Terroir 2014 banner
IVES 9 IVES Conference Series 9 International Terroir Conferences 9 Terroir 2014 9 Grape growing climates, climate variability 9 Thermal risk assessment for viticulture using monthly temperature data

Thermal risk assessment for viticulture using monthly temperature data

Abstract

Temperature extremes affect grapevine physiology, as well as grape quality and production. In most grape growing regions, frost or heat wave events are rare and as such conducting a risk analysis using robust statistics makes the use of long term daily data necessary. However, daily climate data suffers many constraints such as typically having a short-term history, with uneven spatial coverage worldwide, and their homogenization to account for changes in climate sensors or changes in site location are challenging. In contrast, monthly data sets offer a much more robust spatiotemporal coverage. Furthermore, data at monthly time steps is relevant for climate projection analyses over the 21st century.

Therefore, the current study evaluates the relevance of estimating thermal risks for viticulture using monthly data. Daily minimum (Tmin) and maximum (Tmax) temperature data were collected from 369 weather stations in Europe (European Climate Assessment & Dataset) and 1218 weather stations in the USA (United States Historical Climatology Network) for the period from 1972 to 2008. For the whole period and for each station, the average yearly number of winter freeze days (Tmin < -17°C), spring frost days (Tmin < -1°C), and heat stress days (Tmax > 35°C) were calculated. In addition, frequencies of years with at least one spring frost event, the date of the last spring frost event at 90% probability (i.e. the quantile 0.9) and frequencies of years with at least one winter freeze event were calculated.

These thermal risk indicators, analyzed on a daily time step, exhibited strong relationships with maximum and minimum monthly average temperatures during the 1972-2008 period. Winter freeze risk is strongly linked to January average monthly minimum temperature, while spring frost risk is related to April minimum monthly temperature. The average number of heat stress days is strongly correlated to July maximum temperature. Using WorldClim 5 arc-minute resolution climate grids, a winter frost risk map for the 1950-2000 period is proposed. The results suggest that grape growing region limits are strongly restrained by winter freeze risk hazards.

DOI:

Publication date: August 10, 2020

Issue: Terroir 2014

Type: Article

Authors

Benjamin BOIS (1), Marco MORIONDO (2) and Gregory V JONES (3)

(1) Centre de Recherches de Climatologie, UMR 6282 Biogéosciences CNRS Université de Bourgogne, 6 boulevard Gabriel, 21000 DIJON, France 
(2) CNR-IBIMET, via G. Caproni 8, 50145, Florence, Italy 
(3) Department of Environmental Studies, Southern Oregon University, 97520,101A Taylor Hall, Ashland, OR, U.S.A.

Keywords

Thermal risks, climate, viticulture, WFR, SFR, HST

Tags

IVES Conference Series | Terroir 2014

Citation

Related articles…

Armenia: historical origin of domesticated grapevine

The Armenian highlands are located on the northern border of western asia and stretch up to the caucasus from the north. Throughout human history, country has played an important role in connecting the civilizations of europe and the near east. The recent large-scale study about the dual domestication origin and evolution of grapes approved that in the Armenian highlands human and grapevine stories are interlaced through centuries and roots of grapevine domestication are found deep in the pleistocene, ending 11.5 thousand years ago. Findings of this study confirmed that glacial episodes distinguish wild grapes into eastern and western ecotypes around 200-400 ka.

Identification of important genomic regions controlling resistance to biotic and abiotic stresses in Vitis sp. through QTL meta-analysis

In the context of global change, the environmental conditions are expected to be more stressful for viticulture. The choice of the rootstock may play a crucial role to improve the adaptation of viticulture to new biotic and abiotic threats (Ollat et al., 2016). However, the selection of interesting traits in rootstock breeding programs is complex because of the combination of multiple targets in a same ideotype. In this sense, the integration of studies about the genetic architecture for desired biotic and abiotic response traits allow us to identify genomic regions to combine and those with interesting pleiotropic effects.

Extraction of pathogenesis-related proteins and phenolics in Sauvignon Blanc as affected by different

The composition of wine is largely determined by the composition of pre-fermentation juice, which is influenced by extraction of grape components. Different grape harvesting and processing conditions could affect the extraction of grape components into juice. Among these grape components, pathogenesis-related (PR) proteins are of great concern for white wine maker as they are the main cause of haze formation in finished white wine. If not removed before bottling, these PR proteins may progress into haze through the formation of complex with phenolics under certain conditions. Thaumatin-like proteins (TLPs) and chitinases are the main constituents of PR proteins found in protein haze.

Water deficit differentially impacts the performances and the accumulation of grape metabolites of new varieties tolerant to fungi

The use of resistant varieties is a long-term but promising solution to reduce chemical input in viticulture. Several important breeding programs in Europe and abroad are now releasing a range of new hybrids performing well regarding fungi susceptibility and producing good quality wines. Unfortunately, insufficient attention is paid by the breeders to the adaptation of these varieties to climatic changes, notably to the increased climatic demand and water deficit (WD). Thus, prior to the adoption of such varieties by the wine industry in Mediterranean regions, there is a need to consider their suitability to WD. This study aimed to characterize the different drought-strategies adopted by 6 new resistant varieties selected by INRAE in comparison to Syrah. To allow the assessment of long-term impacts of WD, field-grown vines were exposed to contrasted WD from 2018 to 2021 under a semi-arid Mediterranean climate. A gradient of WD was applied in the field and controlled through plant measurements at the single plant level. Grape development was non-destructively monitored to determine the arrest of berry phloem unloading. The impacts of WD on berry composition, including water, primary metabolites (sugars, organic acids), secondary metabolites (anthocyanins, thiols precursors) and main cations contents, were assessed at this specific stage. Results showed different varietal responses during the year and inter-annual acclimation in terms of plant water use efficiency, biomass accumulation, as well as yield components and berry composition. WD differentially reduced the accumulation of primary metabolites at plant and berry levels, but it little changed their concentrations in the fruits at the ripe stage. Moreover, WD differentially impacted the accumulation of secondary metabolites and major cations between the varieties. In the talk, we’ll present the main results regarding the WD impacts on fruit metabolites and enlarge the reflection about the practical assessment of the grapevine acclimation to WD.

Winter physiology in a warmer world: Cold hardiness and deacclimation sensitivity drive variation in spring phenology

As the climate warms, the focus of concern in viticulture often turns to how higher temperatures may shift growing regions, change the character of AVAs, and alter fruit quality. However, climate warming is increasing most quickly during the winter dormancy cycle, a critical and often underappreciated portion of the grapevine life cycle. In response to decreasing temperatures and decreasing daylength, grapes initiate a series of physiological changes to enter dormancy, acquire freeze resistance, and time spring phenology such that the growing season begins after threat of frost.