Article
Time-dependent modeling of the Baltic entrance area. 2. Water and salt exchange of the Baltic Sea
Estuaries and Coasts (impact factor:
2.11).
03/2000;
23(2):253-266.
DOI:10.2307/1352831
pp.253-266
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Citations (0)
- Cited In (2)
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Article: Improvement of Baltic proper water quality using large-scale ecological engineering.
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ABSTRACT: Eutrophication of the Baltic proper has led to impaired water quality, demonstrated by, e.g., extensive blooming of cyanobacteria during the premium summer holiday season and severe oxygen deficit in the deepwater. Sustainable improvements in water quality by the reduction of phosphorus (P) supplies will take several decades before giving full effects because of large P storages both in soils in the watershed and in the water column and bottom sediments of the Baltic proper. In this article it is shown that drastically improved water quality may be obtained within a few years using large-scale ecological engineering methods. Natural variations in the Baltic proper during the last decades have demonstrated how rapid improvements may be achieved. The present article describes the basic dynamics of P, organic matter, and oxygen in the Baltic proper. It also briefly discusses the advantages and disadvantages of different classes of methods of ecological engineering aimed at restoring the Baltic proper from eutrophication effects. Preliminary computations show that the P content might be halved within a few years if about 100 kg O2 s(-1) are supplied to the upper deepwater. This would require 100 pump stations, each transporting about 100 m3 s(-1) of oxygen-rich so-called winter water from about 50 to 125 m depth where the water is released as a buoyant jet. Each pump station needs a power supply of 0.6 MW. Offshore wind power technology seems mature enough to provide the power needed by the pump stations. The cost to install 100 wind-powered pump stations, each with 0.6 MW power, at about 125-m depth is about 200 million Euros.AMBIO A Journal of the Human Environment 05/2007; 36(2-3):280-6. · 2.03 Impact Factor -
Article: The Baltic haline conveyor belt or the overturning circulation and mixing in the Baltic.
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ABSTRACT: A study of the water-mass circulation of the Baltic has been undertaken by making use of a three dimensional Baltic Sea model simulation. The saline water from the North Atlantic is traced through the Danish Sounds into the Baltic where it upwells and mixes with the fresh water inflow from the rivers forming a Baltic haline conveyor belt. The mixing of the saline water from the Great Belt and Oresund with the fresh water is investigated making use of overturning stream functions and Lagrangian trajectories. The overturning stream function was calculated as a function of four different vertical coordinates (depth, salinity, temperature and density) in order to understand the path of the water and where it upwells and mixes. Evidence of a fictive depth overturning cell similar to the Deacon Cell in the Southern Ocean was found in the Baltic proper corresponding to the gyre circulation around Gotland, which vanishes when the overturning stream function is projected on density layers. A Lagrangian trajectory study was performed to obtain a better view of the circulation and mixing of the saline and fresh waters. The residence time of the water masses in the Baltic is calculated to be 26-29 years and the Lagrangian dispersion reaches basin saturation after 5 years.AMBIO A Journal of the Human Environment 07/2004; 33(4-5):261-6. · 2.03 Impact Factor
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Keywords
Baltic entrance area
Baltic Sea
climatic change
deep-water renewal
deep-water salinity
deeper parts
freshwater supply
largest estuarine systems
major Baltic inflows
major inflow
major inflows
resulting inflow time-series
saline water
sea level variability
sea level variations
seasonal cycle
seasonal variation
smaller estuarine systems
tidal exchange
time-dependent model