terclim by ICS banner
IVES 9 IVES Conference Series 9 Terclim 9 Terclim 2022 9 Inaugural conferences 9 Climate, Viticulture, and Wine … my how things have changed!

Climate, Viticulture, and Wine … my how things have changed!

Abstract

The planet is warmer than at any time in our recorded past and increasing greenhouse emissions and persistence in the climate system means that continued warming is highly likely. Climate change has already altered the basic framework of growing grapes for wine production worldwide and will likely continue to do so for years to come. The wine sector can continue to play an important role in leading the agricultural sector in addressing climate change. From developing on farm to production to consumer strategies in mitigating aspects that warm our atmosphere, to the wealth of adaptive measures available, the wine industry has and will continue to be at the forefront of these efforts. However, these endeavors will need substantial advances in our scientific knowledge of grapevine growth, productivity, and quality combined with extensive local, terroir-driven, understanding that identifies constraints and opportunities based on regional economies and cultural identities. Finally, it is clear that open access publication is necessary for the timely dissemination of scientific knowledge to other scientists and to the industry.

Introduction

Growing up in the 1970s I became interested in weather and climate while in high school. At the time my teachers were discussing numerous environmental issues, including aspects of climate change. However, the nature of these discussions was quite different than those that we are considering today. In the 1970s climate science was on the fence about whether we were going into an ice age or a warming trend. In a prominent story in the magazine Newsweek (1975) titled “The Cooling World” scientists detailed their concerns about falling global temperatures with terrible consequences for future food production resulting in catastrophic famines worldwide. The article also mentioned that “climatologists were pessimistic that political leaders will take any positive action to compensate for the climatic change.” Sounds familiar, doesn’t it, but today it is for the opposite reason. Another more extensive article came out a year later in National Geographic (1976) with the subtitle “Temperatures change, storm tracks and drought belts shift, as scientists search for answers around the world.” Again, sounds familiar, doesn’t it? In the well-researched article, the author detailed that science was debating whether the world was cooling off and possibly heading into another onset of growing ice sheets and glaciation or was the planet warming irreversibly due to human activities. The major question posed by the article was “what sort of weather will our children and grandchildren know?” I think we see the answer to this question much more clearly today.

As I was heading to college in the late 1980s, the discussion of cooling or warming started to become much clearer. Climate scientists had started to better understand the aerosol effect, whereby sulfur aerosols from the burning of coal from the start of the industrial revolution and the two world wars had contributed to significant cooling during the middle of the 20th century. Climate models from that time were not as advanced as they are today but had started to show that there was real concern for the growing concentrations of greenhouse gases that would warm the atmosphere. Seeing all this unfolding I decided to be an environmental scientist and a climatologist. Needing a dissertation topic for my PhD, I turned to agriculture for my main climatology interests. While many of my professors attempted to direct me to study broadacre crops such as corn, wheat, rice, and soybeans, I had been around wine some and knew that it encompassed so much of life – geography, historical development of civilizations, art, gastronomy, biology, chemistry, economics, geology, soil, climate, etc. – providing a rich agricultural system to study. Looking into the topic further, I found that there were no climate scientists focused on viticulture and wine, and that while the wine industry knew how important weather and climate was, the industry was not looking at it from a climate scientist perspective. The next step was to find where and what to study. Knowing that one needed long-term data for studying climate, I turned to Bordeaux where I knew that there had been records kept over hundreds of years of growing grapes and making wine. As for what to study, my interest turned to trying to understand what aspects of weather and climate influenced vintage productivity and quality, and why certain varieties grew well in some climates but not others.

My research in Bordeaux started with a wealth of data on local and regional weather/climate, grapevine phenology and harvest information on fruit composition and production (e.g., Jones and Davis, 2000). It did not take long to notice that the significant trends in numerous weather factors, especially temperature, were related to trends in many grapevine, fruit, and wine characteristics. This finding piqued my interest on further examining not only the general relationships between growing grapes and wine production and quality, but how a changing climate was influencing the wine industry both in Bordeaux and around the world.

