Changes between Version 22 and Version 23 of Users/Agenda/2018-07-11

Timestamp:

2018-07-11T13:39:53+02:00 (5 years ago)

Author:

clevy

Comment:

--

Users/Agenda/2018-07-11

@@ -60 +60 @@
      * '''Enhancements
          * Fix for tracer conservation with split explicit free surface
-         * bulk formulae : move to aerobulk package (Brodeau et al. 2016), i.e. NCAR, COARE and ECMWF bulk (remove Clio and MFS bulk)
-         * wetting and drying
-         * added tidal self attraction and loading either read from a file or from usual "scalar" approximation
-         * add a 4th order centered (CEN) and Flux Corrected Transport (FCT) tracer advection (using a 4th compact in the vertical)
+         * Bulk formulae : move to aerobulk package (Brodeau et al. 2016), i.e. NCAR, COARE and ECMWF bulk (remove Clio and MFS bulk)
+         * Wetting and drying
+         * Added tidal self attraction and loading either read from a file or from usual "scalar" approximation
+         * Add a 4th order centered (CEN) and Flux Corrected Transport (FCT) tracer advection (using a 4th compact in the vertical)
          * iso-neutral mixing (iso and triad operators): add the Method of Stabilizing Correction (MSC) (more accurate calculation) + add a bilaplacian case
          * Lateral physics (LDF): scale aware setting of eddy viscosity and diffusivity
-         * vorticity: 2 new energy conserving scheme:  ENT with Coriolis defined at T-point (better for Flux form) and EET a variant of EEN where e3t is used instead of e3f (solved the issue with e3f specification but is not enstrophy conserving)
+         * Vorticity: 2 new energy conserving scheme:  ENT with Coriolis defined at T-point (better for Flux form) and EET a variant of EEN where e3t is used instead of e3f (solved the issue with e3f specification but is not enstrophy conserving)
 
      * '''Test Cases
@@ -83 +83 @@
 
      * '''Wave coupling
-         * coupled interface to external wave model
-         * large scale wave interaction process added in momentum and tracer equations
+         * Coupled interface to external wave model
+         * Large scale wave interaction process added in momentum and tracer equations
 
      * ''' New sea-ice component SI3 (in place of LIMx)
          * Improvements in physics
-            * landfast ice: simple grounding with a "release" stress (not fully operational)
-            * lateral melting
-            * melt ponds: constant or Holland 2012 formulation (and soon topographic melt ponds)
-            * ice-atm. drags from Lupkes 2012 (depending on ice concentration) or Lupkes 2015 (depending on sea ice concentration and atm. stability) 
+            * Landfast ice: simple grounding with a "release" stress (not fully operational)
+            * Lateral melting
+            * Melt ponds: constant or Holland 2012 formulation (and soon topographic melt ponds)
+            * Ice-atm. drags from Lupkes 2012 (depending on ice concentration) or Lupkes 2015 (depending on sea ice concentration and atm. stability) 
          * Improvements in numerics
-            * advection: Ultimate-Macho scheme
-            * rheology: adaptive EVP (Kimmritz 2017)
-            * coupling interface: conductivity as surface forcing instead of heat fluxes (Met-Office requirement)
+            * Advection: Ultimate-Macho scheme
+            * Rheology: adaptive EVP (Kimmritz 2017)
+            * Coupling interface: conductivity as surface forcing instead of heat fluxes (Met-Office requirement)
          * Improvements in performance
-            * all thermodynamics in 1D
-            * reduced mpp communications
+            * All thermodynamics in 1D
+            * Reduced mpp communications
          * Users & developers friendly
-            * comprehensive set of outputs (universal units and understandable names + includes cmip)
-            * new architecture and namelist
-            * all processes can be decoupled from each other (switch on/off)
-            * ice categories bounds can be defined by the user or set automatically
-            * for open boundaries, the number of ice categories from the forcing model can be different from the number of categories in the regional simulation
-            * fully compatible with AGRIF
+            * Comprehensive set of outputs (universal units and understandable names + includes cmip)
+            * New architecture and namelist
+            * All processes can be decoupled from each other (switch on/off)
+            * Ice categories bounds can be defined by the user or set automatically
+            * For open boundaries, the number of ice categories from the forcing model can be different from the number of categories in the regional simulation
+            * Fully compatible with AGRIF
 
      * '''Passive tracer TOP and biogeochemical PISCES components
@@ -125 +125 @@
 
      * '''Simplification and robustness
-         * revised structure of namlist_ref/_cfg and default reference values.
-         * lateral physics (LDF): simplification of user interface and removal of CPP keys
-         * vertical physics (ZDF) (modularity, share shear production calculation between TKE and GKS, removal of all ZDF CPP keys, removal of avmu & avmv, minimization of MPP comm.: ~15 removed)
-         * remove the split-explicit ZDF scheme for both TRA and DYN
-         * remove the acceleration of convergence
+         * Revised structure of namlist_ref/_cfg and default reference values.
+         * Lateral physics (LDF): simplification of user interface and removal of CPP keys
+         * Vertical physics (ZDF) (modularity, share shear production calculation between TKE and GKS, removal of all ZDF CPP keys, removal of avmu & avmv, minimization of MPP comm.: ~15 removed)
+         * Remove the split-explicit ZDF scheme for both TRA and DYN
+         * Remove the acceleration of convergence
          * Generalised lbc_lnk and lbc_nfd 
          * Unify mppini