@article{
 title = {Unified Curvilinear Ocean Atmosphere Model (UCOAM): A vertical velocity case study},
 type = {article},
 year = {2013},
 identifiers = {[object Object]},
 keywords = {Fully curvilinear,Geophysical fluid dynamics,LES,Non-hydrostatic,Vertical momentum equation,Vertical velocity},
 pages = {2158-2168},
 volume = {57},
 websites = {http://dx.doi.org/10.1016/j.mcm.2011.03.023},
 publisher = {Elsevier Ltd},
 id = {99917abc-9647-3b1c-aa0a-683b3834c409},
 created = {2016-04-26T23:13:55.000Z},
 file_attached = {true},
 profile_id = {ef52f833-b61a-3930-8f4c-9bf1e2e805d7},
 group_id = {dcacde6d-a3f0-31cd-bb07-bce6997a7c11},
 last_modified = {2017-03-14T15:59:20.340Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Abouali2013},
 private_publication = {false},
 abstract = {In this paper, the Unified Curvilinear Ocean Atmosphere Model (UCOAM) is described. UCOAM is a non-hydrostatic LES model, capable of reading curvilinear orthogonal and non-orthogonal grid in all the three dimensions including the vertical. Furthermore, the interaction of bottom bathymetry with the flow field and particularly, the vertical component of the velocity in a fully curvilinear grid and a sigma grid are presented. ?? 2011 Elsevier Ltd.},
 bibtype = {article},
 author = {Abouali, Mohammad and Castillo, Jose E.},
 journal = {Mathematical and Computer Modelling},
 number = {9-10}
}

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