Europe Europe Europe Europe

Agriculture: European scale

Length and intensity of Europe's thermal growing season

The agricultural potential and suitable conditions for forest growth in a certain part of the world can be expressed by two measures that describe the growing conditions for crops and trees in the summer season: the length and intensity of the so-called thermal growing season. Thermal growing season is the length of the growing season for crops and trees. It is defined to start when the daily mean temperature rises above a selected threshold in spring, and end as the mean temperature falls below that level in autumn. The intensity of the thermal growing season is represented by the effective temperature sum, also termed temperature accumulation or the growing degree day sum; this sum is calculated by summing the daily mean temperature excesses above the threshold during this season (41).


The commonly used base temperature for the thermal growing season is 5°C in boreal and temperate climate conditions (42) and 10°C in warmer climate zones (43).

Observations

Global warming leads to a prolongation and intensification of the thermal growing season. Prolongation and warming of this season has already been noticed in many regions: in northern Europe thermal growing season has lengthened by about 1week between 1951 and 2000 (44). The intensity of this season (expressed as growing degree day sum) has increased all over Europe after 2000 (45).

Projections

Projections of future changes have been calculated for Europe for the end of the 21st century, based on 22 - 23 global climate models under a moderate and high-end scenario of global warming, respectively (the so-called RCP4.5 and RCP8.5 scenarios). According to these results, in most of Europe the thermal growing season will last 1.5 - 2 months longer in 2100 compared to the reference period 1971 – 2000 for the high-end scenario of climate change, and 20 - 40 days longer for the moderate scenario of climate change; results are similar for the 5°C and 10°C baseline. Lengthening is anticipated to be slightest in southeastern European Russia and largest in coastal areas and central Europe (41).

For the high-end scenario the intensity of the thermal growing season with respect to the 5°C baseline (growing degree day sum) will be 60 - 100% higher in 2100; the increase is somewhat smaller for the moderate scenario. In absolute terms, the increase of the intensity of this season is largest in the south. In relative terms, however, the increase is largest in cold areas (41).

Benefits

The prolongation and intensification of the thermal growing season is beneficial for especially northern Europe. It enables the introduction of new species and cultivars in agriculture (46), allows a more extensive utilization of double-crop rotation (47) and enhances timber growth in forests (48). Besides, the mildness of the dark season facilitates the overwintering of fruit trees and other vulnerable perennial plants (49), and high autumn and winter temperatures accelerate the decomposition of litter and the release of nutrients in boreal forest, a factor that may already have enhanced timber growth (48).

Downside

On the other hand, long growing seasons and mild winters also favour pests and fungi in arable lands and forests, and higher temperatures in late autumn are of little use for plant photosynthesis in northern Europe due to the scantiness of the light. Also, annual cereal crops are harvested in early autumn and thus do not benefit from the autumn lengthening of the thermal growing season. In late autumn, the harvesting conditions would in any case be unfavourable owing to high moisture, even more so as precipitation is projected to increase and the low amount of solar radiation can no longer alone dry the harvest crop (41).

Conclusion

To conclude, the prolongation and intensification of the thermal growing season offers several benefits for northern European forestry and agriculture, but adaptation (plant breeding and pest control) is still necessary. In southern Europe, negative impacts dominate, particularly as a result of excessive heat and the reduced availability of water (41). 

Vulnerabilities and opportunities - global yields

Maize and soybean 

Maize and soybean are among the most important food crops worldwide. 10 countries represent 84 % and 94 % of the world’s maize and soybean production respectively. This includes 4 European countries: France, Romania, Italy and Ukraine (38). A modeling study has shown that global warming results in reduced growing season lengths and ultimately reduced yields for both crops, with maize being more negatively impacted than soybean (37).


Maize yields

Even a small increase in temperature of about 0.5 °C (compared to the period 1961 - 1990) will have negative impacts on global maize yield, the severity of which will increase with increasing temperature. For maize, under no adaptation, large (>30 %) reductions in national average yield were simulated for all the major producing countries under +4 degree warming, and for most under +2 degree warming. The results indicate a global yield reduction of 10 - 20 % for every 1 °C increase in temperature without adaptation. These impacts are stronger than previous estimates of a yield reduction of 3 - 8 % for every 1 °C increase in temperature (39).

Use of farmer-instigated adaptation strategies through changing planting date and crop variety may alleviate the effects of a 0.5 °C warming for maize yields; however, temperatures greater than 1 °C will negatively affect yield in most countries. The response to adaptation strategies is country-specific: of these 10 countries adaptation seems to be most effective for France, demonstrating no decrease in yield under a 4 °C increase in temperature with adaptation measures (37).

Soybean yields

Small temperature increases of 0.5 °C had no effect on soybean yield, although yield decreased as temperature increased. These negative effects, however, were partly compensated for by the implementation of adaptation strategies including planting earlier in the season and changing variety. For soybean, adaptation can be effective at temperatures up to 4 °C but that response is country-dependent (37).

Overview published results (including IPCC) wheat, maize, rice and soybean

There is medium confidence that climate trends have negatively affected wheat and maize production for many regions; there is also medium confidence for negative impacts on global aggregate production of wheat and maize. Changes in temperature caused reduction in global yields of maize and wheat by 3.8 and 5.5% respectively from 1980 to 2008 relative to a counterfactual without climate change, which offset in some countries some of the gains from improved agricultural technology (32). Effects on rice and soybean yields have been small in major production regions and globally (31). There is limited direct evidence that unambiguously links climate change to impacts on food security (31).

