Changeset 10230 for NEMO/trunk/tests
- Timestamp:
- 2018-10-26T12:58:15+02:00 (6 years ago)
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NEMO/trunk/tests/README.rst
r10219 r10230 32 32 It serves as a benchmark for quantitative estimates of nesting errors as in Debreu et al. (2012), 33 33 Penven et al. (2006) or Spall and Holland (1991). 34 34 35 The animation below (sea level anomaly in meters) illustrates with two 1:2 successively nested grids how 35 36 the vortex smoothly propagates out of the refined grids. … … 40 41 ====== 41 42 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 Th e purpose of this test case is to evaluate the impact of various schemes and new development with iceshelf cavities.44 Th is 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>`_. 45 46 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). 47 48 48 49 .. image:: _static/ISOMIP_moc.png … … 83 84 .. image:: _static/wad_testcase_7.gif 84 85 85 86 87 86 ========== 88 87 References
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