GiESCO 2019 banner
IVES 9 IVES Conference Series 9 GiESCO 9 GiESCO 2019 9 Climate change 9 The state of the climate

The state of the climate

Abstract

Context and purpose of the study – The climate has warmed over the past century or more bringing about changes in numerous aspects in both earth and human systems. One of these systems, agriculture, is strongly influenced by climate, which largely determines what type, where, and how crops can be grown. Within agriculture, growing grapes and wine production are a sensitive long‐lived specialty crop system where the environmental and economic sustainability of quality production is at risk from a changing climate. As such, this work examines the current state of the climate globally and within wine regions to provide a framework for these changes historically and into the future.

Material and methods – Summaries of global observations and climate model projections are utilized to provide a current state of the climate. Spatial climate data for 22 prominent wine regions worldwide are also used to assess characteristics and trends in annual and growing season temperature and precipitation.

Results – Growing season temperatures across the 22 regions for 1901‐2017 averaged 16.6°C, ranging from 13‐ 15°C in the cooler regions to 19‐21°C in the warmest regions. Over all 22 regions, the average decadal temperature trend during the growing season is 0.12°C while the average change over the entire time‐ period is 1.4°C. While some regions show higher interannual variability and more gradual warming trends, many regions show stronger trends and more rapid warming. Annual temperature changes closely mirror those during the growing season (not shown). For precipitation, the results detail a wide range in year‐to‐year variability in precipitation, with some regions experiencing consistent annual and growing season precipitation amounts while others are much more prone to extreme dry periods. The average percentage of growing season to annual precipitation across these regions is 45%, with those regions lower than average being predominately west coast regions and those with higher percentages being largely in continental climates with greater summertime thunderstorm activity or where greater oceanic influences exist. Precipitation trends for the 22 wine regions are few, following observations globally and in many other wine regions during the last 50 years

DOI:

Publication date: June 19, 2020

Issue: GiESCO 2019

Type: Article

Authors

Gregory V. JONES

Center for Wine Education, Linfield College, 900 SE Baker St, McMinnville, Oregon, USA

Contact the author

Keywords

viticulture, wine, terroir, climate, climate change

Tags

GiESCO 2019 | IVES Conference Series

Citation

Related articles…

Vegetative propagation during domestication – rooting ability of wild grapevines

The origins of plant propagation trace back to the moment of early humans’ transition from a nomadic existence to settled agricultural societies, cultivating their food.

The importance of rural extension and advisory services to achieve a sustainable viticulture in a climate change scenario

A healthy and dynamic agricultural sector is an important foundation of rural development, generating strong bonds to other economic sectors.

How to deal with the Green Deal – Resistant grapevine varieties to reduce the use of pesticides in the EU

With its Farm-to-Fork Strategy, which is a part of the European Green Deal, the European Union aims at reducing the amount of pesticides used in agriculture by 50% until 2030. As viticulture uses around 70% of the fungicides in the EU, there is substantial pressure on winemakers to reduce their pesticide input. On top of the political goal, winegrowers face increased pressure from the public demanding a more sustainable production of wine.

Wine as cultural national heritage: 10 years of the “Vino Bebida Nacional” law in Argentina: review and lessons

Ten years have passed since the enactment and implementation of law no. 26,870 “national drink wine” in Argentina, a pioneering legislation worldwide that seeks to disseminate the cultural characteristics inherent in the production, elaboration, and consumption of wine, as well as its deep-rooted traditions.

Adaptability of grapevines to climate change: characterization of phenology and sugar accumulation of 50 varieties, under hot climate conditions

Climate is the major factor influencing the dynamics of the vegetative cycle and can determine the timing of phenological periods. Knowledge of the phenology of varieties, their chronological duration, and thermal requirements, allows not only for the better management of interventions in the vineyard, but also to predict the varieties’ behaviour in a scenario of climate change, giving the wine producer the possibility of selecting the grape varieties that are best adapted to the climatic conditions of a certain terroir. In 2014, Symington Family Estates, Vinhos, established two grape variety libraries in two different places with distinctive climate conditions (Douro Superior, and Cima Corgo), with the commitment of contributing to a deeper agronomic and oenological understanding of some grape varieties, in hot climate conditions. In these research vineyards are represented local varieties that are important in the regional and national viticulture, but also others that have over time been forgotten — as well as five international reference cultivars. From 2017 to 2021, phenological observations have been made three times a week, following a defined protocol, to determine the average dates of budbreak, flowering and veraison. With the climate data of each location, the thermal requirements of each variety and the chronological duration of each phase have been calculated. During maturation, berry samples have been gathered weekly to study the dynamics of sugar accumulation, between other parameters. The data was analysed applying phenological and sugar accumulation models available in literature. The results obtained show significant differences between the varieties over several parameters, from the chronological duration and thermal requirements to complete the various stages of development, to the differences between the two locations, confirming the influence of the climate on phenology and the stages of maturation, in these specific conditions.