Ignore:
Timestamp:
2019-10-18T14:33:36+02:00 (16 months ago)
Author:
nicolasmartin
Message:

Review of INSTALL.rst

File:
1 edited

Legend:

Unmodified
Added
Removed
  • NEMO/trunk/tests/README.rst

    r10605 r11723  
    1313 
    1414.. contents:: 
    15    :local: 
     15   :local: 
    1616 
    1717Procedure 
     
    3434------------------------------ 
    3535 
    36 There no requirement of specific input file for the test_cases presented here. The XIOS xml input files and namelist are already setup correctly.  
     36There no requirement of specific input file for the test_cases presented here. The XIOS xml input files and namelist are already setup correctly. 
    3737For detailed description and Jupyter notebook, the reader is directed on 
    3838the `NEMO test cases repository <http://github.com/NEMO-ocean/NEMO-examples>`_ 
     
    4242ICE_AGRIF 
    4343========= 
    44    
     44 
    4545  This test case illustrates the advection of an ice patch across an East/West and North/South periodic channel 
    4646  over a slab ocean (i.e. one ocean layer), and with an AGRIF zoom (1:3) in the center 
    47   The purpose of this configuration is to test the advection of the ice patch in   
     47  The purpose of this configuration is to test the advection of the ice patch in 
    4848  and across the AGRIF boundary 
    4949  One can either impose ice velocities or ice-atm. stresses and let rheology define velocities 
     
    5454VORTEX 
    5555====== 
    56    
     56 
    5757  This test case illustrates the propagation of an anticyclonic eddy over a Beta plan and a flat bottom. 
    5858  It is implemented here with an online refined subdomain (1:3) out of which the vortex propagates. 
    5959  It serves as a benchmark for quantitative estimates of nesting errors as in Debreu et al. (2012) :cite:`DEBREU2012`, 
    6060  Penven et al. (2006) :cite:`PENVEN2006` or Spall and Holland (1991) :cite:`SPALL1991`. 
    61    
     61 
    6262  The animation below (sea level anomaly in meters) illustrates with two 1:2 successively nested grids how 
    6363  the vortex smoothly propagates out of the refined grids. 
    64    
     64 
    6565  .. image:: _static/VORTEX_anim.gif 
    6666 
     
    6969 
    7070  The purpose of this test case is to evaluate the impact of various schemes and new development with the iceshelf cavities circulation and melt. 
    71   This configuration served as initial assesment of the ice shelf module in Losh et al. (2008) :cite:`LOSCH2008` and Mathiot et al. (2017) :cite:`MATHIOT2017`.  
     71  This configuration served as initial assesment of the ice shelf module in Losh et al. (2008) :cite:`LOSCH2008` and Mathiot et al. (2017) :cite:`MATHIOT2017`. 
    7272  The default setup is the one described `here <http://staff.acecrc.org.au/~bkgalton/ISOMIP/test_cavities.pdf>`_. 
    73    
     73 
    7474  The figure below (meridional overturning circulation) illustrates the circulation generated after 10000 days by the ice shelf melting (ice pump). 
    7575 
     
    8282  by Haidvogel and Beckmann (1999) :cite:`HAIDVOGEL1999` for testing advection schemes in ocean circulation models. 
    8383  It has been used by several authors including Burchard and Bolding (2002) :cite:`BURCHARD2002` and Ilicak et al. (2012) :cite:`ILICAK2012`. 
    84   The LOCK EXCHANGE experiment can in particular illustrate the impact of different choices of numerical schemes  
     84  The LOCK EXCHANGE experiment can in particular illustrate the impact of different choices of numerical schemes 
    8585  and/or subgrid closures on spurious interior mixing. 
    8686 
     
    9292======== 
    9393 
    94   The OVERFLOW experiment illustrates the impact of different choices of numerical schemes  
    95   and/or subgrid closures on spurious interior mixing close to bottom topography.  
    96   The OVERFLOW experiment is adapted from the non-rotating overflow configuration described  
     94  The OVERFLOW experiment illustrates the impact of different choices of numerical schemes 
     95  and/or subgrid closures on spurious interior mixing close to bottom topography. 
     96  The OVERFLOW experiment is adapted from the non-rotating overflow configuration described 
    9797  in Haidvogel and Beckmann (1999) :cite:`HAIDVOGEL1999` and further used by Ilicak et al. (2012) :cite:`ILICAK2012`. 
    9898  Here we can assess the behaviour of the second-order tracer advection scheme FCT2 and fortht-order FCT4, z-coordinate and sigma coordinate (...). 
     
    105105=== 
    106106 
    107   A set of simple closed basin geometries for testing the Wetting and drying capabilities.  
     107  A set of simple closed basin geometries for testing the Wetting and drying capabilities. 
    108108  Examples range from a closed channel with EW linear bottom slope to a parabolic EW channel with a Gaussian ridge. 
    109    
     109 
    110110  Below the animation of the test case 7. This test case is a simple linear slope with a mid-depth shelf with an open boundary forced with a sinusoidally varying ssh. 
    111111  This test case has been introduced to emulate a typical coastal application with a tidally forced open boundary with an adverse SSH gradient that, when released, creates a surge up the slope. 
     
    123123ICE_ADV2D 
    124124========= 
    125    
     125 
    126126  This test case illustrates the advection of an ice patch across an East/West and North/South periodic channel 
    127127  over a slab ocean (i.e. one ocean layer). 
     
    130130  (for now, Prather and Ultimate-Macho from 1st to 5th order), 
    131131  especially the occurence of overshoots in ice thickness 
    132    
     132 
    133133 
    134134ICE_ADV1D 
    135135========= 
    136    
     136 
    137137  This experiment is the classical Schar & Smolarkiewicz (1996) test case :cite:`SCHAR1996`, 
    138138  which has been used in :cite:`LIPSCOMB2004`, 
     
    141141  The purpose of this configuration is to test the caracteristics of advection schemes available in the sea-ice code 
    142142  (for now, Prather and Ultimate-Macho from 1st to 5th order), 
    143   especially the constitency between concentration, thickness and volume, and the preservation of initial shapes.   
     143  especially the constitency between concentration, thickness and volume, and the preservation of initial shapes. 
    144144 
    145 References 
    146 ========== 
     145.. rubric:: References 
    147146 
    148 .. bibliography:: test_cases.bib 
    149    :all: 
    150    :style: unsrt 
    151    :labelprefix: T 
     147.. bibliography:: tests.bib 
     148   :all: 
     149   :style: unsrt 
     150   :labelprefix: T 
Note: See TracChangeset for help on using the changeset viewer.