Terroir 2004 banner
IVES 9 IVES Conference Series 9 Method for the evaluation of climatic changes envisaging the protection of grape-growing terroirs: the Géoviticulture MCC system in the evaluation of the potential impact of the construction of hydroelectric power plants on viticulture

Method for the evaluation of climatic changes envisaging the protection of grape-growing terroirs: the Géoviticulture MCC system in the evaluation of the potential impact of the construction of hydroelectric power plants on viticulture

Abstract

[English version below]

La recherche, conduite en 2002, a envisagé l’estimation, a priori, de l’effet du changement mesoclimatique sur le potentiel qualitatif de la région viticole de la Serra Gaúcha (Vallée du Rio das Antas) – Brésil, en fonction de la construction de 3 usines hydroélectriques. Avec une puissance totale de 360 MW, les usines seront opérationnelles entre 2004-2007. La superficie totale d’inondation est de 11,4 km2. La demande des viticulteurs était d’avoir une évaluation des effets d’un éventuel changement climatique en fonction de cette action humaine sur le potentiel viticole de la région. Elle présente climat IS-2 IH+1 IF-1 (humide, tempéré chaud, à nuits tempérées) selon le Système de Classification Climatique Multicritères Géoviticole (Système CCM Géoviticole). Le Système, qui offre plusieurs outils d’aide aux études de zonage vitivinicole à différents échelles, utilise 3 indices climatiques viticoles de référence (Indice de Sécheresse – IS, Indice Héliothermique – IH et Indice de Fraîcheur des Nuits – IF). Ces indices sont représentatifs de la variabilité du climat viticole liée aux exigences des cépages, à la qualité de la vendange (sucre, couleur, arôme) et à la typicité des vins. Dans une première étape, l’étude a été développée en utilisant la modélisation climatique numérique avec le modèle RAMS (Regional Atmospheric Modeling System), version 4.3, au niveau meso et macroclimatique dans la région des usines. Quatre situations ont été simulées : vigne au Fond de la Vallée – FV (situation juste à coté de la rivière) – (1) Climat Actuel (CA-FV) et (2) Climat Futur (CF-FV) ; Haut de la Vallée – HV (416 m supérieure en altitude et à une distance horizontale de 102 m para rapport à FV) – (3) Climat Actuel (CA-HV) et (4) Climat Futur (CF-HV). Le CF représente la situation de plus fort impact potentiel, où la superficie a être inondée sera la plus grande. Egalement, une étude de l’évolution du changement climatique à partir de la rivière jusqu’à la disparition de ces effets dans la région a été conduite. Les variables climatiques concernent les températures (minimale, maximale et moyenne), pluie, Rg, insolation, humidité de l’air e vitesse du vent ont été modélisées au pas de temps mensuel. L’évapotranspiration potentielle (ETP Penman) a été calculée. Par la suite, les indices IH, IF et IS ont été calculés, avec l’utilisation des fonctionnalités du Système, soit pour CA, soit pour CF dans les situations FV et HV. Les résultats ont montré que le climat viticole ne change pas de classe dans le climat futur. Pour l’IH au fond de la vallée, la valeur de 2.488 (CA-FV) passe à 2.483 dans le scénario futur (CF-FV). En haut de la Vallée, l’IH passe de 2.451 (CA) à 2.443 dans CF. Pour l’IF on ne constate pas un changement climatique pour la période de référence de l’indice (moi de mars), sauf pour la période de décembre à février, avec une augmentation de 0,1 à 0,2 ºC dans le climat futur pour les deux situations (FV et HV). L’IS présente des valeurs entre 4 à 6 mm supérieurs dans le climat futur en comparaison avec CA, soit pour FV ou HV. Le résultat est fonction surtout d’une précipitation un peut plus élevé et d’une ETP un peut plus faible dans le climat futur. L’étude a permis d’estimer que la construction des 3 usines hydroélectriques ne changera pas le macroclimat, mais devra causer un changement au niveau du climat local (topoclimat), en fonction d’une augmentation de l’IS et de la réduction de l’IF, restreint aux zones internes (coteaux de la Vallée du Rio das Antas). Le changement tend à zéro quand on s’éloigne de la vallée (plus de 1000 m de distance la rivière). Ce changement est potentiellement négatif vis-à-vis des caractéristiques qualitatives du raisin. Par contre, il est de très faible intensité. Une cartographie en 3D de la région des usines, avec la superficie a être inondé, a été saisie. Une suivie des conditions climatiques de longe terme est en cours envisageant l’évaluation du changement climatique réel et son influence sur la viticulture.