From our early work in this area, it was clear that grapevines were telling us that climate was changing through changes in phenology (Jones and Davis, 2000; Jones et al., 2005a) but that there were also trends in wine quality (Jones et al., 2005b). Furthermore, trends in growing season temperatures had warmed on average 1.3°C during the second half of the 20th century for many of the world’s best known wine regions (Jones et al., 2005b). Additional research looking at other wine regions over a longer period (1901-2018) found that trends averaged 1.4°C for many of the world’s well-known wine regions (Jones, 2019) and that many emerging cool climate regions as far north to 58°N and south to 46°S had warmed on average 1.4°C as well (Jones and Schultz, 2017). In addition, while early climate models had much lower spatial and temporal resolution than we have today, they have been shown to be fairly accurate at what we projected temperatures to be for 2020 (IPCC, 2021).

Recent work by Puga et al. (2022) carried this even more extensively worldwide by examining the general climate characteristics of 813 locations in wine regions during 1959-2018. The research classified the locations into three groups with similar climates and found that temperatures increased, especially in the warmest months of the growing season (99% of the locations), and that daily temperature ranges have decreased largely due to more warming at night than during the daytime. Annual precipitation decreased slightly across all groups, while drier locations got drier and wetter locations got wetter during their respective growing seasons. As a result, higher vapor pressure deficits were seen across all groups and over 93% of the locations examined.

Numerous researchers have followed up our earlier research, confirming many aspects of the relationships between grapevine and climate including widespread trends. Droulia and Charalampopoulos (2022) conducted meta-analysis of scientific publications reporting on viticulture and wine-related impacts in Europe from climate change over the last couple of decades. Their results indicate that increasing trends in temperatures across all regions, declining trends in precipitation in some regions inducing greater water deficits, and shifts in risks from extreme events are the most evident factors. The results highlighted four common themes related to impacts that range from 1) changes in growth characteristics with a longer growing season, earlier phenological timing, more rapid intervals between events, and earlier harvests, 2) to changes in fruit and wine composition and therefore alterations in quality, 3) to varied effects on grapevine yields, and 4) to the expansion of viticulture into regions that were not suitable previously. These impacts have also been documented in other wine regions around the world (Jones et al., 2022).

Others have also helped to fine tune our understanding of the relationships between the grapevine growth characteristics and fruit productivity and quality. García de Cortázar-Atauri et al. (2017) and others have advanced our understanding of the usefulness of quality phenological data to better understand the current distribution of varieties and how more advanced phenological modeling can help us to better understand future climate change impacts. The authors also point to the fact that there is much to be learned about climate’s role in grape composition at harvest and therefore maturity timing. Cameron (2021) found that since grapevine phenology is advancing with increased temperatures, there is often higher sugar concentrations at harvest and/or earlier compressed harvests between cultivars and changes in the synchrony of sugar with other fruit metabolites. Parker et al. (2020) have developed models for both phenology (Grapevine Flowering Véraison [GFV]) and ripeness (Grapevine Sugar Ripeness [GSR]) that help us better understand these relationships and how suitability changes might influence adaptation to new varieties. While these temperature-based models are relatively easy-to-use for predicting flowering, véraison and time to target sugar concentrations (ripeness), I would also argue that these models need to be built with data across more regions with a greater diversity of climate types. Jones et al. (2012) found that only approximately 15% of the worlds wine regions are in traditional Mediterranean climates, while other midlatitude and subtropical dry climates make up roughly 19%, humid subtropical make up close to 24%, and maritime temperate is nearly 13%. Therefore, more climate data across the range of climates that winegrapes are grown in is needed to make these models more universal. In addition, the breath of varieties planted across wine regions needs to be incorporated into these models to be even more applicable. Furthermore, the current prediction error of 6-10 days for phenological events will need to be lowered to be more useful for growers/producers and to better forecast what future changes in climate might bring.