Global yield impacts of climate change and adaptation have been evaluated by analysing a data set of more than 1,700 published simulations for three crops: wheat, rice and maize (21). This is the largest pool of data from diverse modelling studies ever used for a global synthesis of this kind; the results have contributed to the food security and food production systems chapter of the Fifth Assessment Report (AR5) of the IPCC (22,31). The results show that without adaptation, losses in aggregate production are expected for wheat, rice and maize in both temperate and tropical regions by 2°C of local warming. The results also show that crop-level adaptations increase simulated yields by an average of 7-15%, with adaptations being more effective for wheat and rice than maize. Yield losses are greater in magnitude for the second half of the century than for the first. Even moderate warming may reduce temperate crop yields in many locations.

For around 1-3°C warming, the data show both positive and negative yield responses, whereas the previous Fourth Assessment Report (AR4) had primarily positive responses at these temperature changes. For all three temperate crops the new data set shows a greater risk of yield reductions at moderate warming than AR4. The results show that adaptation provides clear benefits for wheat and rice: the central tendencies indicate that most yield loss in wheat may be avoided, or even reversed, in tropical regions up to 2-3°C of local warming and in temperate regions across a broad range of warming (21).

In the more than 1,700 published simulations there is a majority consensus that yield changes will be negative from the 2030s onwards. More than 70% of projections indicate yield decreases for the 2040s and 2050s, and more than 45% of all projections for the second half of the century indicate yield decreases greater than 10%. The magnitude of the yield impact generally increases with time. These projections include simulations with adaptation, suggesting that farmer adaptation earlier in the twenty-first century can ameliorate some, but not all, risk of yield reductions. It looks like increases in yield variability become increasingly likely as the century progresses (21).

There are a number of limitations with respect to this meta-analysis, however, such as:  the lack of simulation of pests, weeds and diseases, the frequent assumption of water availability into the future despite ongoing changes in many regions, inaccuracies in representing adaptations, and structural, parameter and bias correction uncertainty in both crop and climate models (21).

The impact of ozone versus global warming

Global demand for food is expected to increase by at least 50% from 2010 to 2050 mainly as a result of population growth and a shift towards a more `westernized' diet in developing regions (28). Both temperature extremes and surface ozone, formed through the photochemistry of precursor gases mainly arising from human activities, are detrimental to crop yields (27). The impact of global warming and surface ozone concentration has been projected for 2050 compared with 2010 for two greenhouse gasses emission scenarios: an intermediate pathway with a global reduction in surface ozone due to pollution control measures worldwide (RCP4.5) and a more `pessimistic', energy-intensive pathway with a worldwide increase in ozone except in the US and around Japan (RCP8.5) (27). According to these projections, more severe ozone pollution (scenario RCP8.5) leads to substantial crop damage on a global scale, reducing global total crop production by 3.6%. In this scenario, ozone pollution and climate change combine to reduce global crop production by 15% between 2010 and 2050.  Aggressive pollution control worldwide, however, (scenario RCP4.5) leads to an overall 3.1% increase in global production. According to these results, ozone pollution control (scenario RCP4.5) has the potential to partially offset the negative impact of climate change, leading to a smaller combined global crop production decrease of 9.0%.

Cereal yield reduction from ozone could reach 6 and 10% in 2030 for the European Union with the B1 and A2 scenarios, respectively (33).

Vulnerabilities and opportunities - European yields according to review studies 

Review Knox et al. (2016)

Climate impacts in Europe are not necessarily all negative. They could be beneficial for many crops and areas of production. This message was sent by the authors of a recent study in which they combined results of 41 scientific publications (59). Their study confirms that climate change is likely to increase the yield of Europe’s major agricultural cropping systems, with more favourable impacts in northern and central Europe.


The projected impacts of climate change on the yield of seven major crop types have been assessed. These crops are wheat, barley, maize, potato, sugar beet, rice and rye. Compared with the period 1961-1990, the projected change in average yield in Europe for these seven crops by the 2050s is a yield increase by 8%. Only for maize a reduction by 6% is projected. For wheat and sugar beet, projected average yield increase is highest: 14% and 15%, respectively. These increases are largely due to rising atmospheric CO2 concentrations, enhancing both crop productivity and resource use efficiency. Evidence of climate impacts on yield was extensive for wheat, maize, sugar beet and potato, but very limited for barley, rice and rye (59).

The findings of this study show strong regional differences with average crop impacts by the 2050s in northern Europe being higher (+14%) and more variable compared to central (+6%) and southern (+5) Europe (59).

Projections for northern Europe show significant higher average yields for maize and potato in the 2050s (+12% and +18%, respectively) and 2080s (+19% and +14%, respectively), compared with the reference period 1961-1990. Positive impacts for most crops apart from maize were also reported for central and southern Europe. The project decrease in average yield for maize in central Europe is 9% for the 2020s and 15% by the 2080s. Maize is projected to suffer the largest mean decrease in southern Europe, up to 28% by the 2080s (59).

The findings of this study corroborate other studies that show how crop productivity impacts in higher-latitude temperate regions, such as northern Europe, are generally expected to be less severe than in lower-latitude more tropical regions (60). The findings also illustrate that a lot of knowledge is available on projected crop yield changes for wheat and maize, but far less so for climate impacts on important crops such as barley, rice and rye. In addition, the study confirms there is extensive evidence on climate impacts on crop production for northern and central Europe, but much fewer studies for southern Europe (59). 

Review Iglesias et al. (2012)

Recently, Iglesias et al. inventorized the overall impact of climate change on farming across agro-climatic zones in Europe within a time-frame of 2050 to 2080, based on 300 references that have been published in the period 1995 - 2010 (1). Their subdivision in agro-climatic zones is shown in figure 1. The risks and opportunities according to their inventory are summarized in figure 2. The text below is based on their paper unless stated otherwise.

The effects of climate change and increased atmospheric carbon dioxide are expected to lead, overall, to small increases in European crop productivity at moderate warming (2). On a regional scale, impacts on crop yields are expected to vary across Europe due not only to changes in the mean of climate variables but also due to the increase in climate variability or extreme events.

