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…

Genotypic variability in root architectural traits and putative implications for water uptake in grafted grapevine

Root system architecture (RSA) is important for soil exploration and edaphic resources acquisition by the plant, and thus contributes largely to its productivity and adaptation to environmental stresses, particularly soil water deficit. In grafted grapevine, while the degree of drought tolerance induced by the rootstock has been well documented in the vineyard, information about the underlying physiological processes, particularly at the root level, is scarce, due to the inherent difficulties in observing large root systems in situ. The objectives of this study were to determine genetic differences in the root architectural traits and their relationships to water uptake in two Vitis rootstocks genotypes (RGM, 140Ru) differing in their adaptation to drought. Young rootstocks grafted upon the Riesling variety were transplanted into cylindrical tubes and in 2D rhizotrons under two conditions, well watered and moderate water stress. Root traits were analyzed by digital imaging and the amount of transpired water was measured gravimetrically twice a week. Root phenotyping after 30 days reveal substantial variation in RSA traits between genotypes despite similar total root mass; the drought-tolerant 140Ru showed higher root length density in the deep layer, while the drought-sensitive RGM was characterised by shallow-angled root system development with more basal roots and a larger proportion of fine roots in the upper half of the tube. Water deficit affected canopy size and shoot mass to a greater extent than root development and architectural-related traits for both 140Ru and RGM, suggesting vertical distribution of roots was controlled by genotype rather than plasticity to soil water regime. The deeper root system of 140Ru as compared to RGM correlated with greater daily water uptake and sustained stomata opening under water-limited conditions but had little effect on above-ground growth. Our results highlight that grapevine rootstocks have constitutively distinct RSA phenotypes and that, in the context of climate change, those that develop an extensive root network at depth may provide a desirable advantage to the plant in coping with reduced water resources.

Current climate change in the Oplenac wine-growing district (Serbia)

Serbian autochthonous vine varieties Smederevka (for white wines) and Prokupac (for rosé and red wines) are the primary representatives of typical characteristics of wines and terroir of numerous wine-growing areas in Serbia. In the past, these varieties were the leading vine varieties, however, as the result of globalization of winemaking and the trend of consumption of wines from widely prevalent vine varieties, they were replaced by introduced international varieties. Smederevka and Prokupac vine varieties are characterized by later time of grape ripening, and relative sensitivity to low temperatures. Climate conditions can be a restrictive factor for production of high-quality grapes and wine and for the spatial spreading of these varieties in hilly continental wine-growing areas.
This paper focuses on the spatial analysis of changes of main climate parameters, in particular, analysis of viticultural bioclimatic indices that were determined for the purposes of viticulture zoning of wine-growing areas in the period 1961-2010, and those same parameters determined for the current, that is, referential climate period (1988-2017). Results of the research, that is, analysis of climate changes indicate that the majority of examined climate parameters in the Oplenac wine-growing district improved from the perspective of Smederevka and Prokupac vine varieties. These studies of climate conditions indicate that changes of analyzed climate parameters, that is, bioclimatic indices will be favorable for cultivation of varieties with later grape ripening times and those more sensitive to low temperatures, such as the autochthonous vine varieties Smederevka and Prokupac, therefore, it is recommended to producers to more actively plant vineyards with these varieties in the territory of the Oplenac wine-growing district.

