Appliance of climate projections for climate change study in Serbian vineyard regions

Abstract

Climate projections considered here are for two periods in the future throughout two IPCC scenarios: 2001 – 2030 (A1B) and 2071 – 2100 (A2) obtained using Coupled Regional Climate Model EBU-POM. Results are used in calculation of Heliothermal, Drought and Cool Night Index for climate classification of vineyard regions in Serbia. Presented results show significant change of climate in the future, indicating that varieties of grapevine must be adaptable or vineyard regions should be shifted in other areas with appropriate climate.

DOI:

Publication date: December 3, 2021

Issue: Terroir 2010

Type: Article

Authors

A. Vuković (1,3), M. Vujadinović (1,3), V. Djurdjević (2,3), Z. Ranković-Vasić (1), N. Marković (1), Z. Atanacković (1), B. Sivčev (1), N. Petrović (1)

(1) Faculty of Agriculture, Belgrade University, Nemanjina 6, 11080 Belgrade, Serbia
(2) Institute for Meteorology, Faculty of Physics, Belgrade University, Dobracina 16, 11000 Belgrade, Serbia
(3) South East European Virtual Climate Change Center (hosted by Republic Hydrometeorological Service of Serbia), Bulevar oslobodjenja 8, 11000 Belgrade, Serbia

Contact the author

Keywords

climate projections, grapevine, climate classification

Tags

IVES Conference Series | Terroir 2010

Citation

Related articles…

Meso-scale geostatistical analysis: a method for improving experimental design

The growing region of Barolo DOCG certified wines is topographically complex. The region is famous for this complexity and for the associated terroir driven Nebbiolo grapes and wines derived distinctly from this varietal. Although it is recognized that the Barolo area is unusual topographically and it is assumed that this unusual topography lends to the inherit terroir, the specifics of this relationship are less well defined.

An overview of the impact of clone, environmental factors and viticultural techniques on rotundone concentration in red wines

Rotundone is the main aroma compound responsible for peppery notes in red wine. This positive and very potent molecule has an odor threshold of 8 ng/L in water and 16 ng/L in red wine. It has been detected in several grape varieties with some of the highest concentrations recorded in Syrah, Duras, Tardif and Noiret, an interspecific hybrid grown in the North-East of the USA. If several winemaking practices have been identified to lower rotundone in wine, up to date, no enological solution has proved its efficiency to maximize it. This means that efforts to produce high rotundone wines must be undertaken in vineyards. This work provides practical ways that can be used by winegrowers to modulate rotundone levels in their wines.

RED WINE AGING WITHOUT SO₂: WHAT IMPACT ON MICROBIAL COMMUNITY?

Nowadays, the use of food preservatives is controversial, SO2 being no exception. Microbial communities have been particularly studied during the prefermentary and fermentation stages in a context of without added SO2. However, microbial risks associated with SO2 reduction or absence, particularly during the wine aging process, have so far been little studied. The microbiological control of wine aging is a key issue for winemakers wishing to produce wines without added SO2. The aim of the present study is to evaluate the impact of different wine aging strategies according to the addition or not of SO2 on the microbiological population levels and diversity.

Vine-growing zoning of the municipal territories of Ronda and Arriate (Malaga, Spain), « Sierras de Málaga » registered appellation of origin mark

The aim of this communication is the study of the Ronda and Arriate municipal territories environment in order to define and to establish the main physical factors in relation to vine-growing land use. The vine-growing zoning proposed is based on geopedological and climatic features.

Effects of mesoclimate on the yield, quality and phenolic maturity of Grenache

The potential climate change, due to global change, will increase temperature general and could increase at local level. These changes are not going to be the same in different parts of the world, being especially important in the Mediterranean Basin.