1. Background of experts and limitations of the study
From 613 people viewing the online survey, 161 participants started and 60 completed it. Of those 60, 55% were self-declared experts for silvoarable agroforestry systems, 27% for silvopastoral agroforestry systems and 18% for systems with hedgerows, riparian buffer strips and windbreaks (SI Fig. 1). With respect to climate zone, 50% of the participants were self-declared experts for central and eastern Europe, 23% for the Mediterranean region and 13% for north-western and northern Europe (SI Fig. 1).
The professional background of the survey participants was science, practice, administration and advising (SI Fig. 2). With respect to the field of expertise (plant production (crops, trees, hedges), livestock, climate or other), the majority of participants were experts for plants (40% exclusively, 43% in combination with other fields of expertise), most (63%) of the participants had more than 10 years of work experience in their field, 25% up to five years and 12% between 6 and 10 years.
In general, there is still comparatively little knowledge about agroforestry. Modern agroforestry systems are sparse and young, which often hinders the conduction of scientific field studies (Luedeling et al., 2016; Sollen-Norrlin et al., 2020). It is therefore different to evaluate, if experts have realistic expectations on the capacity of agroforestry systems to increase climate resilience in the future. The relatively high variability of the ratings and rankings (SI Fig. 3) mirrors this uncertainty.
Survey participants voiced the difficulty to answer the questions in the questionnaire “in such a general type. Climate change affects different plants in a different way (for example fruits and vegetables compared with maize or winter cereals)”. Effects of climate are thought to be “very crop- and system-specific, so difficult to generalize”. We acknowledge this, yet there is a gap in comparative studies in agroforestry (Torralba et al., 2016), arguing for studies attempting to close this gap.
1. Yield and quality of saleable products
Observed and expected climate change effects on yield
The change in yield (defined as the amount of total saleable products), averaged across all agroforestry systems and climate zones, was assessed as 0% in agroforestry systems for both current and expected future climate changes, while a yield loss of -8% (p < 0.001) was currently observed in the corresponding non-wood agricultural systems and expected to be -20% in the future (p < 0.001) (Tab. 1). Hence, experts expect that the difference between agroforestry and non-agroforestry systems in terms of their resilience to climate change impacts will continue to increase. More specifically, experts assume that while non-agroforestry systems will experience greater yield losses, agroforestry systems can accommodate the changes.
Across all climate zones, agroforestry systems were presently observed to show 0% (silvoarable, silvopastoral) to -2% (hedegrows) change in yield due to climate change, while arable, pastoral and hedgeless systems showed a yield decrease of -5% to -10% (p < 0.001) (Tab. 1). In the future, agroforestry systems were expected to show either a small decrease (-5% for silvopastoral systems), no change (0% for silvoarable systems) or a small increase (+5% for hedgerow systems), while all non-agroforestry reference systems were clearly negative (-12% (pastoral), -20% (arable), -30% (hedgeless)) (p < 0.001). Statistically, the difference between hedgerow systems and hedgeless systems was not significant for estimations until 2050 (p = 0.4), despite distinct differences in median value (+5% vs. ‑30%) because of high dispersion and significant differences in the distribution of the two groups.
Yield reductions due to climate change were presently reported in most woodless reference systems in all climate zones and ranged, for the major part, from -5% to -10%, expect of silvopastoral systems in north-western and northern Europe (+1%). In agroforestry systems, observed changes in yield were zero or minor (-5% to +3%). The differences between agroforestry and non-agroforestry systems within a climate zone were statistically significant for all systems with the exception of hedgerows/hedgeless systems in central and eastern Europe, silvoarable/arable systems in the Mediterranean region and silvopastoral/pastoral systems in north-western and northern Europe.
By 2050, the difference between woodless reference and agroforestry systems were expected to be highest in central and eastern Europe, with an expected yield decrease of -20 to -30% in woodless systems compared to -7% to +5% in agroforestry systems. In north-western and northern Europe, yield was expected to be stable in silvoarable and pastoral systems and to increase in silvopastoral (+12%) and hedgerow systems (+8%) while in arable (-15%) and hedgeless (-30%) systems a decrease was expected. In the Mediterranean region, a yield reduction was expected for all agricultural systems (non-wood and agroforestry) except for silvoarable systems, where a slight increase was expected. Again, the differences between agroforestry and non-agroforestry within a climate zone were statistically significant for all systems with the exception of hedgerows/hedgeless systems in central and eastern Europe, silvoarable/arable systems in the Mediterranean region and silvopastoral/pastoral systems in north-western and northern Europe (where they were albeit close to significance, p = 0.0524).
