Ignore:
Timestamp:
2019-01-21T12:28:58+01:00 (19 months ago)
Author:
clem
Message:

fill up rst files for test cases

File:
1 edited

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  • NEMO/trunk/tests/README.rst

    r10279 r10554  
    1111  The description below is a brief description of the test cases available in NEMO.  
    1212 
    13 ICEDYN 
    14 ------ 
     13ICE_AGRIF 
     14--------- 
    1515   
    16   This test case illustrates the advection of an ice patch across a East/West and North/South periodic channel.  
    17   This configuration can be used to test the advection of the ice patch in an AGRIF zoom (1:3)  
    18   and across the AGRIF boundary or to test the ice advection schemes (Prather and Ultimate-Macho).  
    19   In the latest case user need to remove ``key_agrif`` out of the CPP keys list.  
     16  This test case illustrates the advection of an ice patch across an East/West and North/South periodic channel 
     17  over a slab ocean (i.e. one ocean layer), and with an AGRIF zoom (1:3) in the center 
     18  The purpose of this configuration is to test the advection of the ice patch in   
     19  and across the AGRIF boundary 
     20  One can either impose ice velocities or ice-atm. stresses and let rheology define velocities 
     21  (see README for details) 
    2022 
    21   .. image:: _static/ICEDYN_UDIAG_43days_UM5.gif 
     23  .. image:: _static/ICE_AGRIF_UDIAG_43days_UM5.gif 
    2224 
    2325VORTEX 
     
    9092  .. image::_static/CANAL_image.gif 
    9193 
     94ICE_ADV2D 
     95--------- 
     96   
     97  This test case illustrates the advection of an ice patch across an East/West and North/South periodic channel 
     98  over a slab ocean (i.e. one ocean layer). 
     99  The configuration is similar to ICE_AGRIF, except for the AGRIF zoom. 
     100  The purpose of this configuration is to test the advection schemes available in the sea-ice code 
     101  (for now, Prather and Ultimate-Macho from 1st to 5th order), 
     102  especially the occurence of overshoots in ice thickness 
     103   
     104 
     105ICE_ADV1D 
     106--------- 
     107   
     108  This experiment is the classical Schar & Smolarkiewicz (1996) test case :cite:`SCHAR1996`, 
     109  which has been used in :cite:`LIPSCOMB2004`, 
     110  and in which very specific shapes of ice concentration, thickness and volume converge toward the center of a basin. 
     111  Convergence is unidirectional (in x) while fields are homogeneous in y. 
     112  The purpose of this configuration is to test the caracteristics of advection schemes available in the sea-ice code 
     113  (for now, Prather and Ultimate-Macho from 1st to 5th order), 
     114  especially the constitency between concentration, thickness and volume, and the preservation of initial shapes. 
     115   
     116   
     117 
     118   
    92119Compile test cases 
    93120================== 
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