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

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CHAPTER VI: WATER<br />

climate change, <strong>in</strong>clud<strong>in</strong>g risk management <strong>in</strong> one coast area aquifer. The results<br />

obta<strong>in</strong>ed from this case study can be applied to other similar aquifers, as it outl<strong>in</strong>es<br />

possible threats that would impact shallow groundwater resources, consider<strong>in</strong>g the<br />

implications for the management of water resources <strong>in</strong> different sectors. On the<br />

other words, on the basis of this one case study it was possible to create a model of<br />

potential risks for groundwater and water supply at this aquifer.<br />

The selected case study area was a large sand and gravel formation at Hanko<br />

pen<strong>in</strong>sula, Hanko aquifer, <strong>in</strong> the Southwestern coast of F<strong>in</strong>land. The Hanko aquifer<br />

was chosen because the permeable sand and gravel layers of this aquifer extends<br />

until the seashore, the water of the aquifer is <strong>in</strong> public use, and there are lots of<br />

human activities <strong>in</strong> the area. In addition, the hydrogeology of the area had already<br />

been studied <strong>in</strong>tensively, so that much data was available. Also, the Hanko Town<br />

Water Work was a very cooperative partner. There are several of comparable<br />

aquifers <strong>in</strong> F<strong>in</strong>land, <strong>in</strong> Sweden and <strong>in</strong> other countries on the coastl<strong>in</strong>e of <strong>Baltic</strong><br />

<strong>Sea</strong>, so that the results may be easily adapted to other areas.<br />

The potential effects of climate change on the Hanko shallow groundwater<br />

resources and <strong>in</strong>frastructures would cause risks not only from the change of<br />

precipitation and warmer temperature, but also from the rise of sea water level,<br />

mak<strong>in</strong>g the coastal aquifers more vulnerable to this change than the aquifers <strong>in</strong> the<br />

ma<strong>in</strong> land. The study also describes how the <strong>in</strong>frastructure and management of<br />

Hanko Water might economically adapt and respond to changes <strong>in</strong> climate, <strong>in</strong><br />

context of higher future population and change <strong>in</strong> land use and technology.<br />

Shallow groundwater resources have been studied extensively <strong>in</strong> F<strong>in</strong>land, and<br />

some local groundwater risk assessment has been done, but the study of effects of<br />

climate change on coastal aquifers is a new po<strong>in</strong>t of view. The discussion of all<br />

these factors together <strong>in</strong> relation to a coastal aquifer is also new.<br />

6.2 METHODOLOGY AND MATERIALS<br />

Method and materials<br />

The study method was to produce knowledge about risk assessment and risk<br />

management concern<strong>in</strong>g groundwater <strong>in</strong> one coastal aquifer. The results provided<br />

from this case study area can be applied to other similar aquifers. Some<br />

<strong>in</strong>formation was collected from previous studies and a part produced by this<br />

current study.<br />

All available data from Hanko aquifer was collected. Data was ma<strong>in</strong>ly<br />

collected from the Geological Survey of F<strong>in</strong>land, the Hanko Town Water Works,<br />

the Uusimaa <strong>Region</strong>al Environment Centre, and the F<strong>in</strong>nish Institute of Mar<strong>in</strong>e<br />

Research (FIMR).<br />

The most empirical and orig<strong>in</strong>al part of the material, the groundwater level<br />

monitor<strong>in</strong>g data of the Hanko aquifer, was produced by GTK between 12 February<br />

2007 and 12 June 2007 <strong>in</strong> two observation wells owned by Hanko Town: HP306<br />

observation well <strong>in</strong> the north-west side and HP66 observation well <strong>in</strong> the southeast<br />

side of the aquifer. The locations of the observation wells are shown <strong>in</strong> Figure<br />

5. The observation well HP306 is located <strong>in</strong> the Hopeasanta beach, about 100 m<br />

from the coast and about 100 m from the Hanko Town ma<strong>in</strong> water works. The<br />

NORDREGIO REPORT 2007:5 197

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