Tab. 1: Presently observed and by 2050 expected effects of climate change on yield in % of yield change (median values with minimum and maximum values in brackets) between non-agroforestry and agroforestry systems in general and between silvopastoral, silvoarable agroforestry and hedgerow systems and their respective non-agroforestry reference systems (across all systems n = 60, (silvo)pastoral n = 16, (silvo)arable n = 33, hedgerows/hedgless systems n = 11). Comparisons between non-agroforestry and agroforestry, present observation and expectation until 2050 and between climate zones are visualized in SI Fig. 3 in the SI.

On an ordinal scale, the majority of present observations of yield changes due to climate change as a whole was clearly negative for non-agroforestry systems (75%, 68% and 73% of experts for pastoral, arable and hedgeless systems, respectively), whereas in agroforestry systems observations were more balanced (for details, see Fig. 3). Future expectations for climate change effects on yield in general were more negative for all systems, in particular for non-agroforestry systems (81%, 84% and 73% for pastoral, arable and hedge-free systems). For agroforestry systems, future yield effects in hedgerow systems were estimated to be more evenly distributed (55% negative, 46% positive) than silvoarable (53% negative, 30% positive) or silvopastoral (64% negative, 21% positive) agroforestry.
The most adverse climate change variable for both present and future yield reductions was identified as being prolonged drought, followed by summer heat waves and – for arable crops in particular – late frost and hailstorms (Fig. 3). The effects were much less pronounced in agroforestry systems, which indicates that experts already observe less yield variability in agroforestry systems and that they expect them to also mitigate the increasing climate change effects in the future. On the other hand, the prolonged vegetation season was seen and expected to have beneficial effects on yield, for both non-agroforestry and agroforestry systems.
Observed and expected climate change impacts on quality of saleable products
For the economic success of farming activities, not only the yield as such but also the quality of the products is relevant, as it affects the price at which they can be sold or (for pastoral systems) the fodder quality and in turn the productivity of the livestock. Under current climate change, the quality of saleable agricultural products was perceived to be minorly reduced (47%, 41%, 70%) or not affected (47%, 55%, 30%) for pastoral, arable and hedgeless systems, respectively. For agroforestry systems most observations were between no effect (80%, 57% and 55% for silvopastoral, silvoarable and hedgegrow systems, respectively) and a small to big increase for hedegrow systems (45%).
Estimations for the quality of saleable products until 2050 showed a more pronounced difference between non-agroforestry and agroforestry systems. For arable and hedgeless systems, 100% of experts expected quality to be severely or minorly reduced, while only 48% and 55% thought so for silvoarable and hedgerow systems, respectively. 26% (silvoarable) and 36% (hedgerow systems) expected small to big increases in quality. A summary of experts’ assessment considering climate change in general and specific climate change variables is visualised in SI Fig. 4 and SI Fig. 5.
The climate variables that were expected to affect product quality are roughly the same as the ones identified for yield quantity. Most detrimental to quality were heavy precipitation events, prolonged drought, late frost, summer heat waves and hail.
Considerations for (silvo)arable systems
Climatic conditions influence the growth and maturity of crops. Strong temperature variations, which are expected to increase in occurrence, are linked to changes in humidity levels, which promote, along wetter climate periods in some European regions, the appearance of plant diseases (IPCC, 2021). Warmer temperatures and prolonged vegetation seasons are expected to enable certain pests to increase in numbers (Skendzic et al., 2021). The combination of these elements threatens quantitative yields as well as the quality of saleable products. Experts of this survey expect that “agroforestry systems will gain advantages in the long run, as new beneficial insects are more likely to establish in sufficiently strong populations thanks to the higher diversity”. Yet, Tosh et al. (2024), based on a Bolean regulatory network parametrized with expert opinion, did not expect higher yield stability due to reduced biotic stress.