 

Figure 1. Agro-climatic regions considered by Iglesias et al. (2012).

 

Figure 2. Summary of risks and opportunities in the agro-climatic areas of Europe (from Iglesias et al., 2012).

 

Boreal region

Increased temperatures may increase both the cultivable area and crop yields within the entire zone, as well as provide opportunities for increased livestock production. However, the soil types in this zone may limit the potential for increased agricultural production. In addition, increased rainfall may lead to increased waterlogging, flooding risk and perhaps also a decrease in water quality.

Atlantic region

There is potential for increased agricultural production in the Atlantic north region, especially in the livestock sector, but soil type may limit this potential. Measures need to be introduced to enable adaptation to drier summers, as currently summer rainfall usually enables unrestricted growth of crops and forage.

Particularly vulnerable to flooding from rising sea levels is the Atlantic central region and attention needs to be given to measures that will reduce this risk. Some increases in agricultural production are possible from increased yields of cereals and the introduction of new crops. However, it may be difficult to maintain the yields of more moisture- or temperature-sensitive crops if summer rainfall decreases and insufficient water is available for irrigation.

The priority for the Atlantic south region will be to conserve water to reduce the risk of decreases in crop yields and to avoid conflict with other water users. There may also be opportunities to grow crops more tolerant to heat and drought.

Continental region

In the Continental north region the increase in the northern range of crops and longer growing season offers the potential for increased crop and livestock production. However water stress in summer and infertile soils may limit this potential. Flooding is also a serious risk. Priority needs to be given to manage water supplies to reduce the risk of flooding and to conserve water to increase availability for agriculture.

Agriculture in the Continental south region is likely to be adversely affected by hotter drier summers with yields of crops such as potatoes, sugar beet and forage crops most likely to be reduced. Priority needs to be given to ensuring water supplies for agriculture and also promoting the growth of crops, such as soya, that could replace vulnerable crops.

Alpine region

Changes in precipitation pattern and increased frequency of extreme events appear to pose the greatest risks in the Alpine region. There may be opportunities for increased production of both crops and livestock but the realisation of these opportunities will depend upon the continued availability of water at critical periods of crop growth. However, changes in precipitation pose some of the greatest risks in this zone, together with an increased risk of extreme weather events. There may be benefits from a longer growing season and the ability to grow some crops at higher altitudes, but this potential may not be realised due to soil limitations.

Mediterranean region

In the Mediterranean north region the forecast risks greatly outweigh any potential benefits. Forecast decreases in total annual rainfall make water conservation a priority and careful attention needs to be given to avoiding conflicts over water use.

For the Mediterranean south region eight of the risks are considered to be high priority. The main risks directly concern the consequences of potential reductions in total precipitation. Hence strategies need to be considered to conserve as much water as possible over winter to maintain supply during the summer. The risk of reduced yields was also assessed as high and strategies need to be developed to adopt cultivars or crops better suited to reduced water availability and heat stress. No significant opportunities were identified in this zone, which is not well placed to benefit from the forecast changes in climate. The impacts of climate change are forecast to be so serious that it may lead to land abandonment.

Vulnerabilities and opportunities - European yields other sources

European wheat production

With 25% of the global wheat area and 29% of global wheat production (24), Europe is the largest producer of wheat. The increased occurrence and magnitude of adverse and extreme agroclimatic events are considered a major threat for wheat production. A recent study (25) showed that, by 2030, we should expect a twofold increase in the global wheat-growing area threatened by extremely high temperatures during critical developmental stages in a typical year, and a more than threefold increase of the area at risk by 2050.


From climate change projections (based on the relative extreme high-end scenario RCP8.5) it was shown that the occurrence of adverse conditions for the main European wheat-growing areas might substantially increase by 2060 compared to the present (1981–2010), which is likely to result in more frequent crop failure across Europe. This would have profound repercussions given the importance of European wheat production in the global food trade (23). The adverse agroclimatic conditions that have been studied are: severe winter frost without snow cover, late frost, excessive soil moisture with water logging from sowing to anthesis, high precipitation event with the possibility of widespread lodging, severely dry growing season (sowing–maturity), severe drought event between sowing and anthesis, severe drought event between anthesis and maturity, heat stress at anthesis, heat stress during grain filling, adverse conditions during sowing, adverse conditions during harvest. The climate projections indicate that sowing dates will move forward on average by 15 +/- 7 days in 2060 compared to the present, whereas anthesis and maturity dates will be two weeks earlier (23).

For winter wheat growth duration is reduced, because any changes in sowing date in autumn would have little effect on duration of the vegetative and reproductive phases in the following spring and summer. This response concurs well with observed response of winter wheat yields in Denmark, where the largest reductions were related to high temperatures during the grain-filling phase (54). 

Climate change is likely to increase cereal yields in Northern Europe but decrease yields in Southern Europe (31).

Northward expansion crops

Warming has already caused a northward expansion of the area of silage maize in northern Europe into southern parts of Scandinavia, where the system of grass and silage maize for intensive dairy production has largely replaced the traditional fodder production systems (50). Very recently grain maize has started to be grown in southern parts of Denmark, reflecting the warming trends (51). Analyses of the effects of observed climate change on yield potential in Europe have shown positive effects for maize and sugar beet, which have benefited from the longer growing season for these crops (52). Yield benefits have been greatest in northern Europe. The warming may also have contributed to higher potato yields in northern regions of Europe. In contrast, warmer and more variable climatic conditions with increased occurrence of drought have reduced crop yields in parts of central Europe (53). 

The projections for a range of SRES climate change scenarios show a 30 to 50% increase in suitable area for grain maize production in Europe by the end of the 21st century, including Ireland, Scotland, southern Sweden and Finland (4). Moreover, by 2050, energy crops show a northward expansion in potential cropping area, but a reduction in suitability in southern Europe (5).

