In gridpoint regional climate models (RCMs), the lateral boundary conditions are usually provided by a procedure called relaxation. The technique was originally studied in the context of numerical weather forecasting. This paper complements the preceding theoretical studies in order to assess the practical choices of model relaxation coefficients. Several profiles of coefficients used in RCMs are then evaluated. The complexity of actual model numerics makes any definite choice of the coefficients out of reach of simple theoretical considerations, but these provide practical guidelines. The latter are confirmed by pragmatic considerations such as minimizing discontinuities and keeping relaxation rates in the range of the represented physical...
Global atmospheric models are successfully used for climate simulation and may - in combination with...
A simple four-dimensional assimilation technique, called Newtonian relaxation, has been applied to t...
Regional climate simulations are long time integrations over an open system where the atmosphere ove...
In gridpoint regional climate models (RCMs), the lateral boundary conditions are usually provided by...
High‐resolution Regional Climate Models (RCMs) are driven at their lateral boundaries by information...
The present work introduces a new and useful tool to quantify the lateral boundary forcing of a regi...
The goal of limited area models (LAMs) is to downscale coarse-gridded general circulation model outp...
Limited-area models (LAMs) use higher resolutions and more advanced parameterizations of physical pr...
Dynamical downscaling by atmospheric Regional Climate Models (RCMs) forced with low-resolution data ...
The evaluation of the quality and usefulness of climate modeling systems is dependent upon an assess...
The MIUU mesoscale model was further developed, in order to include information on large-scale atmos...
Regional climate models are used by a large number of groups, for more or less all regions of the wo...
The newest model version of RegCM is adapted with the ultimate aim of providing climate projection f...
International audienceThis paper discusses the potential of Regional Climate Models (RCMs) as reanal...
Regional climate modeling using convection-permitting models (CPMs; horizontal grid spacing 10 km). ...
Global atmospheric models are successfully used for climate simulation and may - in combination with...
A simple four-dimensional assimilation technique, called Newtonian relaxation, has been applied to t...
Regional climate simulations are long time integrations over an open system where the atmosphere ove...
In gridpoint regional climate models (RCMs), the lateral boundary conditions are usually provided by...
High‐resolution Regional Climate Models (RCMs) are driven at their lateral boundaries by information...
The present work introduces a new and useful tool to quantify the lateral boundary forcing of a regi...
The goal of limited area models (LAMs) is to downscale coarse-gridded general circulation model outp...
Limited-area models (LAMs) use higher resolutions and more advanced parameterizations of physical pr...
Dynamical downscaling by atmospheric Regional Climate Models (RCMs) forced with low-resolution data ...
The evaluation of the quality and usefulness of climate modeling systems is dependent upon an assess...
The MIUU mesoscale model was further developed, in order to include information on large-scale atmos...
Regional climate models are used by a large number of groups, for more or less all regions of the wo...
The newest model version of RegCM is adapted with the ultimate aim of providing climate projection f...
International audienceThis paper discusses the potential of Regional Climate Models (RCMs) as reanal...
Regional climate modeling using convection-permitting models (CPMs; horizontal grid spacing 10 km). ...
Global atmospheric models are successfully used for climate simulation and may - in combination with...
A simple four-dimensional assimilation technique, called Newtonian relaxation, has been applied to t...
Regional climate simulations are long time integrations over an open system where the atmosphere ove...