Gambetta and Kurtural (2021), updating the work of Jones et al. (2005b), have asked the important question “are we close to a tipping point” in some of the more traditional wine regions? While both pieces of research indicate that the warming of the last 50 years or more has significantly contributed to increases in average wine quality, ripening relationships and potential wine quality have been shown to be reaching a plateau with concerns for the future. Gambetta and Kurtural (2021) also suggest that fruit-based measures may be better measures of declining fruit quality and tipping points or thresholds under future warming.

Morales-Castilla et al. (2020) have identified that increasing cultivar diversity in wine regions would allow for a measure of adaptation to future climate change as long as broader efforts by society to reduce emissions and avoid higher warming scenarios are realized. Given that there are at least 5000 known varieties grown worldwide and that Robinson et al. (2013) identify 1368 ‘prime’ varieties cultivated around the world for commercial wine production, we have many choices to increase cultivar diversity in wine regions. However, despite the need for increasing the diversity of varieties planted, Anderson and Nelgen (2020) find that the concentration of varieties has increased, where 50% of the world’s plantings are now done with 16 varieties and in new world wine regions it increases to 50% planted to seven varieties.

Still others have helped to further identify potential methods of adaptation with van Leeuwen et al. (2019) strongly suggesting adjusting both plant material and viticultural techniques as climate changes. The authors rightly add that the goal would be to maintain ripening and harvest dates at the end of the season instead of too early, in the warmer part of the summer which disconnects ripening dynamics. In addition, it is recommended that using more drought resistant plant material and modifying training systems to address changing growth characteristics and to consider irrigation where water resources are available and allowed for agricultural use. Santos et al. (2021a, 2021b) provides a summary of the work from a European Union project titled “Clim4Vitis”. This work describes adaptation potential over both the short-term and long-term while noting that there many uncertainties, particularly in the long-term, which could alter the best responses depending on region and specific impacts from climate change. The authors state that unravelling these uncertainties was critical to the sustainable development of the wine industry. Short-term adaptation examples from this research include alterations to canopy management, the application of various sunscreen materials to either the plant or the whole vineyard, supplemental irrigation where available and feasible, focused soil management in warmer and drier conditions, and more integrated pest and disease control at the whole vineyard and region scale (Santos et al., 2021a). The work identifies that the long-term adaptations often require greater structural changes and therefore greater investment, which growers and producers are more reluctant to adopt. These include changes in training systems, alterations in the plant scion and rootstock material, changes in cultivars, and relocation of the vineyard (Santos et al., 2021b).

Naulleau et al. (2021) in a systematic review of adaptation strategies for viticulture has helped to identify that many potential site-specific trade-offs are likely to occur. The authors argue that both scientific and local knowledge is needed to develop better spatial and temporal tools to assess the appropriate adaptations to the local conditions. They highlight the need for more multi-scale studies to identify local constraints and opportunities, but also more in depth and systematic economic studies on the impacts of the various adaptation strategies. One such method to address these needs and better understand what the future might hold, the wine industry could use more work like that of Remenyi et al. (2020) which resulted in a climate atlas for all of Australia. The atlas uses the latest climate projections for Australia’s wine regions and provides growers/producers detailed information about how the climate may change over the near, mid, and long-term time horizons over this century. Having tools like this, that are both regionally focused and built with the best data possible, provides the scientific knowledge base from which management decisions for adaptations can be scaled to local knowledge (Naulleau et al., 2021).

Conclusion

Combined, weather and climate are the most basic and most profound environmental factors in grape growing and wine production. Together they drive the overall suitability for viticulture and matching specific cultivars to individual sites, they largely determine what wine styles can be produced in each area, they drive substantial crop risk factors, and produce vintage variations in production and quality. Historically, wine regions have developed worldwide where the weather and climate were most conducive. But the weather and climates of wine regions vary greatly with some more at the climatic margin, some with warmer days and some with warmer nights (differences in humidity), some drier and some wetter, some with relatively reliable rain during the growing season and others with very little, some being more prone to risk from weather extremes, while others are more equitable and consistent. As such it begs the question: Is there a weather/climate structure that is best suited for a given variety for optimum wine quality and production? Then, within the realm of a changing climate, when and how will these weather/climate structures change beyond what is considered viable for both varieties and regions?

