1 | ********************** |
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2 | Explore the test cases |
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3 | ********************** |
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4 | |
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5 | .. contents:: |
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6 | :local: |
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7 | |
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8 | List |
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9 | ==== |
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10 | |
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11 | The description below is a brief description of the test cases available in NEMO. |
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12 | |
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13 | ICEDYN |
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14 | ------ |
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15 | |
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16 | This test case illustrates the advection of an ice patch across a East/West and North/South periodic channel. |
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17 | This configuration can be used to test the advection of the ice patch in an AGRIF zoom (1:3) |
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18 | and across the AGRIF boundary or to test the ice advection schemes (Prather and Ultimate-Macho). |
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19 | In the latest case user need to remove ``key_agrif`` out of the CPP keys list. |
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20 | |
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21 | .. image:: _static/ICEDYN_UDIAG_43days_UM5.gif |
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22 | |
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23 | VORTEX |
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24 | ------ |
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25 | |
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26 | This test case illustrates the propagation of an anticyclonic eddy over a Beta plan and a flat bottom. |
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27 | It is implemented here with an online refined subdomain (1:3) out of which the vortex propagates. |
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28 | It serves as a benchmark for quantitative estimates of nesting errors as in Debreu et al. (2012) :cite:`DEBREU2012`, |
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29 | Penven et al. (2006) :cite:`PENVEN2006` or Spall and Holland (1991) :cite:`SPALL1991`. |
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30 | |
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31 | The animation below (sea level anomaly in meters) illustrates with two 1:2 successively nested grids how |
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32 | the vortex smoothly propagates out of the refined grids. |
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33 | |
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34 | .. image:: _static/VORTEX_anim.gif |
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35 | |
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36 | ISOMIP |
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37 | ------ |
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38 | |
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39 | The purpose of this test case is to evaluate the impact of various schemes and new development with the iceshelf cavities circulation and melt. |
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40 | 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`. |
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41 | The default setup is the one described `here <http://staff.acecrc.org.au/~bkgalton/ISOMIP/test_cavities.pdf>`_. |
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42 | |
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43 | The figure below (meridional overturning circulation) illustrates the circulation generated after 10000 days by the ice shelf melting (ice pump). |
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44 | |
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45 | .. image:: _static/ISOMIP_moc.png |
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46 | |
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47 | LOCK_EXCHANGE |
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48 | ------------- |
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49 | |
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50 | The LOCK EXCHANGE experiment is a classical fluid dynamics experiment that has been adapted |
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51 | by Haidvogel and Beckmann (1999) :cite:`HAIDVOGEL1999` for testing advection schemes in ocean circulation models. |
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52 | It has been used by several authors including Burchard and Bolding (2002) :cite:`BURCHARD2002` and Ilicak et al. (2012) :cite:`ILICAK2012`. |
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53 | The LOCK EXCHANGE experiment can in particular illustrate the impact of different choices of numerical schemes |
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54 | and/or subgrid closures on spurious interior mixing. |
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55 | |
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56 | Below the animation of the LOCK_EXCHANGE test case using the advection scheme FCT4 (forth order) for tracer and ubs for dynamics. |
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57 | |
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58 | .. image:: _static/LOCK-FCT4_flux_ubs.gif |
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59 | |
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60 | OVERFLOW |
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61 | -------- |
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62 | |
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63 | The OVERFLOW experiment illustrates the impact of different choices of numerical schemes |
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64 | and/or subgrid closures on spurious interior mixing close to bottom topography. |
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65 | The OVERFLOW experiment is adapted from the non-rotating overflow configuration described |
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66 | in Haidvogel and Beckmann (1999) :cite:`HAIDVOGEL1999` and further used by Ilicak et al. (2012) :cite:`ILICAK2012`. |
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67 | Here we can assess the behaviour of the second-order tracer advection scheme FCT2 and fortht-order FCT4, z-coordinate and sigma coordinate (...). |
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68 | |
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69 | Below the animation of the OVERFLOW test case in sigma coordinate with the forth-order advection scheme FCT4. |
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70 | |
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71 | .. image:: _static/OVF-sco_FCT4_flux_cen-ahm1000.gif |
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72 | |
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73 | WAD |
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74 | --- |
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75 | |
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76 | A set of simple closed basin geometries for testing the Wetting and drying capabilities. |
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77 | Examples range from a closed channel with EW linear bottom slope to a parabolic EW channel with a Gaussian ridge. |
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78 | |
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79 | 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. |
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80 | 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. |
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81 | The parameters are chosen such that the surge rises above sea-level before falling back and oscillating towards an equilibrium position |
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82 | |
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83 | .. image:: _static/wad_testcase_7.gif |
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84 | |
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85 | CANAL |
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86 | ----- |
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87 | |
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88 | East-west periodic canal of variable size with several initial states and associated geostrophic currents (zonal jets or vortex). |
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89 | |
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90 | .. image::_static/CANAL_image.gif |
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91 | |
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92 | Compile test cases |
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93 | ================== |
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94 | |
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95 | The compilation of the test cases is very similar to the manner the reference configurations are compiled. |
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96 | If you are not familiar on how to compile NEMO, it is first recomended to read :doc:`the instructions <install>` |
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97 | |
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98 | | In the same manner as the ref. cfg are compiled with '-r' option, test cases can be compile by the use of makenemo with '-a' option. |
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99 | |
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100 | | Here an example to compile a copy named WAD2 of the wetting and drying test case (WAD) on the macport_osx architecture on 4 cores: |
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101 | |
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102 | .. code-block:: console |
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103 | |
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104 | $ ./makenemo -n WAD2 -a WAD -m macport_osx -j 4 |
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105 | |
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106 | Run and analyse the test cases |
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107 | ============================== |
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108 | |
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109 | There no requirement of specific input file for the test_cases presented here. The XIOS xml input files and namelist are already setup correctly. |
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110 | For detailed description and Jupyter notebook, the reader is directed on |
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111 | the `NEMO test cases repository <http://github.com/NEMO-ocean/NEMO-examples>`_ |
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112 | |
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113 | References |
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114 | ========== |
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115 | |
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116 | .. bibliography:: test_cases.bib |
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117 | :all: |
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118 | :style: unsrt |
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119 | :labelprefix: T |
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