Abstract
Abstract. 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.
Highlights
Lagoons are shallow water bodies that are separated from the ocean by barrier islands or spit and connected to the ocean by one or more restricted inlets (Kjerve and Magill, 1989)
In this study the model performance was tested using water level, sea surface temperature (SST) and surface salinity measurements acquired in three stations inside the lagoon (Juodkrante, Nida and Vente), one in the Klaipeda Strait (Klaipeda) and one in the Baltic Sea (Palanga, 25 km north of Klaipeda)
It gradually decreases with distance from the sea entrance going to the south and reaches fresh water salinity level (0.5 ‰) at a distance of approximately 35 km from the sea entrance
Summary
Lagoons are shallow water bodies that are separated from the ocean by barrier islands or spit and connected to the ocean by one or more restricted inlets (Kjerve and Magill, 1989). Their horizontal scale ranges from several to hundreds of kilometres whereas their vertical scale is only several metres. P. Zemlys et al.: Investigation of saline water intrusions into the Curonian Lagoon (Lithuania) fishing, tourism and other activities. Zemlys et al.: Investigation of saline water intrusions into the Curonian Lagoon (Lithuania) fishing, tourism and other activities They are the most productive areas of the coastal environment. It requires more sophisticated tools such as mathematical models that provide scientists and decision makers with a more holistic view of the physical, chemical and biological processes
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