From a climate science perspective, my how times have changed … From the second half of the 20th century to today we have gone from concerns about global cooling due to aerosols to evidence of unequivocal warming in the climate system and changes in numerous aspects of weather and climate (IPCC, 2021). While changing atmospheric concentrations of greenhouse gases are the most evident influence on our warming climate, the sum of human impacts on the Earth’s energy balance from deforestation, desertification, urbanization, and ocean acidification mean that future changes are highly likely. With warming across the Earth’s surface, in the atmosphere, and across the world’s oceans, along with declining amounts of snow and losses in ice mass along with rising sea levels the United Nations’ Intergovernmental Panel on Climate Change estimated that to avoid the worst climate impacts we need to limit warming to 1.5°C by the end of the century, but that to do so the magnitude of emissions reductions need to approach net-zero.

A portfolio of mitigation, adaptation, and geoengineering options will be needed across society writ large to meet the UN’s limits on warming and emissions. Mitigation is necessary to limit further warming, and since agriculture is both part of the problem and part of the solution, on farm mitigation efforts will be needed. For vineyards the greatest opportunity to reduce GHG emissions is the reduction of carbon-based energy sources, followed by managing and reducing nitrogen fertiliser applications, and enhancing soil carbon sequestration. But on farm mitigation measures need to be supported by infrastructure, for example to shift to more renewable energy we need more robust power grids that could store energy more efficiently. Estimates point to needing at least a hundred times more storage by 2040 if we want to shift largely to renewables. On the winery to consumer side, mitigation efforts are most focused on reducing packaging weights but also capturing onsite emissions, developing onsite alternative energy sources, and facilitating more efficient distribution of products. In terms of adaptations in the wine industry, for vineyards most of the conversation is focused on changing to more suitable varieties or moving locations. But this loses site of the myriad adaptations described above that have enormous potential to sustain vineyards and wine production over both short- and long-term time scales. Geoengineering, also known as climate engineering, is the deliberate large-scale processes that would attempt to counteract climate change. Geoengineering is largely focused on solar radiation management and carbon dioxide removal, with most of the IPCC (2021) modelling scenarios relying on some degree of carbon dioxide removal to limit warming below critical limits.

What have we learned in terms of influences from a changing climate on viticulture and wine production? Warming of 1-2°C has occurred in wine regions worldwide since the middle of the 20th century. Changes in extremes are becoming more evident with increases in heat and drought stress, along with an increased risk of wildfires and smoke impacts. Grapevines have also been showing change with earlier phenological events. As such, during warmer late winters and springs, earlier growth has brought greater risk from frost in many regions. Shifts have also moved ripening and harvest into a warmer portion of the summer, accelerating sugar ripening, but disconnecting other ripening clocks, and leading to harvest compression between varieties in many regions. As such ripening profiles (challenges in managing timing of sugar, acid, flavor, and phenolic development) and wine characteristics have changed with wine styles in some regions becoming more full-bodied, fruit-driven, often with higher alcohol.

The planet is warmer than at any time in our recorded past and increasing greenhouse emissions emissions and persistence in the climate system means that continued warming is highly likely. Climate change has already altered the basic framework of growing grapes for wine production worldwide and will likely continue to do so for years to come. Should we be pessimistic or optimistic? From my perspective, life is full of possibilities and to not be optimistic closes the door on the possibilities. As such, the wine industry needs to be diligent, smart, and innovative to build resiliency in our production systems, which will increase our adaptive capacity, and reduce our vulnerabilities to climate change today and into the future. Science has a significant role to play in developing the awareness needed to make smart decisions. First, it is clear that open access publication is necessary for the timely dissemination of scientific knowledge to other scientists and to the industry. Second, we should be challenged to continue to grow more advanced weather and climate studies in viticulture and wine production, developing more robust observation networks, and building models that cover the breadth of varieties and climate types suitable for viticulture and wine production both today and into the future.