The research, conducted in 2002, has aimed at estimating, a priori, how the mesoclimatic change, conditioned by the construction of 3 hydroelectric power plants, will affect the qualitative potential of the grape-growing region of the Serra Gaúcha (Rio das Antas Valley), Brazil. The power plants will begin to operate between 2004 and 2007, and their total capacity will amount to 360 MW. The total inundation surface will be 11,4 km2. The vine growers requested to get an idea about how a possible climatic change, caused by this man-made action, could affect the vineyard potential of this region. According to the Géoviticulture Multicriteria Climate Classification System (Géoviticulture MCC System), the region has the climate IS-2 IH+1 IF-1 (“humid, temperate warm, with temperate nights”). The system, which offers several tools for viticultural zoning studies on different scales, employs 3 viticultural climatic indices of reference (Dryness Index – IS, Heliothermal Index – IH, and Cool Night Index – IF). These indices are representative of the variability of the viticultural climate related to the requirements of the grape varieties, the quality of the grapes (sugar, color, flavor) and the characteristics of the wines. In a first stage of the study, numerical climatic modeling with the RAMS (Regional Atmospheric Modeling System), version 4.3, was employed at the meso- and macroclimatic level in the region of the power plants. Four situations were simulated: vineyard at the foot of the valley – FV – (location right at the riverbanks) – (1) Current Climate (CA-FV) and (2) Future Climate (FC-FV); at the top of the valley – HV – (416m higher and at a horizontal distance of 102m in relation to FV) – (3) Current Climate (CA-HV) and (4) Future Climate (CF-HV). The CF demonstrates the situation with the strongest potential impact where the surface to be flooded is the largest. Equally, a study on the evolution of the climatic change was conducted starting from the river up to the disappearance of these effects in the region. The climatic variables, concerning the temperatures (minimum, maximum and average), rain, Rg, insolation, air humidity and speed of the wind were modeled at a monthly rate. The potential evapotranspiration was calculated. In the following, the indices IH, IS and IF were calculated, using the functions of the System, for CA as well as for CF in the situations FV and HV. The results have shown that the viticultural climate does not change class in the future climate. For IH at the foot of the valley, the value 2.488 (CA-FV) changes to 2.483 in the future climate (CF-FV). At the top of the valley the IH changes from 2.451 (CA) to 2.433 for CF. In this way, no significative influence on IH was observed. For IF it is not possible to observe a climatic change in the period of reference of the index (March) except for the period from December to February, with an increase of 0,1 to 0,2ºC in the future climate for the two situations (FV and HV). The IS shows values between 4 and 6 mm higher in the future climate when compared with CA, be it for FV or HV. The result is above all a consequence of a slightly higher precipitation and of a slightly weaker ETP in the future climate. The study has allowed to estimate that the construction of the three hydroelectric power plants will not change the macroclimate, but should cause a change at the level of the local climate (topoclimate), as an effect of an increase of the IS and of the reduction of the IF, restricted to internal areas (slopes of the Rio das Antas Valley). The change tends towards zero at a certain distance from the valley (more than 1000m distance from the river). This change is potentially negative for the qualitative characteristics of the grapes. However, it is of very weak intensity. A 3D chart of the power plants region with the surface to be flooded has been produced. A study on the long-term climatic conditions is currently being performed aiming at the evaluation of the real climatic change and its influence on the viticulture.