With respect to product quality, pest levels are expected to increase, so also the impact on crop quality with more pest damaged crops. The negative impact on yield quality due to elevated CO2 is discussed below (section “climate change variables”); with respect to an increase in pests: An increase in pests and diseases was repeatedly mentioned in experts’ comments of this survey and are also listed as “other variable” in the question about the most influential climate change variable in our questionnaire. This is in alignment with the state-of-the-art in scientific literature; for example with respect to insects. Temperature is seen as the most important environmental factor affecting insect population dynamics. Global climate warming could trigger an expansion of their geographic range, increased overwintering survival, increased number of generations, increased risk of invasive insect species and insect-transmitted plant diseases, as well as changes in their interaction with host plants and natural enemies (Skendzic et al., 2021).
Considerations for (silvo)pastoral systems
Several experts voiced that “for animal products, welfare and free-range are very important and shade is absolutely necessary. […] Heat stress is devastating for quality. With trees as ‘field pharmacy’, veterinary treatments and antibiotics can be phased out or minimised, this also improves quality […]”. Animal welfare was emphasized by many comments. Yield of grasslands is already being reduced due to drought events. Again, these effects could be buffered in silvopastoral systems through environmental services provided by agroforestry, such as soil erosion protection, temperature and humidity regulation, increased soil fertility and enhancement of the hydrological cycle. Two statements explicitly addressed the applicability of silvopastoral systems: “Changing a treeless pasture to a wood pasture also wouldn't be very difficult” and “agroforestry systems with poultry and fruit trees are certainly an easy and quick system to implement, the results of which can also be seen in the short term”.
A Swiss farmer pointed out that, in his/her opinion, climate change would not have a significant impact on the amount of animal products in Switzerland and that there would probably be no major increase or decrease since there are generally stables for all animals. They are not only kept on open pastures, hence there are ways to protect the animals from hot temperatures. However, he also acknowledged that this incurred costs.
Considerations for systems with(out) hedgerows, windbreaks and riparian systems
Experts stated that “riparian buffer strips, windbreaks and hedgerows would be quite easy to establish” and that these systems “can also give results in the short to medium term, especially in terms of the associated increase in biodiversity that can promote pollination, pest and disease control”.
Our findings for agroforestry systems with hedgerows, windbreaks and riparian buffer strips are statistically limited by the small sample size (n= 11). They show an overall more pronounced difference between hedgeless and hedgerow systems compared to comparisons of arable and silvoarable and pastoral and silvopastoral systems, respectively.
2. Climate change variables
Experts were asked to rank the five most important climate change variables according to their influential power for agricultural production. Prolonged drought, fire, prolonged vegetation season, hail and late frost were considered most influential (Tab. 2). 29% of experts ranked the climate change variables differently for agroforestry systems. They considered that for agroforestry, fire, hail, prolonged vegetation season, late frost and temperature rise are particularly relevant, whereas prolonged drought, being considered the most important climate change variable for agricultural production in general, was not among the top five of climate change variables for agroforestry. This underlines an enhanced water-use efficiency in agroforestry, which has been widely reported, by an improved microclimate (i.e. by mitigating weather extremes) with a resulting lower water demand (lower evapotranspiration of the understory crop), enhanced soil quality (i.e. by high fresh organic matter inputs, high microbial diversity and activity, soil aggregate formation), leading to increased water storage (Rolo et al., 2023).
Some experts used the option “other variable” to specify not-listed climate change variables and named rainfall decrease/annual rainfall distribution, pests and diseases, storms/heavy winds and CO2 increase. The increase of the atmospheric CO2 concentration was mentioned a few times in the comments. A researcher from the natural and economic/social sciences emphasized: “For future projections, it is crucial to account for the atmospheric CO2 fertilization effect. If this is not included, future simulations are likely to show greater yield decrease compared to e.g., simulations that account for atmospheric CO2. In other words, it has been shown that atmospheric CO2 compensates for any e.g., yield reductions caused by temperature and rainfall change”. The crop response to CO2-fertilisation has been given a medium to high confidence by the IPCC (IPCC, 2007), indicating yield increases in “unstressed” conditions. Long-term studies have confirmed this, showing that potential yield increase can be eliminated by nutrient and water limitation (Ainsworth & Long, 2021; Reich et al., 2014). In addition, higher yields induced by elevated CO2 levels may reduce crop quality, e.g., by lowering protein concentration by higher accumulation of photosynthetic assimilates of C and the decreased root N uptake associated with lower transpiration rate and mass flow (Wang & Liu, 2021). An agronomist from northern Europe pointed out that “under enhanced CO2 levels, in crops, an overall decrease in N and protein concentrations is expected, as well as overall decreases for most macronutrients and micronutrients, while increased temperatures (especially if coupled with drought stress) are often associated with production of smaller, more fibrous leaves, which usually exhibit changes in nutritional quality – for example, decreasing N and increasing tannins and phenols.”
