Abstract: Lagrangian Coherent Structures and mixing properties of a tidal driven ow in the Ria de Arousa (Galicia, Spain)
Authors: Florian Huhn and Vicente Pérez-Muñuzuri and Pedro Montero
Florian Huhn and Vicente Pérez-Muñuzuri
Group of
Nonlinear Physics, Faculty of Physics,
University of Santiago de
Compostela, E-15782 Santiago de Compostela, Spain
Instituto Tecnolóxico para o Control do Medio Mari~no (INTECMAR),
E-36611 Vilagarcía de Arousa (Pontevedra), Spain
We study the
two-dimensional time dependent surface currents at the western coast of
Galicia, Spain, including estuarines (Rias Baixas) and o-shore regions
(Costa da Morte). Turbulence in ocean currents plays an important role
for the mixing of water volumes with dierent scalar properties. The
spatial structures of the current indicate, where turbulence-induced
mixing can be expected. The mixing spreads available nutrients and has
therefore a strong influence on the biological production. The currents
also drive the temporal evolution of oil spills and other contaminations
on the surface. Lagrangian Coherent Structures (LCS) of the flow are
detected by the analysis of Finite Time Lyapunov Exponents (FTLE) of the
velocity eld, see [1],[2],[3]. This approach is based on the theory
that the distance of two particle trajectories grows exponentially in
time for turbulent flows and reveals the flow structures that are
relevant for mixing. The analyzed velocity data is obtained from a 3-dim
ocean model (MOHID), which was run for dierent typical meteorological
situations at the coast of Galicia.
Concerning aquaculture, the
region Rias Baixas is one of the most productive areas in the world.
The
presence of harmful algae blooms (HAB) is a severe problem for this
industry. Therefore the
knowledge of areas of retention of primary
production and HABs inside the Rias is very important. In
order to
monitor the distribution of these retention zones, several drifter
experiments are performed
in the framework of the DRIFTER project in
an estuarine (Ria de Arousa), where the flow is mainly
forced by the
tides and the wind. The predicted mixing properties and LCSs are
compared to data
from these experiments.
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2000.
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Fernáandez, E. Hernandez-Garcia, and C. Lopez. Mixing structures in the
Mediterranean Sea from nite-size
Lyapunov exponents. Geophys. Res.
Letters, 31, 2004.
[3] S. Shadden, F. Lekien, J. Paduan, F. Chavez,
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structures
based on high-frequency radar data in Monterey Bay. Deep Sea Research
Part II: Topical Studies in Oceanography,
2008.