DOI:

Publication date: January 12, 2022

Issue: Terroir 2004

Type: Article

Authors

J. Tonietto (1), O.L.L. de Moraes (2) et H. Hasenack (3)

(1) Embrapa – Centre National de Recherche de la Vigne et du Vin ; Rua Livramento, 515 ; 95700-000 –
Bento Gonçalves, Brésil
(2) Département de Climatologie, Université Fédérale de Santa Maria – UFSM
(3) Centre d’Ecologie, Université Fédérale du Rio Grande do Sul – UFRGS

Contact the author

Keywords

Qualité, changement climatique, impact climatique, Système CCM Géoviticole, protection des terroirs viticoles

Tags

IVES Conference Series | Terroir 2004

Citation

Related articles…

Influence of climatic conditions on grape composition of Tempranillo in La Mancha DO (Spain)

The aim of this work was to analyze the variability in grape composition of the Tempranillo cultivar related to climatic conditions, in La Mancha Designation of Origin. Grape composition (sugar content, total acidity, pH, malic acid, and total and extractable anthocyanins) recorded during ripening, were analysed for the period 2000-2019. The weather conditions at daily time scale, recorded during the same period, were also evaluated. The relationships between grape parameters with climatic variables related to temperature and to water deficits, referring different periods between phenological events along the growing cycle, were evaluated using regression analysis. High variability in grape composition was observed in the period analysed. Total acidity varied between 3.7 and 7.3 gL-1 while malic acid varied between 1.2 and 4 gL-1. The extractable anthocyanins ranged between 526 and 972 mgL-1, and total anthocyanins ranged between 922 and 1388 mgL-1, being the lowest values recorded in the hottest year (2017). Total acidity decreased 0.77 gL-1 for an increase of 100 GDD, while malic acid decrease in 0.42 gL-1 for the same GDD increase, being the period between veraison and harvest the one that seemed to have higher influence on acidity. In addition, it was confirmed that increasing water deficits decreased acidity. Total and extractable anthocyanins increased in about 210 and 105 mgL-1, respectively, with an increase of 100 GDD from veraison to harvest, and the increase in water deficits favour the increase of anthocyanins, both total and extractable anthocyanins. Total and extractable anthocyanins concentration increased in 35 and 22 mgL-1 per an increase of 10 mm in the water deficit. These results can be of interest to understand the potential changes that grapes composition may suffer under future warmer climates.

Grape must quality and mesoclimatic variability in Fruška Gora wine-growing region, Serbia

The Fruška Gora mountain is a traditional wine-growing region in Serbia situated in the Pannonian Basin. Due to such a position, the vicinity of the Danube River and the presence of concave configuration, it is suitable for grape production. This paper provides analyses of spatial variations in meteorological parameters and grape juice quality within Fruška Gora wine region over three consecutive vintages (2018-2020). The examined period can be defined as warm with cool nights during September (AVG 18,9°C; GDD 1918°C; CI 12°CF) and with the presence of mesoclimatic variability. The East part of the study area was somewhat drier and hotter compared to other parts of the region. The analyses of grape must samples (190 in total) of five cultivars (Cabernet-Sauvignon, Merlot, Chardonnay, Sauvignon blanc and Grašac (Welschriesling)) commonly grown across the region (19 sites), were performed using Fourier Transform Infrared Technology (FTIR). Among all cultivars, Sauvignon blanc was harvested first in the East area (DOY=246±5, GDD at harvest=1552±74, 22.2±0.7 °Brix), while the latest harvest was recorded for Cabernet-Sauvignon in the West (DOY=283±5, GDD at harvest=1936±187, 23.4±1.0 °Brix ). Both the red and white cultivars had higher acidity and YAN in the grape must if the vines were grown in the North and East compared to South and West areas. According to PCA analysis, Grašac showed the lowest variation in grape must chemical composition. Thus, the results confirm that Grašac is the most stable cultivar in Fruška Gora. All monitored cultivars reached technological fruit ripeness by the end of the growing season. However, it was difficult to reach full ripeness of red cultivars, mostly beacuse of uncoupling of technolocical and phenolic ripeness. Thus, Cabernet-Sauvignon had higher variations in GDD sums at harvest compared to other cultivars, which probably increased variations in grape must quality.