Pests and diseases

Between 10 and 16% of global crop production is lost to pests, with similar losses postharvest (10). From an analysis of published observations of 612 crop pests and pathogens it was concluded that the average poleward shift in recorded incidences of these pests and pathogens since 1960 is 2.2 ± 0.8 km/year for the Northern Hemisphere and 1.7 ± 1.7 km/year for the Southern Hemisphere (11). The results indicate significant positive latitudinal shifts for many important groups of crop pests and pathogens. Overall, there has been a significant trend of increasing numbers of pest and pathogen observations at higher latitudes, globally and in both the Northern and Southern hemispheres. For all pests combined, the mean latitudinal shifts were not significant, however, but this seemed to be due to large variability among pest groups. Although recent climate change is implicated as an important driver of these observations, other factors could bias the results. For instance, new crop varieties and agricultural technologies have extended the agricultural margin northward in the USA, and deforestation has increased production in the tropics, thus providing new opportunities for pest invasions at high and low latitudes (11).

Future irrigation water demand

Crop irrigation is responsible for 70% of humanity’s water demand. Globally, the area equipped for irrigation grew six fold to nearly the size of India between 1900 and 2005 (13). This expansion occurred rapidly at a rate of nearly 5% per year during the period 1950s–1980s, but it has slowed down since the late 1990s when the growth rate decreased to <1% per year. For the coming decades, the global area of irrigated land is not expected to expand dramatically due to limited land and water available (14).


For Europe, by the end of the century (2080s: mean of 2069-2099), compared to the present (2000s: mean of 1980-2010), irrigation water demand is projected to decrease for Eastern Europe under scenarios for moderate climate change (12). Under more severe climate change scenarios irrigation water demand in Europe is projected to increase substantially (>20%) (15); according to the IPCC (31) there is high confidence that irrigation demand will increase by more than 40% across Europe. Future irrigation water demand, however, will also be determined strongly by the growing world population and altering lifestyles and dietary habits (15).

Future yield estimates for changes in climate, atmospheric CO2 concentration and technological development

The impact of projected changes in climate, atmospheric CO2 concentration and technological development on crop yield has been studied for 25 EU countries for the period 2041–2064 compared with the period 1983–2006. This has been done for grain maize, potatoes, sugar beet, winter barley and winter wheat, and for a selection of General Circulation Models (GCMs) and three emission scenarios (SRES B1, A1B and A2) that span the range of changes in temperature and precipitation by the mid-21st century (16).


The results suggest that in these countries the negative effects of climate change on crop yields range between 12% and 34% depending on the crop and region. Climate change effects are less pronounced for winter cereals (barley and wheat) as compared to tuber crops (potatoes and sugar beet) or other spring crops (maize). One possible explanation, still subject of further investigation, is the longer vegetative period for winter crops which may allow the winter crops to better cope with extreme events such as drought spells in spring. Also, changes in growing season length due to temperature increase will be relatively smaller in winter as compared to spring crops. The simulations with the driest scenario A1B resulted in the strongest negative influence on yields (16).

The results also suggest that increasing atmospheric CO2 concentration stimulate yields in wheat, barley, sugar beet and potatoes by 14%, 11%, 14% and 7%, respectively. However, most substantial yield changes were projected when considering the effect of technology development. The yield decreasing effect of climate change was compensated and partially superseded when atmospheric [CO2] elevation and technology development were taken into account which is in good agreement with earlier research (17).

For the winter cereals yield increases of 30% and more are projected compared to the baseline for most European regions under the combined impacts of climate change, increasing atmospheric CO2 concentration and technology development. There are small areas on the Iberian and Italic peninsulas were yield decreases are projected compared to the baseline. These declines are mainly due to the pronounced negative climate change effect which could not be compensated for by the positive effects of increasing atmospheric CO2 concentration and technology. For potatoes and sugar beet yield increases are also simulated for most regions in Europe except for some areas in Southern Europe (Italy, Greece and Spain), and few regions in Poland and Finland, but in most of the cases the decreases do not surpass 10% in relation to the baseline period. For grain maize the spatial variability in yield changes ranges between <−30% to >30%. Yield increases are highest in South-western Europe and yield declines are mainly projected for Eastern Europe (16).

Adaptation measures - Overview

Zoning and crop productivity

Changing planting dates, optimisation of crop varieties and planting schedules, improving cultivar tolerance to high temperature, irrigation optimisation and diversification of activities are climate adaptation options for cropping systems summarized by the IPCC (31).


Some predictions foresee a greater potential for overall crop productivity from a longer growing season in some parts of the EU, a northward shift in the cultivable zone, and increased CO2 concentrations in the atmosphere. Increased average temperatures and a longer growing season may offer the opportunity to grow a wider range of crops over a greater area.

Changing crop sowing days may ensure that maturation occurs before peak temperatures and thus reduce possible negative effects on productivity. Growing the most heat resistant cultivars or those that become more suitable for the specific climate— present new opportunities for farmers (31). While a warmer climate poses a risk to some traditional fruit growing practices, opportunities will also be presented to grow new types of fruit.

Floods

Farm-level actions are needed to improve soil drainage to reduce waterlogging and the consequent impacts on stock health. However, improving drainage from fields, by increasing the rate at which water is discharged to streams and rivers may increase the risk of flooding downstream. In consequence adaptation to this risk should focus on disseminating information on minimising the adverse impacts of waterlogging and on recommending farmers move stock from those fields vulnerable to waterlogging.

