Terroir 2004 banner
IVES 9 IVES Conference Series 9 Climatic zoning of viticultural production periods over the year in the tropical zone: application of the methodology of the Géoviticulture MCC system

Climatic zoning of viticultural production periods over the year in the tropical zone: application of the methodology of the Géoviticulture MCC system

Abstract

L’objectif de cette recherche est le zonage climatique des périodes viticoles de l’année dans la Vallée du São Francisco, région brésilienne productrice de vins située en climat tropical semi-aride. Dans cette région, la production peut être échelonnée sur tous les mois de l’année. La région est placée sur climat viticole à variabilité intra-annuelle, qui correspond aux régions qui, sur des conditions climatiques naturelles, changent de classe de climat viticole en fonction de la période de l’année au cours de laquelle le raisin peut être produit. La méthodologie adoptée est celle du Système de Classification Climatique Multicritères Géoviticole (Système CCM Géoviticole) (Tonietto & Carbonneau, 2004), en utilisant les fonctionnalités de modulation des indices (indices homologues appliqués sur la phénologie locale des cépages). Les indices climatiques viticoles du Système (thermique, nycthermique et hydrique) ont été adaptés aux conditions biologiques du cépage Syrah de la région, qui présente un cycle moyen débourrement-récolte (d-r) de 4 mois. L’étude utilise une base de données climatiques journalières de la période 1976-2002, avec la simulation de 36 récoltes théoriques par an (une récolte théorique a chaque décade), soit un totale de 972 sur l’ensemble de la période étudiée. Ainsi, l’Indice Héliothermique (IH12d) à été calculé sur 4 mois tout au long de l’année. L’Indice de Fraîcheur des Nuits (IF3d) a été calculé sur les 3 décades précédentes la date théorique de récolte (période de maturation). La quantité de pluie en période de maturation (P3d) a également été prise en compte en fonction des effets sur l’incidence de pourriture. Les résultats ont permis de caractériser 3 périodes climatiques viticoles distincts dans l’année : Période “a” – conditions thermiques moins chaudes pendant le cycle d-r pour l’IH12d, conditions nycthermiques (IF3d) plus fraîches et très sec (P3d) en période de maturation ; Période “b” – climat intermédiaire entre la période “a” et “c” pour l’IF3d et l’IH12d et sec à très sec pour P3d (la période “b” peut être subdivisée en 2 sous-périodes : l’une que s’initie en sortant de la période chaude et humide “c”, avec une réserve hydrique utile au niveau du sol, et évolue avec la chute des températures ; et l’autre sous-période qui débute avec l’augmentation des températures et que finie juste avant la rentrée de la période humide “c”) ; Période “c” – Le plus chaud pour l’IF3d et l’IH12d et sub-humide pour P3d. Les résultats montrent que la production de raisin de cuve pour un même cépage présente des caractéristiques potentielles distinctes en fonction des périodes de production “a”, “b” et “c”. D’une façon générale, la période “c” est la plus susceptible a une maturité du raisin incomplète en fonction du risque de pourriture (pluie et température élevée), qui peuvent amener à une récolte avant la complète maturation du raisin. Déjà les périodes “a” et “b” sont les plus aptes a une bonne maturation du raisin. La période “a” est celle qui présente le moindre risque de pluie et des températures les plus fraîches, avec la possibilité du contrôle total de la disponibilité hydrique du sol par l’irrigation. La probabilité d’occurrence des indices climatiques à été caractérisé par décade et par quartile comme information d’aide à la décision (risque ou avantages) des périodes de production. Des études complémentaires, notamment l’estimation de la réserve hydrique potentielle (Indice de Sécheresse – IS) du sol seront développées. On peut conclure que le concept de climat viticole à variabilité intra-annuelle du Système CCM Géoviticole peut être utilisé comme élément de zonage pour l’établissement, dans un même vignoble, des périodes de l’année avec un potentiel climatique supérieur de production de raisin de cuve. Ce critère climatique va être utilisé dans le zonage intégré de la région, notamment avec les facteurs édaphiques.

