -210,7 +210,7 @@ Further details are available in the papers: shallow water equations on unstructured curvilinear meshes with discontinuous bathymetry [DOI: 10.1016/j.jcp.2017.03.036](https://doi.org/10.1016/j.jcp.2017.03.036) - Patrick Ersing, Andrew R. Winters (2023) - An entropy stable discontinuous Galerkin method for the two-layer shallow water equations on + An entropy stable discontinuous Galerkin method for the two-layer shallow water equations on curvilinear meshes [DOI: 10.48550/arXiv.2306.12699](https://doi.org/10.48550/arXiv.2306.12699) """ @@ -237,7 +237,7 @@ This flux can be used together with [`flux_fjordholm_etal`](@ref) at interfaces conservation and well-balancedness. Further details for the original finite volume formulation are available in -- Ulrik S. Fjordholm, Siddhartha Mishr and Eitan Tadmor (2011) +- Ulrik S. Fjordholm, Siddhartha Mishra and Eitan Tadmor (2011) Well-balanced and energy stable schemes for the shallow water equations with discontinuous topography [DOI: 10.1016/j.jcp.2011.03.042](https://doi.org/10.1016/j.jcp.2011.03.042) and for curvilinear 2D case in the paper: @@ -310,7 +310,7 @@ is nonzero this should only be used as a surface flux otherwise the scheme will For well-balancedness in the volume flux use [`flux_wintermeyer_etal`](@ref). Details are available in Eq. (4.1) in the paper: -- Ulrik S. Fjordholm, Siddhartha Mishr and Eitan Tadmor (2011) +- Ulrik S. Fjordholm, Siddhartha Mishra and Eitan Tadmor (2011) Well-balanced and energy stable schemes for the shallow water equations with discontinuous topography [DOI: 10.1016/j.jcp.2011.03.042](https://doi.org/10.1016/j.jcp.2011.03.042) """ @@ -582,7 +582,7 @@ end equations::ShallowWaterEquations1D) Calculate Roe-averaged velocity `v_roe` and wavespeed `c_roe = sqrt{g * h_roe}` -See for instance equation (62) in +See for instance equation (62) in - Paul A. Ullrich, Christiane Jablonowski, and Bram van Leer (2010) High-order finite-volume methods for the shallow-water equations on the sphere [DOI: 10.1016/j.jcp.2010.04.044](https://doi.org/10.1016/j.jcp.2010.04.044) @@ -631,7 +631,7 @@ end end # Calculate the error for the "lake-at-rest" test case where H = h+b should -# be a constant value over time. +# be a constant value over time. @inline function lake_at_rest_error(u, equations::ShallowWaterEquations1D) h, _, b = u diff --git a/src/equations/shallow_water_2d.jl b/src/equations/shallow_water_2d.jl index 7ba36d6ec92..510d4560f9b 100644 --- a/src/equations/shallow_water_2d.jl +++ b/src/equations/shallow_water_2d.jl @@ -329,7 +329,7 @@ This flux can be used together with [`flux_fjordholm_etal`](@ref) at interfaces conservation and well-balancedness. Further details for the original finite volume formulation are available in -- Ulrik S. Fjordholm, Siddhartha Mishr and Eitan Tadmor (2011) +- Ulrik S. Fjordholm, Siddhartha Mishra and Eitan Tadmor (2011) Well-balanced and energy stable schemes for the shallow water equations with discontinuous topography [DOI: 10.1016/j.jcp.2011.03.042](https://doi.org/10.1016/j.jcp.2011.03.042) and for curvilinear 2D case in the paper: @@ -491,7 +491,7 @@ is nonzero this should only be used as a surface flux otherwise the scheme will For well-balancedness in the volume flux use [`flux_wintermeyer_etal`](@ref). Details are available in Eq. (4.1) in the paper: -- Ulrik S. Fjordholm, Siddhartha Mishr and Eitan Tadmor (2011) +- Ulrik S. Fjordholm, Siddhartha Mishra and Eitan Tadmor (2011) Well-balanced and energy stable schemes for the shallow water equations with discontinuous topography [DOI: 10.1016/j.jcp.2011.03.042](https://doi.org/10.1016/j.jcp.2011.03.042) """