Terroir 1996 banner
IVES 9 IVES Conference Series 9 Climatic requirements for optimal physiological processes: a factor in viticultural zoning

Climatic requirements for optimal physiological processes: a factor in viticultural zoning

Abstract

[English version below]

Les profils climatiques appropriés pour une activité photosynthétique optimale de la vigne sont déterminés dans différentes régions d’Afrique du Sud et localités à l’intérieur d’une région particulière. La moyenne horaire de température ambiante, vitesse du vent et humidité relative sont calculées pendant les périodes de pré-et post-véraison à partir de données de trois années et de quatre stations météorologiques dans chacune de trois régions viticoles [classées “chaudes” (Stellenbosch et Roberston) et “très chaudes” (Upington) selon les indices d’Huglin et de Winkler]. La période comprise entre 9 et 16 heures pour l’activité photosynthétique maximale est utilisée. La température (25-30°C), vitesse de vent (<4 m/s) et humidité relative (60-70°C) nécessaires à une activité photosynthétique optimale sont surimposés sur les profils climatiques respectifs des différentes régions. L’intensité lumineuse ambiante est acceptée comme étant suffisante. Une variation remarquable du nombre d’heures disponibles pour une photosynthèse optimale apparaît. Basées sur les seuls besoins climatiques, les conditions pour la photosynthèse seraient les meilleures dans la région de Robertson. Dans les deux autres régions, la photosynthèse serait limitée à un plus haut niveau, en raison de basses températures. en période de pré-véraison et de vents forts en période de pré-et post-véraison dans la région de Stellenbosch et en raison de températures élevées et faibles humidités pendant les périodes de pré-et post-véraison dans la région d’Upington. Les conditions climatiques pour la croissance seraient meilleures dans la région de Robertson, suivies d’Upington et Stellenbosch. Les conditions climatiques à l’intérieur d’une région particulière peuvent également varier remarquablement sur des distances très courtes, spécialement dans la Province occidentale du Cap, tandis que des régions peuvent être de climats semblables malgré des altitudes, expositions et distances à l’océan différentes. Les localités diffèrent beaucoup selon leurs possibilités à subvenir aux besoins de la photosynthèse. Les profils climatiques des différentes régions et localités peuvent évidemment avoir de sérieuses implications sur le bon fonctionnement physiologique de la vigne et l’impact de ce stress climatique potentiel (direct ou indirect) sur les processus physiologiques semblerait être un facteur à considérer dans le zonage viticole.

 

The suitability of climatic profiles for optimal grapevine photosynthetic activity in different South Afiican regions and in localities within a particular region was determined. Three-year hourly mean ambient temperature, wind speed and relative humidity data from four weather stations in each of three viticultural regions [“hot” (Stellenbosch and Robertson Regions) and “very hot” (Upington Region) classification according to Huglin and Winkler indices] were averaged during the pre- and post-véraison growth periods. A period between 09:00 and 16:00 for maximum photosynthetic activity was used. Temperature (25-30 °C), wind speed (< 4 m/s) and relative humidity (60 – 70 %) requirements for optimal photosynthetic activity were superimposed onto the respective regional climatic profiles. Ambient light intensity was accepted as being sufficient. Marked variation in number of heurs available for optimal photosynthesis occurred. Based on climatic requirements only, conditions seemed best suited for photosynthesis in the Robertson region. In the other two regions, photosynthesis would be reduced to a higher extent, due to low pre-véraison temperature and strong pre- and post­véraison wind (Stellenbosch) and high pre- and post-véraison temperature and low humidity (Upington). Climatic conditions for growth seemed best in Robertson, followed by Upington and Stellenbosch. Conditions within a particular region may also vary markedly over very short distances, especially in the Western Cape, whereas other locations may be climatically similar in spite of differences in altitude, aspect and distance fom the sea. The locations differed markedly regarding their feasibility to support photosynthesis. Evidently, climatic profiles in different regions and locations may have serious implications for proper physiological functioning of grapevines and the impact of potential climatic stress (direct and indirect) on physiological processes would seem to be a factor for consideration in viticultural zoning.

DOI:

Publication date: February 15, 2022

Issue: Terroir 2002

Type: Article

Authors

J.J. HUNTER and V. BONNARDOT

ARC Institute for Fruit, Vine and Wine & ARC Institute for Soil, Climate and Water, Private Bag X5026, 7599 Stellenbosch, South Africa

Contact the author

Keywords

Vigne, climat, zonage, physiologie, photosynthèse
Grapevine, climate, zoning, physiology, photosynthesis

