Changeset 10230


Ignore:
Timestamp:
2018-10-26T12:58:15+02:00 (19 months ago)
Author:
mathiot
Message:

minor change in test/README.rst

File:
1 edited

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  • NEMO/trunk/tests/README.rst

    r10219 r10230  
    3232  It serves as a benchmark for quantitative estimates of nesting errors as in Debreu et al. (2012), 
    3333  Penven et al. (2006) or Spall and Holland (1991). 
     34   
    3435  The animation below (sea level anomaly in meters) illustrates with two 1:2 successively nested grids how 
    3536  the vortex smoothly propagates out of the refined grids. 
     
    4041====== 
    4142 
    42   Simple box configuration with an ice shelf covering all the domain. South part is a sloping ice shelf and north part is a flat ice shelf.  
    43   The purpose of this test case is to evaluate the impact of various schemes and new development with iceshelf cavities. 
    44   This configuration served as initial assesment of the ice shelf module in Losh et al. (2008) and Mathiot et al. (2017). 
     43  The purpose of this test case is to evaluate the impact of various schemes and new development with the iceshelf cavities circulation and melt. 
     44  This configuration served as initial assesment of the ice shelf module in Losh et al. (2008) and Mathiot et al. (2017).  
     45  The default setup is the one described `here <http://staff.acecrc.org.au/~bkgalton/ISOMIP/test_cavities.pdf>`_. 
    4546   
    46   The default setup is the one described [http://staff.acecrc.org.au/~bkgalton/ISOMIP/test_cavities.pdf]. 
     47  The figure below (meridional overturning circulation) illustrates the circulation generated after 10000 days by the ice shelf melting (ice pump). 
    4748 
    4849  .. image:: _static/ISOMIP_moc.png 
     
    8384  .. image:: _static/wad_testcase_7.gif 
    8485 
    85  
    86  
    8786========== 
    8887References 
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