The objective of this research is the viticultural climatic zoning of the production periods over the year in the São Francisco Valley, a Brazilian grape-growing region located in semi-arid tropical climate. In this region, the production can be spread over all months of the year. The region is situated in climate with intra-annual variability, that corresponds to the regions which, under natural climatic conditions, change the class of viticultural climate according to the period of the year during which the grape is produced. The methodology adopted is that of the Géoviticulture Multicriteria Climatic Classification System (Géoviticulture MCC System) (Tonietto & Carbonneau, 2004), employing the modulation functions of the indices. The viticultural climatic indices of the System have been adapted to the biological conditions of the Syrah variety, which has an average cycle of 4 months from bud burst to harvest (d-r) in the region. The study is based on a daily climate database from 1976 through 2002, simulating 36 theoretic harvests per year (one theoretic harvest at every ten 10 days), amounting to a total of 972 harvests in the whole period covered by the study. In this way, the Heliothermal Index (HI12d) was calculated over 4 months throughout the year. The Cool Night Index (IF3d) was calculated over the 30 days that preceded the theoretic harvest (maturation period). The amount of rain (P3d) in the maturation period was equally been taken into account according to the potential effect of the incidence of bunch rotting. The results have allowed to distinguish 3 climatic viticultural periods during the year: Period “a” – less warm during d-r cycle (IH12d) and for night temperatures (IF3d) and very dry (P3d); Period “b” – intermediate climate between “a” and “c” period for IF3d and IH12d and dry to very dry for P3d (the period “b” can be subdivided into 2 sub-periods: one which starts with the end of the warm and sub-humid period “c”, with a useful water reserve of the soil, and evolves with the fall of the temperatures, and another which starts with the increase of the temperatures and finishes before the sub-humid period “c” returns); Period “c” – the warmest for the IH12d and IF3d, and sub-humid for P3d. The obtained results allow defining the periods “a” and “b”, even with different climatic viticultural potential, as being the most favorable for the production of grapes for wine. The probability of occurrence of the values of the climatic indices (climatic risk or advantages) was characterized at a ten-day level throughout the year. Other index to complement the study will be included, especially the potential water balance of the soil (dryness index – IS). It can be concluded that the concept of the viticultural climate with intra-annual variability of the Géovitivulture MCC System can be used as a zoning element for establishing, in the same vineyard, periods of the year with a higher climatic potential for the production of quality grapes for wine. This climatic criterion will be used in the integrated zoning of the region, especially with the edaphic factors.

DOI:

Publication date: January 12, 2022

Issue: Terroir 2004

Type: Article

Authors

J. Tonietto (1) and A.H. de C. Teixeira (2)

(1) Embrapa – Centre National de Recherche de la Vigne et du Vin – Cnpuv, Rua Livramento, 515 ; 95700-000 – Bento Gonçalves, Brésil
(2) Embrapa – Centre de Recherche du Tropique Semi-Aride – Cpatsa

Contact the author

Keywords

Tropical, intertropical, vin, raisin, qualité, climat avec variabilité intra-annuelle, zonage climatique, Système CCM Géoviticole 

Tags

IVES Conference Series | Terroir 2004

Citation

Related articles…

Anthocyanin profile is differentially affected by high temperature, elevated CO2 and water deficit in Tempranillo (Vitis vinifera L.) clones

Anthocyanin potential of grape berries is an important quality factor in wine production. Anthocyanin concentration and profile differ among varieties but it also depends on the environmental conditions, which are expected to be greatly modified by climate change in the future. These modifications may significantly modify the biochemical composition of berries at harvest, and thus wine typicity. Among the diverse approaches proposed to reduce the potential negative effects that climate change may have on grape quality, genetic diversity among clones can represent a source of potential candidates to select better adapted plant material for future climatic conditions. The effects of individual and combined factors associated to climate change (increase of temperature, rise of air CO2 concentration and water deficit) on the anthocyanin profile of different clones of Tempranillo that differ in the length of their reproductive cycle were studied. The aim was to highlight those clones more adapted to maintain specific Tempranillo typicity in the future. Fruit-bearing cuttings were grown in controlled conditions under two temperatures (ambient temperature versus ambient temperature + 4ºC), two CO2 levels (400 ppm versus 700 ppm) and two water regimes (well-watered versus water deficit), both in combination or independently, in order to simulate future climate change scenarios. Elevated temperature increased anthocyanin acylation, whereas elevated CO2 and water deficit favoured the accumulation of malvidin derivatives, as well as the acylation and tri-hydroxylation level of anthocyanins. Although the changes in anthocyanin profile observed followed a common pattern among clones, such impact of environmental conditions was especially noticeable in one of the most widely distributed Tempranillo clones, the accession RJ43.

