Changes between Version 3 and Version 4 of Changelog
- Timestamp:
- 2017-07-26T17:59:11+02:00 (7 years ago)
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Changelog
v3 v4 1 1 = NEMO Release notes 2 2 3 [[PageOutline(2 -3)]]3 [[PageOutline(2)]] 4 4 Last edition: '''[[Wikinfo(changed_ts)]]''' by '''[[Wikinfo(changed_by)]]''' 5 5 … … 22 22 }}} 23 23 24 == 2015 : From nemo_v3_6 to nemo_v3_6_STABLE: the release from CMIP6 experiments24 == 2015 v3.6 stable (CMIP6) 25 25 26 26 Main new features … … 41 41 * Faster split-explicit time stepping, Z-tilde ALE coordinates, implicit bottom friction 42 42 * First version of Configuration Manager 43 * Standalone OBS component and improvements in OBS &ASM43 * Standalone OBS component and improvements in OBS & ASM 44 44 45 45 ==== Features becoming obsolete … … 51 51 * On line coarsening of biogeochemistry 52 52 53 == 2014 From nemo_v3_5 to nemo_v3_653 == 2014 v3.6 54 54 55 55 Includes all the developments of 3_5 (especially the new XIOS IO system) , and new features: … … 70 70 * Atmospheric forcing at land-ocean interface 71 71 72 == 2012 From nemo_v3_4 to nemo_v3_572 == 2012 v3.5 73 73 74 74 Brief overview of the v3_5_alpha majors improvements and developments 75 75 76 The newInput/Output server XIOS is a major evolution including a versatile xml interface, the dedicated processors for I/O functionality allowing improved scalability, and a large performance improvement on massively parallel platforms. This option is now set as the default one. The previous IOIPSL code and interface are kept as backup options at this stage.76 The new !Input/Output server XIOS is a major evolution including a versatile xml interface, the dedicated processors for I/O functionality allowing improved scalability, and a large performance improvement on massively parallel platforms. This option is now set as the default one. The previous IOIPSL code and interface are kept as backup options at this stage. 77 77 78 78 === Interfaces … … 88 88 * Wave-NEMO interface module has been further developed with the introduction of the reading of the 2D stoke drift and wave number and the on-line computation of the 3D stoke drift current. 89 89 90 Also 90 === Misc. 91 91 92 92 * A new vertical sigma coordinate stretching function (Siddorn and Furner OM 2012r) 93 93 * Smagorinsky eddy coefficients: Smagorinsky type diffusivity/viscosity for lateral mixing has been introduced 94 94 * Analytical tropical cyclones taken in account using track and magnitude observations (Vincent et al. JGR 2012a,b) 95 95 * MUSCL: an option for local up-stream advection schemes which are useful in case of rivers, straits and in proximity of open lateral boundary conditions. The possibility to switch from MUSCL to a standard up-stream scheme has been included in the MUSCL advection routine … … 98 98 * Evolution of SETTE validation tool 99 99 100 == 2011 From tag nemo_v3_3 to nemo_v3_4100 == 2011 v3.4 101 101 102 102 This is a major release and the documentation has been updated in consequence. … … 106 106 ==== New physics and numerics 107 107 108 * new pressure gradient suitable for s-coordinate109 * completion of Griffies iso-neutral diffusion110 * back to a semi-implicit bottom friction111 * add Pacanowski-Philander scheme for computation of Ekman depth112 * add a new bulk formulae (so called MFS)113 * introduce a drag coefficient compute by wave model114 * add tidal potential forcing108 * New pressure gradient suitable for s-coordinate 109 * Completion of Griffies iso-neutral diffusion 110 * Back to a semi-implicit bottom friction 111 * Add Pacanowski-Philander scheme for computation of Ekman depth 112 * Add a new bulk formulae (so called MFS) 113 * Introduce a drag coefficient compute by wave model 114 * Add tidal potential forcing 115 115 * Netpune effect parametrization 116 * point to point MPI communication for north fold117 * allow sub timestepping for biogeochemistry models when using non-linear free surfac116 * Point to point MPI communication for north fold 117 * Allow sub timestepping for biogeochemistry models when using non-linear free surfac 118 118 * Improvement in PISCES (light limitation ; quota model for iron ; use Pa in gas exchange ; fldread for all data ; calcite dissolution & calcon salinity dependence ) 119 119 120 120 ==== Configurations, diagnostics and tools 121 121 122 * suppression of POMME configuration123 * addition of a regional configuration AMM12124 * improvement of format for lagrangian floats125 * online computing of transport across sections126 * tidal harmonic analysis127 * tools to prepare input files for observation operator128 * timing functionality122 * Suppression of POMME configuration 123 * Addition of a regional configuration AMM12 124 * Improvement of format for lagrangian floats 125 * Online computing of transport across sections 126 * Tidal harmonic analysis 127 * Tools to prepare input files for observation operator 128 * Timing functionality 129 129 130 130 ==== System simplification 131 131 132 * simplification of dynamic allocation133 * end of merge TRA/TRA (no more separate 3d arrays for tracers, only 4d)134 * suppression of obsolete hpg options135 * more flexible definition of BDY input data132 * Simplification of dynamic allocation 133 * End of merge TRA/TRA (no more separate 3d arrays for tracers, only 4d) 134 * Suppression of obsolete hpg options 135 * More flexible definition of BDY input data 136 136 * simplification of interfaces toward biogeochemical models 137 * interface with CICE in coupled mode137 * Interface with CICE in coupled mode 138 138 * Use of fldread to read/interpolate data for passive tracers and dynamical input data for OFFLINE configurations 139 139 140 == 2010 From tag nemo_v3_2 to nemo_v3_3141 142 * introduction of a modified leapfrog-Asselin filter time stepping scheme [Leclair and Madec 2009] ;143 * additional scheme for iso-neutral mixing [Griffies et al. 1998], although it is still a ”work in progress” ;144 * a rewriting of the bottom boundary layer scheme, following Campin and Goosse [1999] ;145 * addition of a Generic Length Scale vertical mixing scheme, following Um- lauf and Burchard [2003] ;146 * addition of the atmospheric pressure as an external forcing on both ocean and sea-ice dynamics ;147 * addition of a diurnal cycle on solar radiation [Bernie et al. 2007] ; river runoffs added through a non-zero depth, and having its own temperature and salinity ;140 == 2010 v3.3 141 142 * Introduction of a modified leapfrog-Asselin filter time stepping scheme [Leclair and Madec 2009] ; 143 * Additional scheme for iso-neutral mixing [Griffies et al. 1998], although it is still a ”work in progress” ; 144 * Rewriting of the bottom boundary layer scheme, following Campin and Goosse [1999] ; 145 * Addition of a Generic Length Scale vertical mixing scheme, following Um- lauf and Burchard [2003] ; 146 * Addition of the atmospheric pressure as an external forcing on both ocean and sea-ice dynamics ; 147 * Addition of a diurnal cycle on solar radiation [Bernie et al. 2007] ; river runoffs added through a non-zero depth, and having its own temperature and salinity ; 148 148 * CORE II normal year forcing set as the default forcing of ORCA2-LIM configuration ; 149 * generalisation of the use of fldread.F90 for all input fields (ocean climatology, sea-ice damping...) ;150 * addition of an on-line observation and model comparison (thanks to NEMOVAR project) ;151 * optional application of an assimilation increment (thanks to NEMOVAR project) ;152 * coupling interface adjusted for WRF atmospheric model ;149 * Generalisation of the use of fldread.F90 for all input fields (ocean climatology, sea-ice damping...) ; 150 * Addition of an on-line observation and model comparison (thanks to NEMOVAR project) ; 151 * Optional application of an assimilation increment (thanks to NEMOVAR project) ; 152 * Coupling interface adjusted for WRF atmospheric model ; 153 153 * C-grid ice rheology now available for both LIM-2 and LIM-3[Bouillon et al. 2009] ; 154 154 * LIM-3 ice-ocean momentum coupling applied to LIM-2 ; 155 * a deep re-writting and simplification of the off-line tracer component (OFF SRC) ;156 * the merge of passive and active advection and diffusion modules ;155 * Deep re-writting and simplification of the off-line tracer component (OFF SRC) ; 156 * Merge of passive and active advection and diffusion modules ; 157 157 * Use of the Flexible Configuration Manager (FCM) to build configurations, generate the Makefile and produce the executable ; 158 158 * Linear-tangent and Adjoint component (TAM) added, phased with v3.0 … … 160 160 In addition, several minor modifications in the coding have been introduced with the constant concern of improving the model performance. 161 161 162 == 2009 From tag nemo_v3_1 to nemo_v3_2162 == 2009 v3.2 163 163 164 164 ''This release has been mainly designed for climate models, with enhanced coupling interface and implementation of AR5 diagnostics.'' … … 166 166 === New science 167 167 168 * tidal mixing parametrization (bottom intensification) + Indonesian specific tidal mixing168 * Tidal mixing parametrization (bottom intensification) + Indonesian specific tidal mixing 169 169 * RGB light penetration and optional use of ocean color 170 170 * vvl option has been restored, including revisit free-surface time-splitting algorithm to reach stability and satisfying result and have vvl option available for all type of coordinates (z, zps, s) … … 173 173 === New High Performance Computing 174 174 175 * the way to handle outputs has been improved176 * implementation of IOM for output with the following functionalities : allows to output at few frequencies during same simulation, e.g both monthly and daily; output vectors/scalars is also available (for a strait transport calculation or for a vertical profile associated to buoys location for instance), and make easier the way to add an output everywhere in the code175 * Way to handle outputs has been improved 176 * Implementation of IOM for output with the following functionalities : allows to output at few frequencies during same simulation, e.g both monthly and daily; output vectors/scalars is also available (for a strait transport calculation or for a vertical profile associated to buoys location for instance), and make easier the way to add an output everywhere in the code 177 177 * Suppression of rigid-lid option and no more island specific treatment 178 178 * Cleaning of lib_mpp 179 179 * SHMEM option has been removed 180 * north fold treatment is now done once for all in a new routine lbcnfd.F909 instead of being duplicated181 * suppression of redundant east-west communication phase (ORCA grid case)182 183 == 2008 From tag nemo_v2.3 to nemo_v3_1180 * North fold treatment is now done once for all in a new routine lbcnfd.F909 instead of being duplicated 181 * Suppression of redundant east-west communication phase (ORCA grid case) 182 183 == 2008 v3.1 184 184 185 185 === New science … … 195 195 * Improvement of IOManager now able to handle long simulations and so to manage successive input files from one year to an other 196 196 * Improvements of AGRIF performance and users interface 197 * improved vectorial performances (~5%) of the rheology module in LIM 2.0197 * Improved vectorial performances (~5%) of the rheology module in LIM 2.0 198 198 * TOP reorganisation with one directory by model Fully written in Fortran 90, include all SMS models ( PISCES, LOBSTER, CFC ...) and interface for users developemnt through the MY_TRC directory) 199 199 * Update IOM modules for OFFLINE tracers … … 201 201 * Passive tracers used with AGRIF package 202 202 203 == 2007 From tag nemo_v2 to nemo_2_3203 == 2007 v2.3 204 204 205 205 === New science … … 212 212 === New High Performance Computing 213 213 214 == 2005-2006 From Tag nemo_v1 to nemo_v2214 == 2005-2006 v2.0 215 215 216 216 === New science