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| Titel |
Investigation of saline water intrusions into the Curonian Lagoon (Lithuania) and two-layer flow in the Klaipėda Strait using finite element hydrodynamic model |
| VerfasserIn |
P. Zemlys, C. Ferrarin, G. Umgiesser, S. Gulbinskas, D. Bellafiore |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
1812-0784
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| Digitales Dokument |
URL |
| Erschienen |
In: Ocean Science ; 9, no. 3 ; Nr. 9, no. 3 (2013-06-27), S.573-584 |
| Datensatznummer |
250018080
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| Publikation (Nr.) |
 copernicus.org/os-9-573-2013.pdf |
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| Zusammenfassung |
| This work is focused on the application of a modelling system to simulate
3-D interaction between the Curonian Lagoon and the Baltic Sea coastal
waters and to reflect spatiotemporal dynamics of marine waters in the
Curonian Lagoon. The model system is based on the finite element programme
package SHYFEM which can be used to resolve the hydrodynamic equations in
lagoons, coastal seas, estuaries and lakes. The results of a one year (2009)
3-D model simulation with real weather and hydrological forcing show that
the saline water intrusions from the sea through Klaipėda Strait are
gradually decreasing with distance from the sea and become negligible
(average annual salinity about 0.57‰) at a distance of
about 20 km to the south of Kiaulės Nugara island. Analyses of the
simulation results also show this area to be highly heterogeneous according
to the vertical salinity distribution. While in the deeper Klaipėda
Strait (harbour waterway) differences in average salinity between near
bottom and surface layers varies in the range 2–2.5‰,
in the rest of the Curonian Lagoon it is less than 0.5‰. The exchange flow showed vertical structure, but was horizontally uniform
with the presence of a two-directional flow that from time to time changes
to either saline water one-directional flow to the Curonian Lagoon or fresh
water one-directional flow to the sea. Two-directional flow duration
decreases with a distance from sea entrance in Klaipėda Strait from
around 180 days yr−1 close to the sea entrance to 50 days yr−1
just behind Kiaulės Nugara island. One-directional outflow duration is
increasing with a distance from the sea entrance from 100 to 225 days yr−1. One-directional inflow duration occurs in the range of 70–100 days
yr−1. The analysis of the ratio of buoyancy layer thickness to water
depth (hb/H) and the Wedderburn number identified the main importance of
wind action on the flow structure. Strong winds from the North and NW
determine a barotropic inflow which is mostly responsible for the salt water
intrusion into the Curonian Lagoon. Absence of wind or cross-strait wind
regimes allows the maintenance of a two-layer flow typical of estuarine
dynamics. |
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