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Lisø PhD Dissertation Manuscript - NTNU

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Figure 2 Empirically downscaled scenario showing increase<br />

in winter precipitation (winter ¼ December^February). Values<br />

are the di¡erence between the 2020^49 and 1961^90 periods<br />

and are given as changes per decade in percentage of 1961^90.<br />

The increase is larger than 1.5% per decade all over the country,<br />

and the largest increase is 3.4% per decade<br />

over the next 50 years, making the climate more similar<br />

to conditions presently experienced in the middle of the<br />

country. In the south of Norway the expected increase<br />

in winter temperature is smaller, but this part of the<br />

country is still expected to experience a warmer winter<br />

climate in future, more similar to the current winter<br />

climate in Denmark and southern areas of Sweden.<br />

Several sources of uncertainties exist related to both<br />

scenarios for global climate change, and to the effects<br />

of global warming on regional-level climate. Climate<br />

models differ in their indications of changes in the<br />

North Atlantic Ocean current (Gulf Stream) and in<br />

the extent of sea-ice cover in the Arctic. Changes in<br />

ocean currents and sea-ice will directly influence on the<br />

climatic conditions in Norway. The regional scenarios<br />

should not be considered as forecasts in an absolute<br />

sense. They offer insights into likely range and nature<br />

of future weather scenarios.<br />

Impacts of climate change<br />

Many sectors of Norwegian society may be affected by<br />

climate change. Impacts may be felt by economic<br />

sectors directly or indirectly dependent on climatic factors<br />

as well as environmental and social sectors. In the<br />

energy and hydropower sector, increased precipitation<br />

and runoff may enable increased power production. At<br />

Norway’s built environment<br />

the same time, however, increased temperatures are<br />

likely to reduce household space heating and energy<br />

demand (Sælthun, 1998). Present RegClim scenarios<br />

indicate that the growing season may increase by 20–<br />

30 days in large parts of the country up to 2050<br />

(Skaugen and Tveito, 2002). A longer growing season<br />

and an expansion of area suitable for crop cultivation<br />

creates potential for increased yields, if optimal adaptations<br />

of the crop calendar and switching to suitable<br />

crop types are possible in the context of structural<br />

changes in Norway’s agricultural sector (O’Brien et al.,<br />

2002). The forestry sector may also see a lengthened<br />

growing season and an expansion of land available for<br />

forest production (Ministry of the Environment, 1991;<br />

Parry, 2000). On the other hand, warmer weather may<br />

increase the incidence of pests and diseases, soil erosion,<br />

poor snow cover and hoar frost, posing threats to forest<br />

and agricultural yields as well as to natural ecosystems<br />

(Sygna and O’Brien, 2001). The fisheries sector is sensitive<br />

to climatic changes in terms of fish stocks, introduction<br />

of fish species from the south, and the frequency of<br />

diseases (Loeng, 1995). Many communities in Norway<br />

depend on the fishery sector. Overfishing has been an<br />

important determining factor of fish stocks in the past<br />

and the interaction between stock management and<br />

climate change may be critical for the performance of<br />

this sector in future.<br />

Few studies have examined the links between climate<br />

change and health in Norway, but studies in other parts<br />

of Europe suggest that health is sensitive to climatic<br />

events and changes. Health impacts occur via a variety<br />

of mechanisms, the direct impacts including heat- and<br />

cold-related illness and death related to thermal extremes<br />

and deaths, as well as injuries and psychological<br />

disorders related to other extreme weather events. In<br />

addition, indirect effects may occur, for example, as a<br />

result of disturbances in ecological systems and changes<br />

in geographic ranges and incidence of vector-borne<br />

diseases; in terms of respiratory disorders as a result of<br />

increased levels of air pollution, including pollen and<br />

spores; or in terms of mental health and nutritional<br />

impairment, infectious diseases and civil strife as a result<br />

of the effects of climatic changes on the economy, infrastructure<br />

and resource supply (Palutikof et al., 1997;<br />

Parry, 2000). This is a useful area of further research.<br />

The maintenance of infrastructure and buildings is likely<br />

to become more costly with an increase in precipitation<br />

and wind and other meteorologically triggered events,<br />

such as hurricanes, floods, avalanches and landslides.<br />

Potential impacts and sensitivity of buildings and<br />

building enclosures are examined in more detail below.<br />

Climate vulnerability in Norway<br />

De¢nitions of vulnerability<br />

Vulnerability is generally perceived to have both a physical<br />

and a social component. Chambers (1989 p.1)<br />

defines vulnerability as:<br />

203

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