Acknowledgment

I wish to thank the many people in the Bordeaux that opened doors for me to gather the data necessary to do my PhD research, which ultimately provided the basis for my entire research and teaching career. I would also like to thank the entire collection of researchers worldwide examining climate aspects of growing grapes and making wine. You have all made my career rich with interactions and brought a wealth of knowledge to our science and to the wine industry.

References

Anderson, K., Nelgen, S. (2020b). Which Winegrape Varieties are Grown Where? A Global Empirical Picture (Revised Edition). Adelaide: University of Adelaide Press.
Cameron, W. (2021). The Effect of Temperature on the Timing of Grapevine Phenology. PhD Dissertation, Faculty of Veterinary and Agricultural Sciences, the University of Melbourne. ORCID iD://orcid.org/0000-0002-4702-2068
Droulia, F.; Charalampopoulos, I. (2022). A Review on the Observed Climate Change in Europe and Its Impacts on Viticulture. Atmosphere 2022, 13, 837. https://doi.org/10.3390/atmos13050837
Gambetta, G. A., & Kurtural, S. K. (2021). Global warming and wine quality: are we close to the tipping point?. OENO One, 55(3), 353–361. https://doi.org/10.20870/oeno-one.2021.55.3.4774
García de Cortázar-Atauri, I., Duchêne, E., Destrac-Irvine, A., Barbeau, G., de Rességuier, L., Lacombe, T., Parker, A. K., Saurin, N., & van Leeuwen, C. (2017). Grapevine phenology in France: from past observations to future evolutions in the context of climate change. OENO One, 51(2), 115–126. https://doi.org/10.20870/oeno-one.2017.51.2.1622
IPCC (2021). Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change [Masson-Delmotte, V., P. Zhai, A. Pirani, S.L. Connors, C. Péan, S. Berger, N. Caud, Y. Chen, L. Goldfarb, M.I. Gomis, M. Huang, K. Leitzell, E. Lonnoy, J.B.R. Matthews, T.K. Maycock, T. Waterfield, O. Yelekçi, R. Yu, and B. Zhou (eds.)]. Cambridge University Press. In press, https://doi:10.1017/9781009157896
Jones, G.V. (2019). The State of the Climate. Proceedings of the 21st GiESCO International Meeting: ‘A Multidisciplinary Vision towards Sustainable Viticulture’ (23-28 June, Thessaloniki, Greece).
Jones, G.V. and Davis, R.E. (2000). Using A Synoptic Climatological Approach to Understand Climate/Viticulture Relationships, International Journal of Climatology, 20:813-837.
Jones, G.V., Duchene, E., Tomasi, D., Yuste, J., Braslavksa, O., Schultz, H., Martinez, C., Boso, S., Langellier, F., Perruchot, C., and G. Guimberteau (2005). Changes in European Winegrape Phenology and Relationships with Climate, XIV International GESCO Viticulture Congress, Geisenheim, Germany, 23-27 August, 2005. 875 pp. Vol.1(23.0-27.8): 55-62.
Jones, G.V., White, M.A., Cooper, O.R., and Storchmann, K., (2005). Climate Change and Global Wine Quality. Climatic Change, 73(3): 319-343.
Jones, G.V., Reid, R., and A. Vilks (2012). Climate, Grapes, and Wine: Structure and Suitability in a Variable and Changing Climate pp 109-133 in The Geography of Wine: Regions, Terrior, and Techniques, edited by P. Dougherty. Springer Press, 255 pp.
Jones, G.V. and H.R Schultz (2017). Climate change and emerging cool climate wine regions. Wine & Viticulture Journal,31(6): 51–53.