Adaptation to soil and climate through the choice of plant material

Choosing the rootstock, the scion variety and the training system best suited to the local soil and climate are the key elements for an economically sustainable production of wine. The choice of the rootstock/scion variety best adapted to the characteristics of the soil is essential but, by changing climatic conditions, ongoing climate change disrupts the fine-tuned local equilibrium. Higher temperatures induce shifts in developmental stages, with on the one hand increasing fears of spring frost damages and, on the other hand, ripening during the warmest periods in summer. Expected higher water demand and longer and more frequent drought events are also major concerns. The genetic control of the phenotypes, by genomic information but also by the epigenetic control of gene expression, offers a lot of opportunities for adapting the plant material to the future. For complex traits, genomic selection is also a promising method for predicting phenotypes. However, ecophysiological modelling is necessary to better anticipate the phenotypes in unexplored climatic conditions Genetic approaches applied on parameters of ecophysiological models rather than raw observed data are more than ever the basis for finding, or building, the ideal varieties of the future.

Impact of climate variability and change on grape yield in Italy

Viticulture is entangled with weather and climate. Therefore, areas currently suitable for grape production can be challenged by climate change. Winegrowers in Italy already experiences the effect of climate change, especially in the form of warmer growing season, more frequent drought periods, and increased frequency of weather extremes.
The aim of this study is to investigate the impact of climate variability and change on grape yield in Italy to provide winegrowers the information needed to make their business more sustainable and resilient to climate change. We computed a specific range of bioclimatic indices, selected by the International Organisation of Vine and Wine (OIV), and correlated them to grape yield data. We have worked in collaboration with some wine consortiums in northern and central Italy, which provided grape yield data for our analysis.
Using climate variables from the E-OBS dataset we investigate how the bioclimatic indices changed in the past, and the impact of this change on grape productivity in the study areas. The climate impact on productivity is also investigated by using high-resolution convection-permitting models (CPMs – 2.2 horizontal resolution), with the purpose of estimating productivity in future emission scenarios. The CPMs are likely the best available option for this kind of impact studies since they allow a better representation of small-scale processes and features, explicitly resolve deep convection, and show an improved representation of extremes. In our study, we also compare CPMs with regional climate models (RCMs – 12 km horizontal resolution) to assess the added value of high-resolution models for impact studies. Further development of our study will lead to assessing the future suitability for vine cultivation and could lead to the construction of a statistical model for future projection of grape yield.

δ13C : A still underused indicator in precision viticulture  

The first demonstration of the interest of carbon isotope composition of sugars in grapevine, as an integrated indicator of vineyard water status, dates back to 2000 (Gaudillère et al., 1999; Van Leeuwen et al., 2001). Thanks to the isotopic discrimination of Carbon that takes place during plant photosynthesis, under hydric stress conditions, it is possible to accurately estimate the photosynthetic activity. Ever since, δ13C has been widely applied with success to zonation, terroir studies and vine physiology research, but is still not widely used by viticulturists. This is quite astonishing by considering the impact of global warming on viticulture and the need to improve water management, that would justify a widespread use of δ13C.
The lack of private laboratories proposing the analysis, the cost of the technology, as well as the long analytical delays, have been detrimental to its development. Some laboratories tried to overcome the analytical difficulties of isotopic analysis by using fourier transformed infrared spectroscopy, as a fast and cheap alternative to the official OIV method (IRMS). These claimed FTIR models have never been published or peer reviewed and cannot be considered robust. In this work, thanks to the recent acquisition of IRMS technology, new modern and robust applications of δ13C for viticulture are proposed. This includes the use of the analysis to make parcel separations at harvesting, the possibility to increase the precision of hydric stress cartography and the potential cost reduction when compared with Scholander pressure bomb analysis.