Tags

IVES Conference Series | Terroir 2002

Citation

Related articles…

Influence of agronomic practices in soil water content in mid-mountain vineyards

In the context of LIFE project MIDMACC (LIFE18 CCA/ES/001099), several pilots have been installed in vineyards in mid mountain areas of Catalonia (NE Spain) to test well stablished agronomic practices to increase the adaptation of Mediterranean mid mountain to climate change. Soil water content (SWC) at three different depths (15, 30 and 45cm) was measured in continuum from August 2020. One pilot (WC) included a well-established green cover (GC), a new GC (NC) and a conventional soil management (CM, tilling+herbicides). NC presented an intermediate state between WC and CM, responding similarly to CM in autumn but quickly reaching similar SWC to WC, then following the same evolution till next spring, with CM presenting lower values along autumn and winter. Then vegetation activation decreased SWC in all plots, (much slower in CM, lacking GC). Sensibility to spring rains is again intermediate for NC, which joins SWC evolution of CM by the end of spring till next autumn. It is expected that NC will resemble WC more and more as its GC develops. In the pilot combining vine training (VSP vs Gobelet) and hillside management (slope vs terrace), no clear pattern could be related with these conditions. However, both terraces seem to be more sensitive to spring rains. A third pilot included new vineyards (7 and 1 year old). In the new vineyard (N), higher canopy development, a spontaneous green cover and row straw resulted in a slower SWC dynamic, not so sensitive to rains but conserving more soil water in spring and most of summer, even with presumably a higher water extraction by vines. In the newest vineyard (VN) the deepest sensor is still sensitive to rain events all over the year and SWC is always highest at this depth, revealing small water capture by vines.

Characterization of variety-specific changes in bulk stomatal conductance in response to changes in atmospheric demand and drought stress

In wine growing regions around the world, climate change has the potential to affect vine transpiration and overall vineyard water use due to related changes in atmospheric demand and soil water deficits. Grapevines control their transpiration in response to a changing environment by regulating conductance of water through the soil-plant-atmosphere continuum. Most vineyard water use models currently estimate vine transpiration by applying generic crop coefficients to estimates of reference evapotranspiration, but this does not account for changes in vine conductance associated with water stress, nor differences thought to exist between varieties. The response of bulk stomatal conductance to daily weather variability and seasonal drought stress was studied on Cabernet-Sauvignon, Merlot, Tempranillo, Ugni blanc, and Semillon vines in a non-irrigated vineyard in Bordeaux France. Whole vine sap flow, temperature and humidity in the vine canopy, and net radiation absorbed by the vine canopy were measured on 15-minute intervals from early July through mid-September 2020, together with periodic measurement of leaf area, canopy porosity, and predawn leaf water potential. From this data, bulk stomatal conductance was calculated on 15-minute intervals, and multiple regression analysis was performed to identify key variables and their relative effect on conductance. Attention was focused on addressing multicollinearity and time-dependency in the explanatory variables and developing regression models that were readily interpretable. Variability of vapor pressure deficit over the day, and predawn water potential over the season explained much of the variability in conductance, with relative differences in response coefficients observed across the five varieties. By characterizing this conductance response, the dynamics of vine transpiration can be better parameterized in vineyard water use modeling of current and future climate scenarios.

austrianvineyards.com: online viewer of all designations of Austrian wine

To digitally record and present all the origins of Austrian wines in the same perfect and clear way was the motivation for the Austrian Wine Marketing Board (Austrian Wine) to start with the project in 2018. In June 2021 the results were presented to the public in an online viewer showing all the designations of Austrian wine, available at https://austrianvineyards.com in a largely barrier-free manner. The online viewer provides tailored individual maps fitted to the respective zoom level. The smallest unit of wine-origins in Austria is called Ried and is displayed in a plot-specific manner highlighting areas under vine. Information on the Ried include administrative district, winegrowing municipality, cadastral municipality, large collective vineyard site, specific winegrowing region, generic winegrowing region, winegrowing area and, in many cases, an illustrative picture. Complementary data on the size, elevation (minimum-maximum), orientation (in 8 sectors plus flat) and gradient (minimum, maximum, average) are based on the area under vine according to the EU’s Integrated Administration and Control System. Additional information covers climate data. The diagrams are taken from the monthly breakdown of data in the annals of the Central Institute for Meteorology and Geodynamics, Austria provide a display of values for air temperature, precipitation, and sunshine hours for the reference year and the long-term average. Seasonal aggregated data on temperature, precipitation, and sunshine hours complete the display. Short descriptions with emphasis on geology and soil, field name in historical maps, etymology of the denomination, and main planted variety complements the available information for the main designations in the online viewer. These descriptions are compiled by winegrowers, geologists, historians, and journalists. All the information and data can be extracted to a pdf-file. Printed vineyard maps are also available. Missing content regarding wine origins in Styria will be completed in winter 2021/22.

Late frost protection in Champagne

Probably one of the most counterintuitive impacts of climate change on vine is the increased frequency of late frost. Champagne, due to its septentrional position is historically and regularly affected by this meteorological hazard. Champagne has therefore developed a strong experience in frost protection with first experiments dating from the end of 19th century. Frost protection can be divided in two parts: passive and active. Passive protection includes all the methods that do not seek to modify the vine’s environment or resistance at the time of frost. The most iconic passive protection in Champagne is the establishment of the individual reserve. This reserve allows to stock a certain quantity of clear wine during a surplus year to compensate a meteorological hazard like frost during the following years. Other common passive methods are the control of planting area (walls, bushes, topography), the choice of grape variety, late pruning, or the impact of grass cover and tillage. Active frost protection is also divided in two parts. Most of the existing techniques tend to modify vine’s environment. Most of the time they provide warmth (candles, heaters, windmills, heating cables…), or stabilise bud’s temperature above a lethal threshold (water sprinkling). The other way to actively fight is to enhance the resistance of buds to frost (elicitors). The Comité Champagne evaluates frost protection methods following three main axes: the efficiency, the profitability, and the environmental impact through a lifecycle assessment. This study will present the results on both passive and active protection following these three axes.

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.