Jones, G.V., Edwards, E.J., Bonada, M., Sadras, V.O., Krstic, M.P., and M.J. Herderich. (2022). Climate change and its consequences for viticulture. In Managing Wine Quality: Volume One: Viticulture and Wine Quality (Second Edition). Woodhead Publishing Series in Food Science, Technology and Nutrition, Pages 727-778, ISBN 9780081020678, https://doi.org/10.1016/B978-0-08-102067-8.00015-4.
Morales-Castilla I, García de Cortázar-Atauri I, Cook BI, Lacombe T, Parker A, van Leeuwen C, Nicholas KA, Wolkovich EM. (2020). Diversity buffers winegrowing regions from climate change losses. Proc Natl Acad Sci U S A. 2020 Feb 11;117(6):2864-2869. https://doi:10.1073/pnas.1906731117
Naulleau, A., Gary, C., Prévot, L., Hossard, L. (2021). Evaluating Strategies for Adaptation to Climate Change in Grapevine Production–A Systematic Review. Frontiers in Plant Science, 11. https://www.frontiersin.org/article/10.3389/fpls.2020.607859
National Geographic (1976). What’s Happening to Our Climate? Samuel W. Matthews. November 1976, 150(5): 576-615.
Newsweek (1975). The Cooling World. Science Section, Peter Gwynne with Bureau Reports. April 28, 1975. Page 64.
Parker, A. K., García de Cortázar-Atauri, I., Trought, M. C., Destrac, A., Agnew, R., Sturman, A., & van Leeuwen, C. (2020). Adaptation to climate change by determining grapevine cultivar differences using temperature-based phenology models: XIIIth International Terroir Congress November 17-18 2020, Adelaide, Australia. Guest editors: Cassandra Collins and Roberta De Bei. OENO One, 54(4), 955–974. https://doi.org/10.20870/oeno-one.2020.54.4.3861
Puga, G., Anderson, K., Jones, G.V., Tchatoka, F.D., and W. Umberger (2022). A climatic classification of the world’s wine regions. OENO One, 165–177. https://doi.org/10.20870/oeno-one.2022.56.2.4627
Remenyi, T. A., Rollins, D. A., Love, P. T., Earl, N. O., Bindoff, N. L., Harris R. M. B. (2020). Australia’s Wine Future: A Climate Atlas, Hobart: University of Tasmania. See https://wineaustralia.com/climate-atlas
Robinson, J. Harding, J. Vouillamoz, J. (2013). Wine Grapes: A complete guide to 1,368 vine varieties, including their origins and flavours. Penguin Books Limited, 1280 pages. ISBN: 0141968826, 9780141968827
Santos, J.A.; Fraga, H.; Malheiro, A.C.; Moutinho-Pereira, J.; Dinis, L.-T.; Correia, C.; Moriondo, M.; Leolini, L.; Dibari, C.; Costafreda-Aumedes, S.; Kartschall, T.; Menz, C.; Molitor, D.; Junk, J.; Beyer, M.; Schultz, H.R. (2020). A Review of the Potential Climate Change Impacts and Adaptation Options for European Viticulture. Appl. Sci. 2020, 10, 3092. https://doi.org/10.3390/app10093092
Santos, J.A., and others (2021). Short-term adaptation of European viticulture to climate change: an overview from the H2020 Clim4Vitis action. IVES Technical Reviews vine and wine. https://0.20870/IVES-TR.2021.4637
Santos, J.A, and others (2021). Long-term adaptation of European viticulture to climate change: an overview from the H2020 Clim4Vitis action. IVES Technical Reviews vine and wine. https://10.20870/IVES-TR.2021.4644
van Leeuwen, C.; Destrac-Irvine, A.; Dubernet, M.; Duchêne, E.; Gowdy, M.; Marguerit, E.; Pieri, P.; Parker, A.; de Rességuier, L.; Ollat, N. (2019). An update on the impact of climate change in viticulture and potential adaptations. Agronomy 9(9):514; https://doi.org/10.3390/agronomy9090514

