This study was funded by the Alaska Outer Continental Shelf Region of the Minerals Management
The opinions, findings, conclusions, or recommendations expressed in this report or product are those of the authors and do not necessarily reflect the views of the U.S. Department of the Interior, nor does mention of trade names or commercial products constitute endorsement or recommendation for us...
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| Format: | Text |
| Language: | English |
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2009
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.383.5140 http://www.arlis.org/docs/vol1/D/710218841.pdf |
| Summary: | The opinions, findings, conclusions, or recommendations expressed in this report or product are those of the authors and do not necessarily reflect the views of the U.S. Department of the Interior, nor does mention of trade names or commercial products constitute endorsement or recommendation for use by the Federal Government. This document was prepared with L ATEX xfig, and inkscape. Acknowledgments The ROMS model is descended from the SPEM and SCRUM models, but has been entirely rewritten by Sasha Shchepetkin, Hernan Arango and John Warner, with many, many other contributors. I am indebted to every one of them for their hard work. Bill Hibler first came up with the viscous-plastic rheology we are using. Paul Budgell has rewritten the dynamic sea-ice model, improving the solution procedure and making the waterstress term implicit in time, then changing it again to use the elastic-viscous-plastic rheology of Hunke and Dukowicz. I am very grateful that he is allowing us to use his version of the code. The sea-ice thermodynamics is derived from Sirpa Häkkinen’s implementation of the Mellor-Kantha scheme. She was kind enough to allow Paul and I to start with her code. Thanks to the internet community for providing great tools like Perl, patch, cpp, svn, and gmake to aid in software development (and to make it more fun). |
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