Climate ethnography and wine environmental futures

Globalisation and climate change have radically transformed world wine production upsetting the established order of wine ecologies. Ecological risks and the future of traditional agricultural systems are widely debated in anthropology, but very little is understood of the particular challenges posed by climate change to viticulture which is seen by many as the canary in the coalmine of global agriculture. Moreover, wine as a globalised embedded commodity provides a particularly telling example for the study of climate change having already attracted early scientific attention. Studies of climate change in viticulture have focused primarily on the production of systematic models of adaptation and vulnerability, while the human and cultural factors, which are key to adaptation and sustainable futures, are largely missing. Climate experts have been unanimous in recognising the urgent need for a better understanding of the complex dynamics that shape how climate change is experienced and responded to by human systems. Yet this call has not yet been addressed. Climate ethnography, coined by the anthropologist Susan Crate (2011), aims to bridge this growing disjuncture between climate science and everyday life through the exploration of the social meaning of climate change. It seeks to investigate the confrontation of its social salience in different locations and under different environmental guises (Goodman 2018: 340). By understanding how wine producers make sense of the world (and the environment) and act in it, it proposes to focus on the co-production of interdisciplinary knowledge by identifying and foreshadowing problems (Goodman 2018: 342; Goodman & Marshall 2018). It seeks to offer an original, transformative and contrasted perspective to climate change scenarios by investigating human agency -individual or collective- in all its social, political and cultural diversity. An anthropological approach founded on detailed ethnographies of wine production is ideally placed to address economic, social and cultural disruptions caused by the emergence of these new environmental challenges. Indeed, the community of experts in environmental change have recently called for research that will encompass the human dimension and for more broad-based, integrated through interdisciplinarity, useful knowledge (Castree & al 2014). My paper seeks to engage with climate ethnography and discuss what it brings to the study of wine environmental futures while exploring the limitations of the anthropological environmental approach.

Optimizing stomatal traits for future climates

Stomatal traits determine grapevine water use, carbon supply, and water stress, which directly impact yield and berry chemistry. Breeding for stomatal traits has the strong potential to improve grapevine performance under future, drier conditions, but the trait values that breeders should target are unknown. We used a functional-structural plant model developed for grapevine (HydroShoot) to determine how stomatal traits impact canopy gas exchange, water potential, and temperature under historical and future conditions in high-quality and hot-climate California wine regions (Napa and the Central Valley). Historical climate (1990-2010) was collected from weather stations and future climate (2079-99) was projected from 4 representative climate models for California, assuming medium- and high-emissions (RCP 4.5 and 8.5). Five trait parameterizations, representing mean and extreme values for the maximum stomatal conductance (gmax) and leaf water potential threshold for stomatal closure (Ψsc), were defined from meta-analyses. Compared to mean trait values, the water-spending extremes (highest gmax or most negative Ysc) had negligible benefits for carbon gain and canopy cooling, but exacerbated vine water use and stress, for both sites and climate scenarios. These traits increased cumulative transpiration by 8 – 17%, changed cumulative carbon gain by -4 – 3%, and reduced minimum water potentials by 10 – 18%. Conversely, the water-saving extremes (lowest gmax or least negative Ψsc) strongly reduced water use and stress, but potentially compromised the carbon supply for ripening. Under RCP 8.5 conditions, these traits reduced transpiration by 22 – 35% and carbon gain by 9 – 16% and increased minimum water potentials by 20 – 28%, compared to mean values. Overall, selecting for more water-saving stomatal traits could improve water-use efficiency and avoid the detrimental effects of highly negative canopy water potentials on yield and quality, but more work is needed to evaluate whether these benefits outweigh the consequences of minor declines in carbon gain for fruit production.

Influence of a spontaneous cover crop on the vineyard and soil erosion under Mediterranean climate

Sixty five % of the agricultural area of the Basque Country located in the DO Ca Rioja corresponds to vineyards. More than 40% of it has an average slope greater than 10%, which makes it sensitive to erosive processes. Furthermore, it is foreseeable that extreme weather events (storms, hail, extreme heat and cold, etc.) will be favored due to climate change. Cover cropping can mitigate this risk, and therefore the objective of this work is to evaluate the impact that a vegetable cover has on the agronomic behavior of the vineyard, the quality of the grape and soil erosion. For this, a trial has been carried out with a Graciano variety vineyard with a slope between 10% -20% during the years 2020 and 2021. Conventional tillage management in the area has been compared (4-6 passes per year of tillage machinery) versus spontaneous vegetation cover management in the vineyard. This implies not tilling and allowing the grass of the land to colonize the range between the lines of vines, controlling their height through 1-3 mowing passes per year, always trying to affect the surface of the land as little as possible. The vegetative growth, yield and quality of the grape and wine was measured. Furthermore, erosion has been measured using Gerlasch boxes. The yield was lower in the second year of the trial in the cover crop treatment, but erosion was significantly reduced.

Effects of graft quality on growth and grapevine-water relations

Climate change is challenging viticulture worldwide compromising its sustainability due to warmer temperatures and the increased frequency of extreme events. Grafting Vitis vinifera L.