DOI:

Publication date: June 23, 2022

Issue: Terclim 2022

Authors

Gregory V. Jones, PhD 1

Presenting author

1Abacela Vineyards and Winery, Roseburg, Oregon, USA

Contact the author

Keywords

weather, climate, climate change, viticulture, phenology, wine

Tags

IVES Conference Series | Terclim 2022

Citation

Related articles…

Modulation of berry composition by different vineyard management practices

High concentration of sugars in grapes and alcohol in wines is one of the consequences of climate change on viticulture production in several wine-growing regions. In order to investigate the possibilities of adaptation of vineyard management practices aimed to reduce the accumulation of sugar during the maturation phase without reducing the accumulation of anthocyanins in grapes, a study with severe shoot trimming, shoot thinning, cluster thinning and date of harvest was conducted on Merlot variety in Istria region (Croatia), under the Mediterranean climate. Four factors which may affect grape maturation and its composition at harvest were investigated in a two-years experiment; severe shoot trimming applied at veraison when >80% of berries changed colour (in comparison to untreated control), shoot thinning (0 and 30%), cluster thinning (0 and 30%), and the date of harvest (early and standard harvest dates). Shoot thinning had no significant impact on berry composition, despite the obtained reduction in yield per vine. Lower Brix in grapes were obtained with earlier harvest date and if no cluster thinning was applied, although at the same time a reduction in the concentration of anthocyanins in berries was observed in these treatments. On the other hand, if severe shoot trimming was applied when >80% of berries changed colour, a reduction of Brix was obtained without a negative impact on berry anthocyanins concentration. We conclude that in cases when undesirably high sugar concentrations at harvest are expected, severe shoot trimming at 80% veraison may effectively be used in order to obtain moderate sugar concentration in berries together with the adequate phenolic composition.

Upscaling the integrated terroir zoning through digital soil mapping: a case study in the Designation of Origin Campo de Borja

homogeneous zones by intersecting several partial zonings of major factors that influence vineyard growth. Each of them follows specific process from their corresponding disciplines. Soil zoning specifically refers to a Soil Resource Inventory map that has traditionally been generated by conventional soil mapping methods. These methods have shortcomings in reaching fine cartographic and categorical details and involve significant expenses, which undermines their applicability. A new framework named Digital Soil Mapping has introduced quantitative models by statistical techniques to establish soil-landscape relationships and is able to provide intensive scale cartography.

In the present study, a microzoning at 1:10.000 scale is generated from an initial zoning, where the conventional soil map with polytaxic map units is replaced by a new one from digital techniques that disaggregates them. The comparison between the zonings considers a quantitative evaluation of capability for each Homogeneous Terroir Unit by means of the Viticultural Quality Index and its categorization based on its distribution by map. The spatial intersection of both maps gives rise to a confusion matrix in which the flows of class variations after the substitution are assessed.

The results show a five-fold increase in the number of Homogeneous Terroir Units identified and a larger differentiation among them, evidenced by a wider range in the capability index distribution. Both elements are accompanied by an increase in the detection of areas of higher potential within previously undervalued uniform zones.These features are a direct effect of the improvements brought by Digital Soil Mapping techniques and would verify the advantages of their implementation in the Integrated Terroir zoning. Eventually, such new highly detailed terroir units would benefit precision viticulture and sustainable management practices.

Effect of vigour and number of clusters on eonological parameters and metabolic profile of Cabernet Sauvignon red wines

Vegetative growth and yield are reported to affect grape and wine quality. They can be controlled through different techniques linked to vine management. The objective of this research was to determine the effect of vine vigour and number of clusters per vine on physicochemical composition and phenolic profile of red wines. The experiment was carried out during two vegetative cycles, with cv. Cabernet Sauvignon grafted onto Paulsen 1103. Three vine vigour were defined, according to shoot weight at previous harvests, being low, medium and high. Five treatments of number of clusters were used for each vigour, with 15, 22, 29, 36, and 45 clusters per vine. Grapes from all treatments were harvested in the same day from Brix and total acidity criteria. Thirty days after bottling, classical analyzes and phenolic compounds were performed. As results, different responses were obtained from each vintage. In 2020, a dry season from veraison to harvest, grapes and wines obtained from low vigour treatment and 45 clusters per vine was the highest in sugar and alcohol content respectively, while grapes and wines from high vigour and 15 clusters presented the lowest sugar and alcohol content. Total anthocyanins were higher in treatment with low vigour and 15 clusters, while the lowest amounts were found in low vigour with 45 clusters, as well as medium and high vigour with 36 clusters per vine. Total tannins were higher in high vigour with 22 clusters and medium vigour with 29 clusters, while were lower in low vigour with 36 clusters. In 2021, a wet season at harvest, responses were different, and great variations were observed between treatments. As conclusions, yield and vine vigour had strong influence on grape and wine quality, promoting different enological potentials on which can be indicated/used for aging strategies of red and even rosé wines.