The majority of adaptation measures proposed would be implemented at the farm level and range from improving soil structure to contour ploughing. Providing ‘breaks’ such as hedges and increasing the area of undrained farm woodlands would help to buffer peak rainfall events, slowing the  movement of water from soil to watercourse. This will help balance the increase in water transfer from soils to watercourses brought about by improved drainage.

Improved on-farm management alone may not fully adapt to the risk; infrastructural adaptation including ‘hard’ defences and drainage systems is likely needed.

Drought, Water Scarcity and Irrigation

Farm level actions such as changing land use in areas that are more susceptible to drought, changing cropping by switching to less water intensive crops, and investing in rain water harvesting equipment are needed. Measures to adapt to the expected decrease in water availability and drought risk may include measures to increase the water-holding capacity of soils (increasing the organic matter content of soils); measures that increase the collection of rainwater over winter to increase the supply for subsequent irrigation; measures to improve the efficiency with which irrigation water is applied.

Earlier sowing, of both Autumn and Spring-sown crops, will result in the maturation phase occurring earlier and before the occurrence of peak temperatures in the summer. Also, crops may be shifted to areas where the climate is more suitable for their cultivation.

If the agriculture industry aims to adapt by increasing irrigation, the water resources necessary may need to be supplied from within the farm. This may be achieved by on-farm rainwater harvesting and establishing small-scale water reservoirs on farmland while improving the efficiency with which irrigation water is used. Irrigation may be used more efficiently by a range of approaches from irrigating at night to use of trickle irrigation.

Government agencies and regulators may provide an incentive for farmers to take action by re-negotiating water abstraction licenses and/or introducing charging/tradable permit schemes to promote efficient use of reduced water resources.

Crop husbandry adaptation measures include intercropping (where available space between rows is used by different crops to allow maximum use of the soil moisture); altering row and plant spacing (to increase root access to available soil moisture); and introducing or changing fallow and mulching practices to retain soil moisture and organic matter (Iglesias et al. 2006). In response to forest fires during summer drought, the introduction and maintenance of firebreaks (where areas are cleared or burnt under controlled conditions) with access to water for fire fighting, will limit fire spread and damage.

Water quality

Water quality may be polluted by fertilizers through increased point-source and diffusive pollution (more runoff). Fertilizer efficiency and application methods need to be improved and farmers should be made aware of best practices regarding the application of manures and fertilizers and the control of soil erosion. The use of buffer strips (hedgerows, vegetative rows) beside water courses can be effective in reducing nutrient leaching.

Glaciers and permafrost

Mountain communities that depend upon melt waters for their domestic and agricultural supply will need to invest in water capture and storage systems to compensate for the projected changes in seasonal water availability that will affect these regions.

Sea-Level-Rise

The threat from rising sea levels is the one that most requires an infrastructural approach. National governments will need to decide the balance between constructing ‘hard’ flood defences and allowing land to be abandoned to inundation.

Pests and diseases

The introduction of resistant or less-susceptible varieties is one approach. To deal with new crop pests a sustainable integrated pesticides strategy should be developed. The use of new pesticides needs to be carefully evaluated with respect to the potential impacts on water quality. Within greenhouses the use of thermostats and rapid cooling may be used to reduce pest and disease infestation. Livestock disease adaptation measures include vaccination of both the domestic and wild populations (31). An increased use of pesticides is expected due to climate change (36).

Livestock

Wetter winters and an increased likelihood of fields remaining waterlogged into spring mean that the housing period of ruminant livestock may need to be increased, with the animals remaining inside for longer in the spring. Hotter summers forecasted may also mean that ruminants need to be housed in summer to reduce problems from heat stress or because pastures may not remain productive during the summer months. The grazing season may be lengthened in autumn and into the early winter period, and therefore may at least partially compensate for the reduced grazing opportunities in early spring and late summer.

Increased temperatures and decreased rainfall in summer are also likely to reduce forage yields, especially on pastures grazed during summer (3). Adaptation measures include growing a new range of forage crops, such as soya, or making increasing use of forage grown during early spring and late autumn. Reduced yields of current forages could also be compensated for by the introduction of more drought and heat resistant forage varieties.

The longer growing season, greater grass production and warmer temperatures all mean that livestock housing costs could be reduced. For ruminants this will be due to a longer growing season, which will enable livestock to graze longer. For carnivores, the reduction in housing costs will be due to a reduced need for heating over winter. A further cost reduction may accrue from the increased potential to grow forage legumes.

The spread of bluetongue virus in sheep across Europe has been partly attributed to climate change (34) through increased seasonal activity of the Culicoides vector (35).

Adaptation potential

Adaptation potential

The adaptation potential of European agriculture in response to climate change has been assessed for a number of crops (29). It was shown that adaptation potential is high for maize and (to a lesser extent) sugar beet and oilseed, and limited for wheat and barley. For instance, maize yields are projected to decline by 9% in 2040 relative to 1975 without adaptation but adaptation has the potential to cut this to just over 1%. Barley yields, on the other hand, are projected to decline by 22% in this period but this loss could be cut to 15% with adaptation.


Under climate change, average farm profits across Europe would increase modestly (1.5%) with adaptation but could decline by 2.3% without adaptation (29). However, warmer regions in southern France, Spain, Italy, Greece and Portugal already beyond the temperature optimum of 16°C could see substantial residual damages from climate change of over 10% even after adaptation. Without adaptation even cooler regions in central France and Germany could see declines in profitability due to warming by 2040. In agreement with several previous studies, the authors found that projected temperature changes are more important than precipitation changes in determining the impacts of climate change over the next few decades (30). They found that the impact of mean temperature change on yield is around 5-10 times larger than the impact of precipitation by 2040; projected precipitation changes tend to be small compared with projected temperature changes. It should be noted, however, that these estimates do not include a number of moderating influences that may limit climate change impacts such as potential yield gains in southern Scandinavia or the CO2 fertilization effect (29).

