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Towards a Baltic Sea Region Strategy in Critical ... - Helsinki.fi

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CRITICAL INFRASTRUCTURE PROTECTION IN THE BALTIC SEA REGION<br />

observation well HP66 is located on the<br />

south beach, about 215 m from the<br />

Mannerheim<strong>in</strong>tie water works and 50 m<br />

from the coast.<br />

The measurement was done us<strong>in</strong>g<br />

the VanEssen Diver and VanEssen<br />

Barometer tools (Figure 4). Pressure<br />

and temperature were measured <strong>in</strong><br />

every 30 m<strong>in</strong>utes <strong>in</strong> both diver sensor<br />

and <strong>in</strong> air pressure sensors, which were<br />

situated <strong>in</strong> the hous<strong>in</strong>g of the HP66<br />

observation well. The groundwater<br />

level was calculated from the pressure<br />

<strong>in</strong> a diver sensor and was compensated<br />

with air pressure. <strong>Sea</strong> level monitor<strong>in</strong>g<br />

data of the same period were received<br />

from the F<strong>in</strong>nish Institute of Mar<strong>in</strong>e<br />

Research. This data was measured<br />

every hour.<br />

The most important factors<br />

controll<strong>in</strong>g the sea level <strong>in</strong> the <strong>Baltic</strong><br />

<strong>Sea</strong> are air pressure, w<strong>in</strong>d, water flow<br />

through the Danish Straits, and ice<br />

conditions <strong>in</strong> w<strong>in</strong>ter. Accord<strong>in</strong>g to FIMR<br />

(2007), tide has an effect of only a few<br />

centimetres on the F<strong>in</strong>nish coast. The<br />

Figure VI—4 Groundwater monitor<strong>in</strong>g tool<br />

<strong>in</strong>stallation at the well<br />

HP0306. (Photo by S.<br />

Luoma)<br />

currents flow through the Danish Straits, caused by sea level differences between<br />

the <strong>Baltic</strong> <strong>Sea</strong> and the North <strong>Sea</strong>, and can cause a change <strong>in</strong> the total amount of<br />

water <strong>in</strong> the <strong>Baltic</strong> <strong>Sea</strong> (bathtub effect). The air pressure is one of the ma<strong>in</strong> factors<br />

that affect the sea level. An air pressure change of 1 mbar corresponds to a sea<br />

level change of 1 cm. The normal pressure variations may thus cause a sea level<br />

variation of several tens of centimetres.<br />

6.3 HANKO AQUIFER<br />

Hanko study area<br />

The topography of the Hanko Pen<strong>in</strong>sula is relatively low and the average altitude<br />

is only about 13 m a.s.l. (N 60 ) (Figure 5). The studied 14 km 2 sand and gravel area,<br />

the Hanko aquifer, is a part of the First Salpausselkä end mora<strong>in</strong>e and the altitude<br />

<strong>in</strong> the area of this formation is about 10 – 12 m <strong>in</strong>creas<strong>in</strong>g slowly towards<br />

northeast. The general feature of the aquifer is flat pla<strong>in</strong> shelv<strong>in</strong>g to the seaside on<br />

its south and northwester side.<br />

The study area belongs to the town of Hanko, which lies partly on top of the<br />

aquifer under study. Hanko has about 10 000 <strong>in</strong>habitants and an area of about 800<br />

km 2 . The economy consists of 60 % services and 38 % <strong>in</strong>dustry. The town has a<br />

busy port, ma<strong>in</strong>ly handl<strong>in</strong>g transit trade to Russia, and many chemical <strong>in</strong>dustries.<br />

198 NORDREGIO REPORT 2007:5

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