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…

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.

Grapevine xylem embolism resistance spectrum reveals which varieties have a lower mortality risk in a future dry climate

Wine growing regions have recently faced intense and frequent droughts that have led to substantial economical losses, and the maintenance of grapevine productivity under warmer and drier climate will rely notably on planting drought-resistant cultivars. Given that plant growth and yield depend on water transport efficiency and maintenance of photosynthesis, thus on the preservation of the vascular system integrity during drought, a better understanding of drought-related hydraulic traits that have a significant impact on physiological processes is urgently needed. We have worked towards this end by assessing vulnerability to xylem embolism in 30 grapevine commercial varieties encompassing red and white Vitis vinifera varieties, hybrid varieties characterized by a polygenic resistance for powdery and downy mildew, and commonly used rootstocks. These analyses further allowed a global assessment of wine regions with respect to their varietal diversity and resulting vulnerability to stem embolism. Hybrid cultivars displayed the highest vulnerability to embolism, while rootstocks showed the greatest resistance. Significant variability also arose among Vitis vinifera varieties, with Ψ12 and Ψ50 values ranging from -0.4 to -2.7 MPa and from -1.8 to -3.4 MPa, respectively. Cabernet franc, Chardonnay and Ugni blanc featured among the most vulnerable varieties while Pinot noir, Merlot and Cabernet Sauvignon ranked among the most resistant. In consequence, wine regions bearing a significant proportion of vulnerable varieties, such as Poitou-Charentes, France and Marlborough, New Zealand, turned out to be at greater risk under drought. These results highlight that grapevine varieties may not respond equally to warmer and drier conditions, outlining the importance to consider hydraulic traits associated with plant drought tolerance into breeding programmes and modeling simulations of grapevine yield maintenance under severe drought. They finally represent a step forward to advise the wine industry about which varieties and regions would have the lowest risk of drought-induced mortality under climate change.

Assessment of the impact of actions in the vineyard and its surrounding environment on biodiversity in Rioja Alavesa (Spain)

Traditional viticulture areas have experienced in the last decades an intensification of field practices, linked to an increased use of fertilisers and phytosanitary products, and to a more intensive mechanization and uniformization of the landscape. This change in management has sometimes led to higher rates of soil erosion andloss of soil structure, fertility decline, groundwater contamination, and to an increased pressure of pests and diseases. Additionally, intensification usually leads to a simplification of landscapes, of particular concern in prestigious wine grape regions where the economical revenue encourages the conversion of land use from natural habitats to high value wine grape production. To revert this trend, it is necessary that growers implement actions that promote biodiversity in their vineyards. The aim of this study is to assess the impact of the implementation of cover crops, vegetational corridors, dry stone walls and vineyard biodiversity hotspots estimated through the study of arthropods. The work has been carried out in four vineyards in Rioja Alavesa belonging to Ostatu winery, where these infrastructures were implemented in 2020. The presence and diversity of arthropods was studied by capturing them at different times in the season and at different distances from the infrastructure using pit-fall traps in the soil and yellow, white and blue chromatic traps at the canopy level. This is a preliminary study in which all adult insects were sorted to the taxonomic level of order and Coleoptera were classified to morphospecies. The results obtained show that there is a relationship between the basic characteristics of the vineyard and the arthropods captured, with a positive effect, although also dependent on the vineyard, of the presence of infrastructure.

A better understanding of the climate effect on anthocyanin accumulation in grapes using a machine learning approach

The current climate changes are directly threatening the balance of the vineyard at harvest time. The maturation period of the grapes is shifted to the middle of the summer, at a time when radiation and air temperature are at their maximum. In this context, the implementation of corrective practices becomes problematic. Unfortunately, our knowledge of the climate effect on the quality of different grape varieties remains very incomplete to guide these choices. During the Innovine project, original experiments were carried out on Syrah to study the combined effects of normal or high air temperature and varying degrees of exposure of the berries to the sun. Berries subjected to these different conditions were sampled and analyzed throughout the maturation period. Several quality characteristics were determined, including anthocyanin content. The objective of the experiments was to investigate which climatic determinants were most important for anthocyanin accumulation in the berries. Temperature and irradiance data, observed over time with a very thin discretization step, are called functional data in statistics. We developed the procedure SpiceFP (Sparse and Structured Procedure to Identify Combined Effects of Functional Predictors) to explain the variations of a scalar response variable (a grape berry quality variable for example) by two or three functional predictors (as temperature and irradiance) in a context of joint influence of these predictors. Particular attention was paid to the interpretability of the results. Analysis of the data using SpiceFP identified a negative impact of morning combinations of low irradiance (lower than about 100 μmol m−2 s−1 or 45 μmol m−2 s−1 depending on the advanced-delayed state of the berries) and high temperature (higher than 25oC). A slight difference associated with overnight temperature occurred between these effects identified in the morning.

Ecophysiological performance of Vitis rootstocks under water stress

The use of rootstocks tolerant to soil water deficit is an interesting strategy to cope with limited water availability. Currently, several nurseries are breeding new genotypes, but the physiological basis of its responses under water stress are largely unknown. To this end, an ecophysiological assessment of the conventional 110-Richter (110R) and SO4, and the new M1 and M4 rootstocks was carried out in potted ungrafted plants. During one season, these Vitis genotypes were grown under greenhouse conditions and subjected to two water regimes, well-watered and water deficit. Water potentials of plants under water deficit down to < -1.4 MPa, and net photosynthesis (AN) <5 μmol m-2 s-1 did not cause leaf oxidative stress damage compared to well-watered conditions in any of the genotypes. The antioxidant capacity was sufficient to neutralize the mild oxidative stress suffered. Under both treatments, gravimetric differences in daily water use were observed among genotypes, leading to differences in the biomass of root, shoot and leaf. Under well-watered conditions, SO4 and 110R were the most vigorous and M1 and M4 the least. However, under water stress, SO4 exhibited the greatest reduction in biomass while M4 showed the lowest. Remarkably, under these conditions, SO4 reached the least negative stem water potential (Ψstem), while M1 reduced stomatal conductance (gs) and AN the most. In addition, SO4 and M1 genotypes also showed the highest and lowest hydraulic conductance values, respectively. Our results suggest that there are differences in water use regulation among genotypes, not only attributed to differences in stomatal regulation or intrinsic water use efficiency at the leaf level. Therefore, because no differences in canopy-to-root ratio were achieved, it is hypothesized that xylem vessel anatomical differences may be driving the reported differences among rootstocks performance. Results demonstrate that each Vitis rootstock differs in its ecophysiological responses under water stress.