Autonomous vs planned

Two types of adaptation are generally discriminated (8):

  • autonomous adaptation often occurs at short time-scales and small spatial scales (e.g. farms). Autonomous means that no other sectors (e.g. policy, research) are needed in their development and implementation. Examples of such adjustments are changes in varieties, sowing dates and fertilizer and pesticide use. In particular, in southern Europe, autonomous adaptations may include changes in crop species (e.g. replacing winter with spring wheat, (6)), changes in cultivars and sowing dates (e.g. for winter crops, sowing the same cultivar earlier or choosing cultivars with longer crop cycle; for summer irrigated crops, earlier sowing for preventing yield reductions or reducing water demand) (8). In northern Europe, new crops and varieties may be introduced only if improved varieties will be introduced to respond to specific characteristics of the growing seasons (e.g. length of the day) (4).
  • planned adaptation refers to major structural changes to overcome adversity caused by climate change. This involves changes in land allocation and farming systems, breeding of crop varieties, new land management techniques, etc. It requires longer time than autonomous adaptation and often concerns regions or nations. A different allocation of European agricultural land use seems to represent one of the major planned adaptation strategies available (8).

Adaptive capacity

The ability to adapt agricultural practices is strongly influenced by social and economic factors. Farmers who have been historically exposed to variable climatic conditions, such as in the Mediterranean region, tend to be more prepared to cope with climatic change. Adaptive decisions ought to occur at the farm level in response to local conditions, which makes it impossible to prescribe a single strategy at global level (9).

The world’s cereal producing regions have been identified that are likely to become vulnerable to climate change over the 21st century by identifying those regions that will be [a] exposed to climatic stress and [b] have a limited capacity to adapt (8). Model projections on available soil moisture were made to identify regions likely to be exposed to drought under the SRES A1B and B2 emissions scenarios for the 2050s and 2080s. These regions were compared with model projections of adaptive capacity based on agricultural, meteorological and socio-economic data. These projections were compared with the baseline period of 1990–2005. “Vulnerability hotspots” were identified for wheat and maize, a vulnerability hotspot being defined as a region where both a decline in adaptive capacity and in available soil moisture is projected. The results suggest there are perhaps five wheat and three maize growing regions likely to be both exposed to worse droughts and a reduced capacity to adapt. The “vulnerability hotspots” for wheat are: southeastern USA, southeastern South America, the northeastern Mediterranean, and parts of central Asia. For maize, the suggested vulnerability hotspots are: southeastern South America, parts of southern Africa, and the northeastern Mediterranean. This analysis did not consider the effects of available ground water on adaptive capacity, however (8).

Differences between Eastern and Western Europe

The same scenario of climate change will have different effects on agriculture in Eastern and Western Europe. These differences arise because today agriculture in Eastern Europe is not at the same high level as agriculture in Western Europe, and because the options to adapt to future climate change are not the same in these two regions (55). The big difference of agriculture today between Eastern and Western Europe is illustrated by the difference in agricultural labour productivity: between 2011 and 2013 this productivity in Eastern Europe was only 19% of productivity in Western Europe (56). This is despite investment of approximately 20 billion euro of European Union (EU) and national funds to modernize Eastern European agriculture between 2000 and 2012 (57). Apparently, transition of agriculture in Eastern Europe is a slow process.

Due to these big differences, Eastern and Western Europe do not have the same adaptive capacity or climate response, and thus face different climate change impacts. A farmer in Eastern Europe that is faced with a negative impact on a certain crop, for instance, has fewer options to adapt than a farmer in Western Europe facing the same impact for the same crop. Farmers will continue to adapt to changing circumstances to maximize their profit. This profit-maximization has different outcomes for Eastern and Western Europe. This hypothesis has been tested for changes in temperature and precipitation between now and 2071-2100 under scenarios of a moderate change in climate (55). For this test two assumptions have been assessed:

  1. What if Eastern and Western European regions were to adapt in isolation, not being able to benefit from adaptation options the other region might offer? If agriculture in Eastern and Western Europe were to adapt in isolation, and thus farmers in Eastern and Western Europe could only benefit from adaptation options in their respective regions, this would negatively affect farmers in Eastern Europe. After all, the number of potential adaptation options is smaller in Eastern than in Western Europe: the variation in Eastern European farms is smaller, and agriculture is less developed, modernized, and capital-intensive than in Western Europe (55).
  2. What if farmers in both regions have full access to adaptive capacity in the other region? The results show that if farmers in Eastern Europe have full and easy access to the adaptive capacity of Western Europe, Eastern Europe will respond more positively to changes in climate. Vice versa, having full access to the adaptive capacity of Eastern Europe does not increase the adaptive capacity of Western Europe (55).

Both extremes are not realistic at this moment, however. Adaptation will not take place in isolation. There is an exchange of knowledge and expertise that strengthens adaptation capacity in Eastern Europe. Eastern European countries are continuing to re-adjust their institutions according to Western European templates, and Eastern European farmers have access to EU farm subsidies. The other end of the spectrum, where Eastern Europe gains access to the same level and quantity of adaptation options as Western Europe, is also unrealistic at this moment. Complex behavioural, technical, societal and institutional costs and adjustments at all levels of the society are required to make this happen (58). Even though market principles are now predominant all over the European Union, and Eastern Europe has made a lot of progress to close the gaps, the countries in this region continue to face significant socio-economic setbacks that decrease the countries’ options to respond to the current and future climate (55).

