In several recent large-eddy simulation studies, the lowest grid level was located well within the roughness sublayer. Monin–Obukhov similarity-based boundary conditions cannot be used under this scenario, and in this note we elaborate on this fundamental problem and suggest potential solutions.
Original languageEnglish
Pages (from-to)351-355
Number of pages5
JournalBoundary-Layer Meteorology: an international journal of physical and biological processes in the atmospheric boundary layer
Issue number2
Publication statusPublished - 2017

    Research areas

  • Inertial sublayer, Large-eddy simulation, Mo0nin–Obukhov similarity theory, Roughness sublayer , Surface layer

ID: 10083416