hdl:10013/epic.48334
Non-Hydrostatic Dynamics of a Region with an Underwater Mountain
Contact
Alexey.Androsov [ at ] awi.de
Abstract
Non-hydrostatic boundary–value problem is considered in the 3-D domain representing a strait with an underwater sill. The equations are integrated in the boundary–fitted coordinates on irregular grid. For detection of non-hydrostatic effects the grid has increased resolution at sill slopes. The method is applied for simulation non-hydrostatic dynamics in the Strait of Messina.
Item Type
Article
Authors
Divisions
AWI Organizations > Climate Sciences > Climate Dynamics
AWI Organizations > Infrastructure > Scientific Computing
AWI Organizations > Infrastructure > Scientific Computing
Primary Division
Programs
Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 4: Research in science-stakeholder interactions > WP 4.1: Operational analyses and forecasting
Primary Topic
Helmholtz Programs > Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 4: Research in science-stakeholder interactions
Research Networks
Peer revision
Peer-reviewed
Publication Status
Published
Eprint ID
41421
DOI
10.7868/S0030157416030242
Cite as
Voltzinger, N.
and
Androsov, A.
(2016):
Non-Hydrostatic Dynamics of a Region with an Underwater Mountain
,
Oceanology,
56
(4),
pp. 537-546
.
doi: 10.7868/S0030157416030242
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