Tab. 2: Ranking of climate change variables in order of importance for their influential power on agricultural production (n= 59) and for agroforestry systems (n = 18) in particular (1 = most influential). The sample size for agroforestry systems was smaller as only experts stating that they would rank these climate change variables differently for agroforestry systems were asked for a specific ranking. The scores represent the means of all given rankings.
|
agricultural production in general
|
specifically for agroforestry systems
|
|
climate change variable
|
score
|
climate change variable
|
score
|
|
prolonged drought
|
1.62
|
fire
|
1.33
|
|
fire
|
1.93
|
hail
|
1.78
|
|
prolonged vegetation season
|
2.20
|
prolonged vegetation season
|
1.94
|
|
hail
|
2.31
|
late frost
|
2.39
|
|
late frost
|
2.37
|
temperature rise
|
2.44
|
|
temperature rise
|
2.64
|
prolonged drought
|
2.61
|
|
heat waves
|
3.16
|
heat waves
|
2.89
|
|
heavy precipitation events
|
3.31
|
heavy precipitation events
|
3.00
|
Agricultural resilience to climate change impacts may occur through i) a reduced exposure to climate variations (e.g., increasing soil organic matter content to reduce the risk of soil erosion from heavy rainfall), ii) a reduced sensitivity to climate variability (e.g., using drought-resistant species and varieties) and iii) an increased adaptive capacity (e.g., increasing the diversity of products) (Smith et al., 2023). Agroforestry systems address all three mechanisms. They reduce the exposure of crops, pasture and livestock through an improved microclimate (reduced wind speed, light intensity and surface runoff) (Jacobs et al., 2022). Woody plants evaporate a large amount of water through their foliage, which cools the temperature around these woody structures (Ellison et al., 2017) and can increase air humidity at the microclimatic level (den Hond-Vaccaro et al. 2025).
3. Approaches to improve resilience to climate change in agroforestry
70% of experts answered the question, to what extent environmental services could buffer the effects of climate change in Europe, with “much” or “very much”. On a seven-point scale from “less effective” (1) to “more effective” (7), 87% of experts rated agroforestry to be a more effective measure than other measures to improve climate resilience (5: 32%, 6: 35%, 7: 20%).
“System design” and “keyline design” were most often named in answers with respect to the question what biophysical measures could enhance climate change resilience in agroforestry systems, followed by “species choice”. Regarding system design, the importance of tree density, tree row orientation, etc., has become common knowledge (e.g., Dupraz et al. (2018); Dupraz et al. (2019)). Sensitivity to climate variability can also be reduced on agroforestry systems by planting adapted varieties of trees and/or crops or variety/crop mixtures. For example, an agronomist from the Mediterranean region expressed a need for “the identification and promotion of suitable tree species and varieties e.g., looking to northern Africa for species suited to an arid environment”. Composite crop populations, representing a high genetic pool, have a high potential for low-input, inhomogeneous conditions found in agroforestry, which has yet to be explored (den Hond-Vaccaro et al. 2024). A greater crop species/variety/crop population diversity also diversifies the land use on a given parcel and at the landscape scale.
A farmer from northern Europe explicitly stated: “We are hoping that the prolonged growing season will bring us new varieties of fruit and nuts, faster growth of trees and new grain varieties – maybe autumn sown. That might increase yields. On the other hand, if the weathers will not favor new, southern fruit varieties or winters are too harsh for new grains, we will have to wait years or decades to have proper cultivars that tolerate new conditions.”