Changeset 11723 for NEMO/trunk/tests
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- 2019-10-18T14:33:36+02:00 (5 years ago)
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NEMO/trunk/tests/README.rst (modified) (11 diffs)
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NEMO/trunk/tests/README.rst
r10605 r11723 13 13 14 14 .. contents:: 15 15 :local: 16 16 17 17 Procedure … … 34 34 ------------------------------ 35 35 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. 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. 37 37 For detailed description and Jupyter notebook, the reader is directed on 38 38 the `NEMO test cases repository <http://github.com/NEMO-ocean/NEMO-examples>`_ … … 42 42 ICE_AGRIF 43 43 ========= 44 44 45 45 This test case illustrates the advection of an ice patch across an East/West and North/South periodic channel 46 46 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 48 48 and across the AGRIF boundary 49 49 One can either impose ice velocities or ice-atm. stresses and let rheology define velocities … … 54 54 VORTEX 55 55 ====== 56 56 57 57 This test case illustrates the propagation of an anticyclonic eddy over a Beta plan and a flat bottom. 58 58 It is implemented here with an online refined subdomain (1:3) out of which the vortex propagates. 59 59 It serves as a benchmark for quantitative estimates of nesting errors as in Debreu et al. (2012) :cite:`DEBREU2012`, 60 60 Penven et al. (2006) :cite:`PENVEN2006` or Spall and Holland (1991) :cite:`SPALL1991`. 61 61 62 62 The animation below (sea level anomaly in meters) illustrates with two 1:2 successively nested grids how 63 63 the vortex smoothly propagates out of the refined grids. 64 64 65 65 .. image:: _static/VORTEX_anim.gif 66 66 … … 69 69 70 70 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`. 72 72 The default setup is the one described `here <http://staff.acecrc.org.au/~bkgalton/ISOMIP/test_cavities.pdf>`_. 73 73 74 74 The figure below (meridional overturning circulation) illustrates the circulation generated after 10000 days by the ice shelf melting (ice pump). 75 75 … … 82 82 by Haidvogel and Beckmann (1999) :cite:`HAIDVOGEL1999` for testing advection schemes in ocean circulation models. 83 83 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 85 85 and/or subgrid closures on spurious interior mixing. 86 86 … … 92 92 ======== 93 93 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 97 97 in Haidvogel and Beckmann (1999) :cite:`HAIDVOGEL1999` and further used by Ilicak et al. (2012) :cite:`ILICAK2012`. 98 98 Here we can assess the behaviour of the second-order tracer advection scheme FCT2 and fortht-order FCT4, z-coordinate and sigma coordinate (...). … … 105 105 === 106 106 107 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. 108 108 Examples range from a closed channel with EW linear bottom slope to a parabolic EW channel with a Gaussian ridge. 109 109 110 110 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. 111 111 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. … … 123 123 ICE_ADV2D 124 124 ========= 125 125 126 126 This test case illustrates the advection of an ice patch across an East/West and North/South periodic channel 127 127 over a slab ocean (i.e. one ocean layer). … … 130 130 (for now, Prather and Ultimate-Macho from 1st to 5th order), 131 131 especially the occurence of overshoots in ice thickness 132 132 133 133 134 134 ICE_ADV1D 135 135 ========= 136 136 137 137 This experiment is the classical Schar & Smolarkiewicz (1996) test case :cite:`SCHAR1996`, 138 138 which has been used in :cite:`LIPSCOMB2004`, … … 141 141 The purpose of this configuration is to test the caracteristics of advection schemes available in the sea-ice code 142 142 (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. 144 144 145 References 146 ========== 145 .. rubric:: References 147 146 148 .. bibliography:: test _cases.bib149 150 151 147 .. bibliography:: tests.bib 148 :all: 149 :style: unsrt 150 :labelprefix: T
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