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This environmental impact assessment for Kriegers flak ... - Vattenfall

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70 PRESENTATION OF THE AREA<br />

1995). During normal winter storms the water level in<br />

Kattegat increases and, in comparison to the southern<br />

Baltic, there will be a height difference of ca 1 metre.<br />

<strong>This</strong> increased water level generates a greater inß ow<br />

of salt water from Kattegat via Öresund, increasing the<br />

Correlation between wind speed and current flow speed<br />

salination level in the Baltic. Periods of Þ ve to ten days<br />

of storm will also increase saltwater currents through<br />

the Bælts <strong>for</strong> the same reason.<br />

With a frequency of three years or more, large<br />

additions of salty water occur caused by prolonged<br />

winter storms preceded by periods of high pressure,<br />

<strong>for</strong>cing water from the Baltic, thus lowering the water<br />

level considerably. <strong>This</strong> prolonged inß ow means that<br />

the Belt sea front, where the bracken water mixes with<br />

the salty sea water, is shifted <strong>for</strong>ward to the Darss<br />

threshold. <strong>This</strong> makes it possible <strong>for</strong> a mixed water<br />

plume with a salinity of at least 17 PSU to move into<br />

the Arcona basin and later Þ ll up the other basins with<br />

heavy and oxygen rich water. These large additions of<br />

salty water are less frequent, resulting in a shortage of<br />

oxygen in the deep basins of theBaltic.<br />

11.2.2 Salinity, temperature and oxygen<br />

content<br />

The area at and around <strong>Kriegers</strong> Flak is hydrologically<br />

well documented. SMHI has since 1958 a measuring<br />

station in the Arcona basin east of <strong>Kriegers</strong> Flak measuring<br />

temperature, salination and oxygen content once<br />

or twice a month at each Þ ve metre interval from the<br />

surface down to a depth of 45 m (BY2). <strong>This</strong> measuring<br />

series can be downloaded from www.smhi.se.<br />

IOW in Rostock is working on a model <strong>for</strong> the salt<br />

level balance of the entire Baltic, taking into account<br />

the cumulative effects of establishing a number of<br />

offshore wind farms. Results should be known during<br />

2005.<br />

On behalf of the Group, the water conditions around<br />

<strong>Kriegers</strong> Flak have been researched continuously by<br />

IfAÖ during 2002-2003. <strong>This</strong> was carried out simultaneously<br />

with other water related <strong>environmental</strong><br />

Hydrographical data (median values +/- SD) during the three fishing campaigns in the test area in 2003<br />

Spring 2002<br />

Salt content<br />

[PSU]<br />

Water temperature<br />

[C°]<br />

Oxygen content<br />

[mg/l] [% fullness]<br />

Surface Seabed Surface Seabed Surface Seabed Surface Seabed<br />

Median values 7,6 7,9 15,6 13,9 9,1 8,6 91,5 83,1<br />

Standard deviation 0,2 0,6 0,3 1,3 0,2 0,2 1,9 1,9<br />

Differens surface/seabed<br />

Measurements: n=10<br />

-0,3 1,7 0,5 8,3<br />

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