Ignore:
Timestamp:
2018-10-26T17:59:10+02:00 (3 years ago)
Author:
mathiot
Message:

include README in README.rst + del README + update .bib + add .bib management in README.rst

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1 edited

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  • NEMO/trunk/tests/test_cases.bib

    r10201 r10240  
    1 @book{epic31172, 
     1@book{HAIDVOGEL1999, 
    22   author = {D. B. Haidvogel and A. Beckmann}, 
    33   publisher = {Imperial College Press, London}, 
     
    66} 
    77 
    8 @book{burchard2002getm, 
     8@book{BURCHARD2002, 
    99   title={GETM: A General Estuarine Transport Model; Scientific Documentation}, 
    1010   author={Burchard, Hans and Bolding, Karsten}, 
     
    1313} 
    1414 
    15 @article{ILICAK201237, 
     15@article{ILICAK2012, 
    1616   title = "Spurious dianeutral mixing and the role of momentum closure", 
    1717   journal = "Ocean Modelling", 
     
    2121   issn = "1463-5003", 
    2222   doi = "10.1016/j.ocemod.2011.10.003", 
    23    author = "Mehmet Ilıcak and Alistair J. Adcroft and Stephen M. Griffies and Robert W. Hallberg", 
     23   author = "Mehmet Ilicak and Alistair J. Adcroft and Stephen M. Griffies and Robert W. Hallberg", 
    2424   keywords = "Spurious dianeutral transport, Cabbeling, Overflows, Exchange-flow, Ocean models, Momentum transport, Tracer advection, Reference potential energy" 
    2525} 
    2626 
    27 @article{DEBREU20121, 
     27@article{DEBREU2012, 
    2828   title = "Two-way nesting in split-explicit ocean models: Algorithms, implementation and validation", 
    2929   journal = "Ocean Modelling", 
     
    3737} 
    3838 
    39 @article{PENVEN2006157, 
     39@article{PENVEN2006, 
    4040   title = "Evaluation and application of the ROMS 1-way embedding procedure to the central california upwelling system", 
    4141   journal = "Ocean Modelling", 
     
    5050} 
    5151 
    52 @article{SPALL1991205, 
    53    author = {Spall, Michael A. and Holland, William R.}, 
     52@article{SPALL1991, 
     53   author = {Spall, M. A. and Holland, W. R.}, 
    5454   title = {A Nested Primitive Equation Model for Oceanic Applications}, 
    5555   journal = {Journal of Physical Oceanography}, 
     
    6060   doi = {10.1175/1520-0485(1991)021<0205:ANPEMF>2.0.CO;2}, 
    6161} 
     62 
     63@article{MATHIOT2017, 
     64   author = {Mathiot, P. and Jenkins, A. and Harris, C. and Madec, G.}, 
     65   title = {Explicit representation and parametrised impacts of under ice shelf seas in the ${z}^{\ast}$ coordinate ocean model NEMO 3.6}, 
     66   journal = {Geoscientific Model Development}, 
     67   volume = {10}, 
     68   year = {2017}, 
     69   number = {7}, 
     70   pages = {2849--2874}, 
     71   url = {https://www.geosci-model-dev.net/10/2849/2017/}, 
     72   doi = {10.5194/gmd-10-2849-2017} 
     73} 
     74 
     75@article{LOSCH2008, 
     76   author = {Losch, M.}, 
     77   title = {Modeling ice shelf cavities in a z coordinate ocean general circulation model}, 
     78   journal = {Journal of Geophysical Research: Oceans}, 
     79   volume = {113}, 
     80   year = {2008}, 
     81   number = {C8}, 
     82   pages = {}, 
     83   keywords = {Ice shelf cavities, numerical ocean modeling, z coordinates}, 
     84   doi = {10.1029/2007JC004368}, 
     85   url = {https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2007JC004368}, 
     86   eprint = {https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2007JC004368}, 
     87   abstract = {Processes at the ice shelf-ocean interface and in particular in ice shelf cavities around Antarctica have an observable effect on the solutions of basin scale to global coupled ice-ocean models. Despite this, these processes are not routinely represented in global ocean and climate models. It is shown that a new ice shelf cavity model for z coordinate models can reproduce results from an intercomparison project of earlier approaches with vertical ?~C or isopycnic coordinates. As a proof of concept, ice shelves are incorporated in a 100-year global integration of a z coordinate model. In this simulation, glacial meltwater can be traced as far as north as 15??S. The observed effects of processes in the ice shelf cavities agree with previous results from a ?~C coordinate model, notably the increase in sea ice thickness. However, melt rates are overestimated probably because the parameterization of basal melting does not suit the low resolution of this configuration.} 
     88} 
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