Assessments of future impacts of climate change show that the region with the lowest adaptive capacity, Eastern Europe, suffers the most from climate change. This is because Eastern Europe cannot fully apply the same adaptation options as Western Europe. Autonomous adaptation will not bridge the existing adaptation gap. Planned adaptation in Eastern Europe is needed. The European Union, national governments, and regional policy must attempt to overcome the barriers to adaptation in Eastern Europe and increase Eastern European adaptive capacity by providing more information on adaptation opportunities and climate change, by enlarging the adaptation options and resource inventory and by creating a favourable implementation and management environment, by encouraging knowledge and skills transfer between all European farmers, and by guiding farmers in making efficient adaptation decisions (55). 

Adaptation measures – Risk management policies

Risk management instruments in agriculture, such as crop insurance and disaster assistance programme, and especially how they are designed, will affect incentives to adapt (19). Three types of crop production insurance are: individual yield, area-yield and weather index insurance. In addition to these insurance schemes governments may decide to assist farmers financially after climate extremes that caused a lot of damage to their yields (ex post assistance) (18):


  • Traditional individual-yield crop insurance makes an indemnity payment when the farm incurs a yield loss. This can help to manage production risk but it is known to be expensive and will diminish incentives to adapt to climate change (18).
  • Area-yield crop insurance is a crop insurance scheme in which both indemnities and premiums are based on the aggregate yield of a geographical area. The indemnity equals the difference in value, if positive, between the area yield and some predetermined critical yield level. Participating producers in a given area would receive the same indemnity per insured unit of land, regardless of their own crop yield, and all would pay the same premium rate (20). Under changing climate conditions, area yield insurance would have the advantage of maintaining incentives to adapt (18).
  • Weather index insurance is an insurance scheme where a threshold in the proxy variable marks the point at which payments begin. Once the threshold is reached, the payment increases incrementally as the value of the index worsens. The payment rate is independent of the actual loss incurred by a policyholder (18).
  • Ex post payments are highly variable and can be extremely high in some years (18).

Weather index insurance or area yield insurance, which do not require on-farm verification, can help keep administrative costs down as compared to individual yield insurance, and they do not discourage adaptation since indemnities are paid independently of actual loss incurred by a policyholder. However, they are not a means for structural adaptation. Farmers will incorporate any insurance subsidies or ex post disaster payments to their production decisions, which may favour insurance over crop diversification or other risk management and adaptation strategies (18).

European wheat production

From a study on adverse weather conditions for European wheat production (23) it was concluded that the adaptation strategies must be a compromise between using early-ripening cultivars to avoid stress as much as possible and maintaining a growing season length with the highest possible effective global radiation to sustain current yields or minimize yield decrease. With early-ripening cultivars adverse condition risk can be reduced; shortening the growing season, however, reduces the effective global radiation and therefore yield potential. The authors from this study stress the importance of regionalization of adaptation strategies: in Northern Europe, by using late-ripening cultivars the growing season is longer without the penalty of increased exposure to adverse agroclimatic conditions; in central Europe, by switching to late-maturing cultivars the risk of adverse event frequency significantly increases. They state that diversity of wheat varieties for different regions and season-specific threats should be promoted to enhance climate resilience (26).

Adaptation measures – Specified for agro-climatic zones

Boreal zone

In the Boreal zone, farming will mainly need to adapt to increased rainfall. The rapid removal of water from agricultural land, by increasing stream flow, may increase the risk of flooding downstream, however. Hence there will need to be an assessment of the impacts of any programme to improve farm drainage on the requirement for hard flood defences in vulnerable zones.


The opportunities in the Boreal zone (including the greater area of land available for a range of crops, longer growing seasons and increased temperatures) offer the potential to improve the productivity and/or profitability of all agricultural sectors. Farmers will need access to information on new cultivars and their husbandry in order to maximise those opportunities. Careful consideration also needs to be given to the potential impacts that increasing agricultural production may have on biodiversity and the overall landscape quality.

Atlantic zone

The whole Atlantic zone presents improvements on land availability, longer growing season and higher temperatures. Farmers will need access to information on new farming techniques and species to benefit from those opportunities. Nevertheless, farming in the Atlantic zones will have to adapt to the risks of intensification of winter rainfall as well as reduced summer rainfall and, under warmer conditions, the likely introduction of new pests and disease. Farm-level measures are needed to allow rainwater harvesting and improve drainage to reduce waterlogging while improving crop growth and stock health and reducing the risk of pollution from run-off and fertilizer leaching.

The risk of sea level rise is more pronounced in the Atlantic Central zone where measures will need to be put in place to give up or protect land from salt water intrusion and to improve drainage. The impacts of improved farm drainage and the need for hard flood defences from sea and rainwater flooding in vulnerable zones will have to be assessed.

In the Atlantic South zone adaptations need to prioritise efficiency in the water supply. Improving water supplies, introducing less water-demanding crops and screening fruit and orchard crops from direct sunlight are possible farm-level measures. Potential risks (heat waves) and opportunities (rise of forage productivity) can be anticipated for livestock and more shade and shelter will be needed to avoid heat stress. Using woodland for this will provide co-benefits by increasing rainfall retention in soils and therefore help reduce the risk of winter flooding and run-off.

Continental zone

Adaptation to winter flooding and summer drought by the agricultural sector is a top priority in the Continental North zone. Farm level measures to capture additional winter rainfall will reduce flood and water quality risk and allow farmers to respond to summer drought. Changing to new cultivars and different crop varieties at farm level will allow farmers to make the most of increasing temperatures and CO2.

The greatest risks in the Continental South zone are likely to be a decrease in water supply due to a decline in annual rainfall, reduced crop yields and increased heat stress to livestock. The priorities for adaptation measures will be to identify suitable new crops and new cultivars that can be grown in place, or in combination with, those currently cultivated. Priority should be given, by farmers, to conserving water on their farms to provide a source for irrigation and to apply efficient irrigation schemes.

