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Details of Award

NERC Reference : NE/F010214/1

Nontraditional baroclinic wave effects in the Strait of Gibraltar

Grant Award

Principal Investigator:
Dr V Vlasenko, University of Plymouth, Sch of Earth Ocean and Environment
Science Area:
Marine
Overall Classification:
Marine
ENRIs:
Pollution and Waste
Natural Resource Management
Environmental Risks and Hazards
Science Topics:
Water Quality
Ocean Circulation
Survey & Monitoring
Abstract:
General wave theory suggests that baroclinic bores produced by a barotropic tide over bottom topography and propagated from the source of generation, disintegrate into a system of well rank-ordered internal waves packet. However, the majority of observational data collected in the Strait of Gibraltar by the University of Malaga during the three-month measurements at moorings located in the middle of the strait and beyond it (50 km off the strait in the Alboran Sea) doesn't support this idea. Less than 40% of all registered wave packets demonstrated the rank-ordered structure, whereas the rest of wave packets were clearly non-rank ordered. An evident contradiction between the up-to-date understanding of the wave process and observational evidence is a big challenge and strong motivation of the present study. It is important to make clear bearing in mind the great role which mixing processes initiated by tidally generated internal waves play both for regional ecological situation in the strait and adjacent areas and for the formation of the Deep Mediterranean Waters on a global scale. It is hypothesized in the project that the irregular structure of the observed packets is a manifestation of a more general mechanism of interaction of propagating along the channel large-amplitude internal waves with its lateral boundaries where extensive wave breaking, water mixing, wave refraction and reflection take place. Being repeated many times in every wave packet, these processes produce a complex spatial wave structure in which wave energy can transform both from wave to wave and sink to turbulence. Thus, the present proposal is intended to fill the gap in understanding of the not studied yet mechanism of the three-dimensional evolution of large-amplitude internal waves in the strait. As distinct from many previous theoretical studies which exploited the two-dimensional idea or the hydrostatic approximation for pressure and excluded the effects related to non-hydrostatic internal mixing, this project is aimed to apply a three-dimensiona fully-nonlinear nonhydrostatic numerical model and in combination with observational data to describe and quantify dynamical processes in the strait related to propagation of large amplitude internal waves. The achievement of the project goals is based on the the use of detailed observational data set collected in the Strait of Gibraltar and application of the state-of-the art the Massachusetts Institute of Technology general circulation model.
Period of Award:
1 Apr 2008 - 31 Mar 2009
Value:
£46,467
Authorised funds only
NERC Reference:
NE/F010214/1
Grant Stage:
Completed
Scheme:
Small Grants (FEC)
Grant Status:
Closed
Programme:
Small Grants

This grant award has a total value of £46,467  

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FDAB - Financial Details (Award breakdown by headings)

DI - Other CostsIndirect - Indirect CostsDA - InvestigatorsDI - StaffDA - Estate CostsDI - T&S
£2,379£16,218£4,529£15,092£5,211£3,040

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