GiESCO 2019 banner
IVES 9 IVES Conference Series 9 GiESCO 9 GiESCO 2019 9 Climate change 9 Impacts on water availability for vitiviniculture worldwide using different potential evapotranspiration methods

Impacts on water availability for vitiviniculture worldwide using different potential evapotranspiration methods

Abstract

Context and purpose of the study ‐ Beyond the sole warming globally perceived and monitored, climate change impacts water availability. Increasing heatwaves frequency observed during the last decades and projected for the 21st century certainly result (or will result)in more water deficit stress for grapevine. Change in water availability throughout the season depends on the balance between precipitation and evapotranspiration. The latter is seldom assessed through potential evapotranspiration (ET0) calculated with empirical formulae relying on air temperature only. This study compares the changes in water availability estimates for viticulture using such formulae in comparison to the reference Penman‐ Monteith approach.

Material and methods – Monthly interpolated minimum and maximum temperature, precipitation and Penman‐Monteith (PM) ET0 data for land surfaces worldwide were collected from the CRU TS4.01 gridded dataset, from 1971 to 2017. Other ET0estimates were produced using the Thornthwaite (T) and the Hargreaves (H) temperature‐based as well as the Modified Hargreaves (M) temperature‐and‐ rainfall‐based methods. PM, T, H, M ET0 data were used to calculate the dryness index (DI), a monthly water balance‐based index for viticulture. Changes between the periods 1971‐2000 (HIST) and 2001‐ 2017 (PRES) in potential evapotranspiration and in DI were compared for each of the 4 ET0calculation methods. The changes were analyzed in wine producing regions using the vineyard geodatabase v1.2.3, a shapefile referencing 691 wine producing regions worldwide.

Results – All 4 methods compute an average increase (from HIST to PRES) in ET0 of about 20 mm during the grapevine growing season, i.e. April to September (October to March) for the northern (southern) hemisphere. The change (PRES ‐ HIST) differ substantially in space, according to the method used. For instance, a decrease in ET0 is shown in southwestern and central North America when using PM method, while T method indicates a weak to moderate raise in ET0 in these regions. Changes in dryness index th st from the late 20 to the early 21 century are large and highly variable in space: from ‐65 mm to +62 mm (0.05 and 0.95 percentiles), according to the location and to the ET0 calculation method. DI also strongly varies in space, but results are less sensitive to ET0 calculation method. PM shows a decrease in DI (PRES ‐ HIST) down to ‐75 mm in most regions but Australia, central Europe and Italy. While PM, H and M methods indicate a clear decrease of DI in France, Portugal and Spain, T method suggests an increase in DI in the northern part of France and in most of Spain. It is concluded that (1) ET0 has risen and contributed to DI decrease in many wine regions worldwide and (2) using T empirical method to derive ET0 from temperature can lead to different conclusions concerning changes in water availability for viticulture

DOI:

Publication date: June 19, 2020

Issue: GiESCO 2019

Type: Article

Authors

Benjamin BOIS

CRC,UMR Biogeosciences (6282 CNRS/uB), Université Bourgogne Franche-Comté, 6 Boulevard Gabriel, 21000 Dijon, France

Contact the author

Keywords

potential evapotranspiration, viticulture, climate change, temperature‐based methods, dryness

Tags

GiESCO 2019 | IVES Conference Series

Citation

Related articles…

Impact of long term agroecological and conventional practices on subsurface soil microbiota in Macabeu and Xarel·lo vineyards

