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Economy: European scale

Global Impacts

Globally aggregated economic impacts of global warming are a small fraction of income up until 3°C. A global mean average temperature rise of 2.5°C may lead to global aggregated economic losses between 0.2 and 2.0% of income and losses increase with greater warming. Little is known about aggregate economics impacts above 3°C (6).

Impacts in European economies: future snapshots

For most economic sectors, the impact of climate change will be small relative to the impacts of other drivers. Changes in population, age, income, technology, relative prices, lifestyle, regulation, governance and many other aspects of socio-economic development will have an impact on the supply and demand of economic goods and services that is large relative to the impact of climate change (6).

The economic impacts of climate change have been estimated for a global mean temperature rise of +2°C and +4°C, respectively (1). This has been done for 85 sub-regions covering 27 European countries. Impact functions were attached to specific activities within sectors that will be directly impacted by climate change. The same impact function was used to represent impacts in all sub-regions of Europe.The resulting climatic changes for the different regions in Europe were based on the results of the PESETA study (2). Hence, the results are to be interpreted as snapshots of the European economies under different climate futures. A so-called general equilibrium model (GRACE) was used; general equilibrium models suppose in principle that adaptation happens instantly when resource constraints shift, technologies change or new information arrives.

+2°C increase

The results indicate that the European economies are moderately affected by a +2°C increase: the total GDP for the European region falls by 0.03% when compared with GDP without climate change. These results agree with results from the PESETA study for a +2.5°C increase in 2080 (3).

The strongest negative impacts are found in the two southern regions, where a +2°C increase implies per year reductions in GDP up to 0.1% in Spain and Portugal. The effects in these southern regions are mainly caused by a drier climate, which affects agriculture and forestry. Higher temperature also implies negative impacts to tourism. Moderate, and even positive, effects are projected for the Baltics and Central-Eastern European countries. The western regions and the north of Europe are, in general, negatively affected by the +2°C shift, and with relatively small variations (1).

+4°C increase

At a +4°C shift, all sub-regions lose in economic terms in this study, and the reduction in GDP are considered substantial, especially in the southern regions of Europe. As expected, the sectors based on utilization of natural resources, agriculture, forestry and fisheries, are the most affected. For Europe the estimated reduction of annual GDP in 2080 is 0.26% (1). These results are stronger (more negative) than the results from the PESETA study for a +3.9°C increase in 2080 (3).

Regions that face the most negative impacts in the +2°C shift are the most severely impacted in the +4°C shift, and those who gain in the +2°C shift are the least affected in the +4°C shift. GDP loss in the sub-regions of Europe varies from less than 0.1% in some sub-regions of the Baltic States and Central-Eastern European countries to between 0.6 and 0.7% in the sub-regions of Galicia and Andalucia in Spain (1).

Impact on natural resources: agriculture and forestry

The results for a +4°C shift indicate an increase of the value of agricultural land by 0.6% in the Baltics, by 0.2% on the British Islands and by 5.4% in the Nordic countries. In the other regions, the value of land declines, up to 4.4% in Spain and Portugal. A general reduction of agricultural prices leads to a reduction in the contribution to GDP from agriculture in all regions, although there is a positive change in certain sub-regions (1).

In relative terms, the value of forested land exhibits the most substantial effect among the natural resources of a +4°C shift. It increases in all regions except the Mediterranean countries, and most in the Baltics and the Nordic countries, by 14.9% and 16.4%, respectively. This reflects a combination of increased physical growth and value of forested land, making a slight increase in the supply of forest products. This results in a reduced price of output, and the overall effect on the contribution to GDP is moderate (1).

Adaptation strategies

In a recent study it has been assessed that about a quarter of the world’s productive capital could be sensitive to climate (4). The study suggests that in a “perfect” world aggregate adaptation costs could be low when adaptation is proactive and anticipates warming approximately twenty years ahead. Delaying adaptation may increase adaptation costs by a factor of ten when adaptation only starts after vulnerable sectors are impacted. Overinvestment in protection capital, on the other hand, would allow the economy to stay consistently well-adapted to climate and avoid transient maladaptation costs.

The theory of adaptation timing identifies two situations where it is advisable to bring adaptation forward (5):

  1. Early benefits: Fast-tracking adaptation makes sense if measures have immediate benefits that would be otherwise be forgone. Examples include: improvements in water efficiency; flood protection measures; measures to deal with heat stress.
  2. Costly lock-in: Fast-tracking adaptation is also desirable if acting today costs less, in present value terms, than acting tomorrow. The most obvious cases are: long-lived infrastructure investments such as ports, roads, water supply systems and flood protection schemes; the design of buildings; spatial planning.


The references below are cited in full in a separate map 'References'. Please click here if you are looking for the full references for Europe.

  1. Aaheim et al. (2012)
  2. Christensen et al. (2007), in: Aaheim et al. (2012)
  3. Ciscar et al. (2011b), in: Aaheim et al. (2012)
  4. Dumas and Ha-Duong (2012)
  5. Fankhauser and Soare (2012)
  6. IPCC (2014)

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