Deconstructing the soil component of terroir: from controversy to consensus

Wine terroir describes the collectively recognized relation between a geographical area and the distinctive organoleptic characteristics of the wines produced in it. The overriding objective in terroir studies is therefore to provide scientific proof relating the properties of terroir components to wine quality and typicity. In scientific circles, the role of climate (macro-, meso- and micro-) on grape and wine characteristics is well documented and accepted as the most critical. Moreover, there has been increasing interest in recent years about new elements with possible importance in shaping wine terroir like berry/leaf/soil microbiology or even aromatic plants in proximity to the vineyard conferring flavors to the grapes. However, the actual effect of these factors is also dependent on complex interactions with plant material (variety/clone, rootstock, vine age) and with human factors.
The contribution of soil, although a fundamental component of terroir and extremely popular among wine enthusiasts, remains a much-debated issue among researchers. The role of geology is probably the one mostly associated by consumers with the notion of terroir with different parent rocks considered to give birth to different wine styles. However, the relationship between wine properties and the underlying parent material raises a lot of controversy especially regarding the actual existence of rock-derived flavors in the wine (e.g. minerality). As far as the actual soil properties are concerned, the effect of soil physical properties is generally regarded as the most significant (e.g sandy soils being associated with lighter wines while those on clay with colored and tannic ones) mostly through control of water availability which ultimately modifies berry ripening conditions either directly by triggering biosynthetic pathways, or indirectly by altering vigor and yield components. The role of soil chemistry seems to be weakly associated to wine sensory characteristic, although N, K, S and Ca, but also soil pH, are often considered important in the overall soil effect.
Recently, in the light of evidence provided by precision agriculture studies reporting a high variability of vineyard soils, the spatial scale should also be taken into consideration in the evaluation of the soil effects on wines. While it is accepted that soil effects become more significant than climate on a local level, it is not clear whether these micro-variations of vineyard soils are determining in the terroir effect. Moreover, as terroir is not a set of only natural factors, the magnitude of the contribution of human-related factors (irrigation, fertilization, soil management) to the soil effect still remains ambiguous. Lastly, a major shortcoming of the majority of works about soil effects on wine characteristics is the absence of connection with actual vine physiological processes since all soil effects on grape and wine chemistry and sensorial properties are ultimately mediated through vine responses.
This article attempts to breakdown the main soil attributes involved in the terroir effect to suggest an improved understanding about soil’s true contribution to wine sensory characteristics. It is proposed that soil parameters per se are not as significant determining factors in the terroir effect but rather their mutual interactions as well as with other natural and human factors included in the terroir concept. Consequently, similarly to bioclimatic indices, composite soil indices (i.e. soil depth, water holding capacity, fertility, temperature etc), incorporating multiple soil parameters, might provide a more accurate and quantifiable means to assess the relative weight of the soil component in the terroir effect.

Elevational range shifts of mountain vineyards: Recent dynamics in response to a warming climate

Increasing temperatures worldwide are expected to cause a change in spatial distribution of plant species along elevational gradients and there are already observable shifts to higher elevations as a consequence of climate change for many species. Not only naturally growing plants, but also agricultural cultivations are subject to the effects of climate change, as the type of cultivation and the economic viability depends largely on the prevailing climatic conditions. A shift to higher elevations therefore represents a viable adaptation strategy to climate change, as higher elevations are characterized by lower temperatures. This is especially important in the case of viticulture because a certain wine-style can only be achieved under very specific climatic conditions. Although there are several studies investigating climatic suitability within winegrowing regions or longitudinal shifts of winegrowing areas, little is known about how fast vineyards move to higher elevations, which may represent a viable strategy for winegrowers to maintain growing conditions and thus wine-style, despite the effects of climate change. We therefore investigated the change in the spatial distribution of vineyards along an elevational gradient over the past 20 years in the mountainous wine-growing region of Alto Adige (Italy). A dataset containing information about location and planting year of more than 26000 vineyard parcels and 30 varieties was used to perform this analysis. Preliminary results suggest that there has been a shift to higher elevations for vineyards in general (from formerly 700m to currently 850 m a.s.l., with extreme sites reaching 1200 m a.s.l.), but also that this development has not been uniform across different varieties and products (i.e. vitis vinifera vs hybrid varieties and still vssparkling wines). This is important for climate change adaptation as well as for rural development. Mountain areas, especially at mid to high elevations, are often characterized by severe land abandonment which can be avoided to some degree if economically viable and sustainable land management strategies are available.

Inhibition of Oenococcus oeni during alcoholic fermentation by a selected Lactiplantibacillus plantarum strain

The use of selected cultures of the species Lactiplantibacillus plantarum in Oenology has grown in prominence in recent years. While initial applications of this species centred very much around malolactic fermentation (MLF), there is strong evidence to show that certain strains can be harnessed for their bio-protective effects. Unwanted spontaneous MLF during alcoholic fermentation (AF), driven by rogue Oenococcus oeni, is a winemaking deviation that is very difficult to manage when it occurs. This work set out to determine the efficacy of one particular strain of Lactiplantibacillus plantarum(Viniflora® NoVA™ Protect), against this problem in Cabernet Sauvignon must. The work was carried out at commercial scale and in a winery environment and compared the bio-protective culture with the more traditional approach of reducing must pH by the addition of tartaric acid. The combination of both was also investigated. The concentration of both Oenococcus oeni and Lactiplantibacillus plantarum was determined using qPCR. The adventitious Oenococcus oeni showed the most growth during AF in the control wine, whereas in the wines treated with Lactiplantibacillus plantarum a bacteriostatic effect against this species was observed. This effect was comparable to the wines treated with tartaric acid. This has particular commercial relevance for controlling the flora in musts with high pH, or when the addition of tartaric acid is either not permitted or is prohibitive for other reasons.