Alpine zone

Farming will need to adapt to an intensification of winter rainfall and altered hydrological cycles in rivers, as well as flash floods and summer drought. Farm level measures are needed to improve natural buffering to reduce erosion and landslides. Drainage to reduce waterlogging is also an important measure. Flood prevention plans may need to be put in place along with the appropriate infrastructure. Win-win measures include the collection of winter rainfall for summer irrigation. Again, in this area, longer growing season and higher temperature offer the possibility to improve the productivity and profitability of agriculture.

Mediterranean zone

Farming will need to adapt to both drought stress and heat stress and the subsequent losses in yield and earnings. Farm level agro-forestry so as to provide shade for animals and nocturnal irrigation for crops will need to be implemented at farm level. In this region, farming will need to adapt to a hotter, drier climate that will increase demand for reduced water resources. While adaptive measures can be taken by farmers themselves, particularly with regard to harvesting and storing water for efficient irrigation, national bodies need to provide information and advice on a range of potential measures. These include new crops and cultivars, soil and husbandry requirements for new cultivars and integrated strategies to deal with the new pest and disease problems likely to be encountered.

The priorities in the southern areas of the Mediterranean are measures to face increased summer drought and its subsequent impacts—crop drought stress, livestock heat stress and reduced forage yield in combination with loss of agricultural land to sea level rise are all high priority in the Mediterranean South zone. As no opportunities have

been identified in this zone, and therefore cannot be used to compensate against the risks, it is paramount that adaptive measures against the risks identified—such as mechanical ventilation for livestock and drought resistant crops—are adopted at farm level with adequate support at the sectoral level.

References

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. Iglesias et al. (2012)
  2. Carter and Saarikko (1996); Maracchi et al. (2004); Porter and Semenov (2005); Tubiello et al. (2007), all in: Iglesias et al. (2012)
  3. Howden et al. (2007), in: Iglesias et al. (2012)
  4. Hildén et al. (2005); Olesen et al. (2007), in: Bindi and Olesen (2011)
  5. Schröter et al. (2005), in: Bindi and Olesen (2011)
  6. Minguez et al. (2007), in: Bindi and Olesen (2011)
  7. Olesen et al. (2007), in: Bindi and Olesen (2011)
  8. Fraser et al. (2013)
  9. Reidsma et al. (2009), in: Teixeira et al. (2013)
  10. Flood (2010); Oerke (2006); Chakraborty and Newton (2011), in: Bebber et al. (2013)
  11. Bebber et al. (2013)
  12. Wada et al. (2013)
  13. Freydank and Siebert (2008), in: Wada et al. (2013)
  14. Faurès et al. (2002); Turral et al. (2011), both in: Wada et al. (2013)
  15. Fischer et al. (2007); Pfister et al. (2011), both in: Wada et al. (2013)
  16. Angulo et al. (2013)
  17. Ewert et al. (2005), in: Angulo et al. (2013)
  18. Antón et al. (2013)
  19. Collier et al. (2009), in: Antón et al. (2013)
  20. Miranda (1991); Barnett et al. (2005), both in: Antón et al. (2013)
  21. Challinor et al. (2014)
  22. Rötter (2014)
  23. Trnka et al. (2014)
  24. FAOSTAT (2012), in: Trnka et al. (2014)
  25. Gourdji et al. (2013), in: Trnka et al. (2014)
  26. Kahiluoto et al. (2014), in: Trnka et al. (2014)
  27. Tai et al. (2014)
  28. Alexandratos and Bruinsma (2012), in: Tai et al. (2014)
  29. Moore and Lobell (2014)
  30. Hawkins et al. (2013); Supit et al. (2012), both in: Moore et al. (2014)
  31. IPCC (2014)
  32. Lobell et al. (2011), in: IPCC (2014)
  33. Avnery et al. (2011a); Avnery et al. (2011b), both in: IPCC (2014)
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  35. Wilson and Mellor (2009), in: IPCC (2014)
  36. Uyttendaele et al. (2015)
  37. Rose et al. (2016)
  38. FAOSTAT (2015)
  39. Lobell and Gourdji (2012)
  40. Craufurd and Wheeler (2009)
  41. Ruosteenoja et al. (2016)
  42. Engen-Skaugen and Tveito (2004); Brewer et al. (2007); Kellomäki et al. (2008); Linderholm et al. (2008); Jiang et al. (2011); Booth et al. (2012); Dong et al. (2013); Kauppi et al. (2014), all in: Ruosteenoja et al. (2016)
  43. Matzarakis et al. (2007), in: Ruosteenoja et al. (2016)
  44. Linderholm et al. (2008), in: Ruosteenoja et al. (2016)
  45. Spinoni et al. (2015), in: Ruosteenoja et al. (2016)
  46. Peltonen-Sainio et al. (2009); Uleberg et al. (2014), both in: Ruosteenoja et al. (2016)
  47. Grass et al. (2013), in: Ruosteenoja et al. (2016)
  48. Kauppi et al. (2014), in: Ruosteenoja et al. (2016)
  49. Laapas et al. (2012), in: Ruosteenoja et al. (2016)
  50. Odgaard et al. (2011); Eckersten et al. (2014); Nkurunziza et al. (2014), all in: Olesen (2016)
  51. Elsgaard et al. (2012), in: Olesen (2016)
  52. Supit et al. (2010), in: Olesen (2016)
  53. Eitzinger et al. (2013), in: Olesen (2016)
  54. Kristensen et al. (2011), in: Olesen (2016) 
  55. Vanschoenwinkel et al. (2016)
  56. European Commision (2014), in: Vanschoenwinkel et al. (2016)
  57. Erjavec (2012), in: Vanschoenwinkel et al. (2016)
  58. Downing et al. (1997); Tol et al. (2004), both in: Vanschoenwinkel et al. (2016)
  59. Knox et al. (2016)
  60. Challinor et al. (2014), in: Knox et al. (2016) 

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