Is wine terroir a valid concept under a changing climate?

The OIV[i] defines terroir as a concept referring to an area in which collective knowledge of the interactions between the physical and biological environment (soil, topography, climate, landscape characteristics and biodiversity features) and vitivinicultural practices develops, providing distinctive wine characteristics. Those are perceptible in the taste of wine, which drives consumer preference and, therefore, wine’s value in the marketplace. Geographical indications (GI) are recognized regulatory constructs formalizing and protecting the nexus between wine taste and the terroir generating it. Despite considering updates, GIs do not consider the nexus as a dynamic one and do not anticipate change, namely of climate. Being climate a fundamental feature of terroir, it strongly impacts wine characteristics, such as taste. According to IPCC[ii], many widespread, rapid and unprecedented changes of climate occurred, some being irreversible over hundreds to thousands of years. Climatic shifts and atmospheric-driven extreme events have been widely reported worldwide. Recent climatic trends are projected to strengthen in upcoming decades, whereas extremes are expected to increase in frequency and intensity, forcing wines away from GI definitions. Geographical shifts of viticultural suitability are projected, often moving into regions and countries different from current ones. Some authors propose adaptation in viticulture, winemaking and product innovation. We show evidence of climate changing wine characteristics in the Douro valley, home of 270-year-old Port GI. We discuss herein resist or adapt stances for when climate changes the nexus between terroir and wine characteristics. Using the MED-GOLD[iii] dashboard, a tool allowing for easy visual navigation of past and future climates, we demonstrate how policymakers can identify future moments, throughout the 21st century under different emission scenarios, when GI specifications will likely need updates (e.g., boundaries, varieties) to reduce climate-change impacts.

Projected changes in vine phenology of two varieties with different thermal requirements cultivated in La Mancha DO (Spain) under climate change scenarios

The aim of this work was to analyze the phenology variability of Tempranillo and Chardonnay cultivars, related to the climatic characteristics in La Mancha Designation of Origin, and their potential changes under climate change scenarios. Phenological dates referred to budbreak, flowering, veraison and harvest were analyzed for the period 2000-2019. The weather conditions at daily time scale, recorded during the same period, were also evaluated. The thermal requirements to reach each of these phenological stages were calculated and expressed as the GDD accumulated from DOY=60. Changes in phenology were projected by 2050 and 2070 taking into account those values and the projected temperatures and precipitation, simulated under two Representative Concentration Pathway (RCP) scenarios –RCP4.5 and RCP8.5– using an ensemble of models. The average phenological dates during the period under study were, April 16th ± 6.6 days and April 5th ± 6.0 days for budbreak, May 31st ± 6.0 days and May 27th ± 5.3 days for flowering, July 26th ± 5.6 days and July 25th ± 5.8 days for veraison, and Ago 23rd ± 10.8 days and Ago 17th ± 9.0 days for harvest, respectively, for Tempranillo and Chardonnay. The projected changes in temperature imply an average change in the maximum growing season (April-August) temperatures of 1.2 and 1.9°C by 2050, and 1.6 and 2.6°C by 2070, under the RCP4.5 and RCP8.5 scenarios, respectively. A reduction in precipitation is predicted, which vary between 15% for 2050 under RCP4.5 scenario and up to 30% by 2070 under RCP8.5. The advance of the phenological dates for 2050, could be of 6, 7, 7, and 8 days for Tempranillo and 4, 6, 6 and 9 days for Chardonnay, respectively for budbreak, flowering, veraison and harvest under the RCP4.5 scenario. Under the RCP8.5 emission scenario, the advance could be up to 30% higher.