There is a growing trend on the transition from conventional to agroecological management of vineyards. However, the impact of practices, such as reduced-tillage, organic fertilization and cover crops, is not well-understood regarding the soil microbial diversity, and its relationship with the soil physicochemical properties in the subsurface depth near the rooting zone. Soil bacterial diversity is an important contributor towards plant health, productivity and response to environmental stresses. A field experiment was conducted by sampling subsurface soil bacterial community (NGS and qPCR) near to the root zone of Macabeu and Xarel·lo vineyards, located at the Penedes. 3 organic (ECO) and 3 conventional (CON) vineyards, with more than 10 years of respective management were sampled (n=5 each plot). ECO practices did not affect bacterial and fungal abundance but increased significantly the ammonium oxidizing bacteria and alpha-diversity (Inv.Simpson). Interestingly beta-diversity was significantly affected by the management strategy. ANOSIM-tests revealed a significative effect of the management (ecological vs conventional) and plot, on the soil microbial structure (ASV abundance). Main phyla depicted were Proteobacteria, Actinobacteria and Acidobacteria, whose relative abundances were not affected by the management. EdgeR assay revealed a significant increase of Cyanobacteria and decrease of Gemmatimonadetes and Firmicutes phyla in ECO. Interestingly, the grapevine variety was not correlated with the soil microbial community structure. Mantel-test revealed an important correlation (Spearman) of some physicochemical parameters with the soil microbiota structure, in order of importance: texture, EC, pH Ca/Mg, Mg/P, K+, Mg2+, Ca2+, SO42-, and OM. N-NH4 and NTK, which were higher in the ECO managed soils, did not correlated significantly with the soil microbiome population. The results revealed the importance of combining a deep physicochemical characterization of each replicate with the microbial diversity assessment to gain better insights on the relationship between soil microbiome and vineyard management.

Analysis of Cabernet Sauvignon and Aglianico winegrape (V. vinifera L.) responses to different pedo-climatic environments in southern Italy

Water deficit is one of the most important effects of climate change able to affect agricultural sectors. In general, it determines a reduction in biomass production, and for some plants, as in the case of grapevine, it can endorse fruit quality. The monitoring and management of plant water stress in the vineyard

Vineyards and clay minerals: multi-technique analytical approach and correlations with soil properties

Purpose of this research is to quantitatively assess the mineral component of vineyard soils, with particular attention to the mineralogical analysis of clays, which represent an element of high importance in the vineyard culture as well as in general agriculture. An X-ray diffraction (XRD) / thermogravimetric (TG) multi-technique analytical approach was developed, tested on soil samples taken from vineyards around the world. This codified analytical procedure was necessary to obtain precise qualitative and quantitative mineralogical data, globally comparable to distinguish the geopedological identity of the vineyards. Soil samples from vineyards of various locations were analysed, in very different geological conditions. The bulk-rock quantitative phase analysis (QPA) was obtained by the Rietveld method while the detailed composition of the clay-sized fraction was determined by modelling of the oriented X-ray diffraction patterns. The research provided a precise classification of the mineral component of soils, distinguishing the mineral phases of the clays and the so-called mixed-layer clay minerals. We found that the content in mixed layers can be directly correlated with the water retention and the cation exchange capacity ​​of the soil, while the presence of other clayey minerals and phyllosilicates in this research did not affect this CEC parameter, which codes the fertility level of the soils. The study demonstrates that terroir, in particular soils formed in complex or very different geological conditions, can only be effectively interpreted by properly analysing its mineral phases, in particular the mixed-layer clay component. These are characteristic abiotic ecological indicators, which may have specific eco-physiological influences on the plant.

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.

Soil quality in Beaujolais vineyard. Importance of pedology and cultural practices

A pedological study was carried out from 2009 to 2017 in Beaujolais vineyard, to improve physical and chemical knowledge of soils. It was completed in 2016 and 2017 by the current study, dealing with microbial aspects, in order to build a reference frame for improved advice in soil management. Microbial biomass was measured on representative plots of the six most common soil types identified in Beaujolais and, for each soil type, on plots with different levels of the main impacting parameters: total organic carbon, pH, cation exchange capacity, extractable copper. A total of 59 soil samples were collected. Confirming the results of various trials carried out in Beaujolais over the past 20 years, the results of the present study showed that the soils were still alive, but exhibited a large variability of biological parameters, which appeared dependant on both pedological and anthropic factors. Therefore, a good interpretation of biological parameters and advice for vine growers must rely on a pedologically-based referential with differentiated main driving factors. For example, the control of pH is of primary importance in granitic soils and in no way organic matter addition can improve soil quality if pH is too low. Conversely, in calcareous soils, biological parameters are more directly affected by direct or indirect (cover crops for example) inputs of organic matter. The use of biological parameters, such as microbial biomass, is of great potential value to improve advice on agro-viticultural practices (soil management, fertilization, liming, etc.), basis of a sustainable wine production on fragile soils.