GiESCO 2019 banner
IVES 9 IVES Conference Series 9 GiESCO 9 GiESCO 2019 9 Effect of topography on vine evapotranspiration and water status in hillside vineyards

Effect of topography on vine evapotranspiration and water status in hillside vineyards

Abstract

Context and purpose of the study – Many winegrape regions have hillside vineyards, where vine water use is affected by vine age, density and health, canopy size, row orientation, irrigation practices, and by block slope and aspect. Topography affects the amount of solar radiation the vines receive, which is a major “driving force” of evapotranspiration (ET). Nearly all crop ET studies have been conducted on level ground, where the contributions of weather and crop factors to ET are well known. Information on winegrape ET on hillside terrains is scarce but much needed, as growers seek more resource‐efficient production practices and vine water stress monitoring techniques to manage grapes quality, and as future water supplies become increasingly variable, limited and costly. Our UC team measured the seasonal dynamics of actual ET (ETa) and vine water status in two similar vineyard blocks with north and south aspects during three consecutive seasons, with the aim to inform irrigation management decisions.

Material and methods ‐ The vineyard blocks are located in El Dorado County, California, and both are Cabernet sauvignon on 3309 rootstock, planted in 2000 with VSP trellis on approximately 24% (north‐ facing) and 25% (south‐facing) slopes, where the grower managed the irrigation. We determined ETa in the 2016 to 2018 seasons using the residual of energy balance method with a combination of eddy covariance and surface renewal equipment to measure sensible heat flux (H). Reference ET (ETo) data was taken from the nearest weather station to calculate actual crop coefficients (Ka). We also periodically measured midday stem water potential (ΨSTEM). 

Results ‐ The north and south blocks had similar seasonal ETa, but the water use dynamic varied with the slope aspect. Until early May, ETa was slightly higher in the south (Ka between 0.5 and 0.9) than the north block (Ka between 0.4 and 0.7). From mid‐May to June and mid‐July to August, the north block had higher ETa (Ka ~ 0.65 versus 0.55 in the south slope). A progressive decrease in water use was observed from late June onwards in both blocks, with Ka of ~ 0.4 and 0.3 in August and September, respectively. Early and late in the season, we measured lower net radiation in the north block, likely due to the greater incidence angle of the incoming solar radiation. Late in the season, the north block had lower ΨSTEM (more stress) in 2016 and 2017, and the south block had lower ΨSTEM in 2018. Our results show that monitoring ETa and vine water status can inform irrigation and water stress management in hillside vineyards. 

DOI:

Publication date: June 19, 2020

Issue: GiESCO 2019

Type: Article

Authors

Daniele ZACCARIA (1), Lynn WUNDERLICH (2), Giulia MARINO (1), Kristen SHAPIRO (1), Sloane RICE (1), Kenneth SHACKEL (3), Richard SNYDER (1)

(1) Department of Land, Air and Water Resources, UC-Davis, One Shields Avenue, Davis, CA. 95616 USA.
(2) UCCE, 311 Fair Lane, Placerville, CA. 95667 USA.
(3) Department of Plant Sciences, UC-Davis, One Shields Avenue, Davis, CA. 95616, USA.

Contact the author

Keywords

Energy balance, actual water use, slope, crop coefficient, stem water potential

Tags

GiESCO 2019 | IVES Conference Series

Citation

Related articles…

Grape berry size is a key factor in determining New Zealand Pinot noir wine composition

Making high quality but affordable Pinot noir (PN) wine is challenging in most terroirs and New Zealand’s (NZ) situation is no exception. To increase the probability of making highly typical PN wines producers choose to grow grapes in cool climates on lower fertility soils while adopting labour intensive practices. Stringent yield targets and higher input costs necessarily mean that PN wine cost is high, and profitability lower, in line-priced varietal wine ranges. To understand the reasons why higher yielding vines are perceived to produce wines of lower quality we have undertaken an extensive study of PN in NZ. Since 2018, we established a network of twelve trial sites in three NZ regions to find individual vines that produced acceptable commercial yields (above 2.5kg per vine) and wines of composition comparable to “Icon” labels. Approximately 20% of 660 grape lots (N = 135) were selected from within a narrow juice Total Soluble Solids (TSS) range and made into single vine wines under controlled conditions. Principal Component Analysis of the vine, berry, juice and wine parameters from three vintages found grape berry mass to be most effective clustering variable. As berry mass category decreased there was a systematic increase in the probability of higher berry red colour and total phenolics with a parallel increase in wine phenolics, changed aroma fraction and decreased juice amino acids. The influence of berry size on wine composition would appear stronger than the individual effects of vintage, region, vineyard or vine yield. Our observations support the hypothesis that it is possible to produce PN wines that fall within an “Icon” benchmark composition range at yields above 2.5kg per vine provided that the Leaf Area:Fruit Weight ratio is above 12cm2 per g, mean berry mass is below 1.2g and juice TSS is above 22°Brix.

Climate and the evolving mix of grape varieties in Australia’s wine regions

The purpose of this study is to examine the changing mix of winegrape varieties in Australia so as to address the question: In the light of key climate indicators and predictions of further climate change, how appropriate are the grape varieties currently planted in Australia’s wine regions? To achieve this, regions are classified into zones according to each region’s climate variables, particularly average growing season temperature (GST), leaving aside within-region variations in climates. Five different climatic classifications are reported. Using projections of GSTs for the mid- and late 21st century, the extent to which each region is projected to move from its current zone classification to a warmer one is reported. Also shown is the changing proportion of each of 21 key varieties grown in a GST zone considered to be optimal for premium winegrape production. Together these indicators strengthen earlier suggestions that the mix of varieties may be currently less than ideal in many Australian wine regions, and would become even less so in coming decades if that mix was not altered in the anticipation of climate change. That is, grape varieties in many (especially the warmest) regions will have to keep changing, or wineries will have to seek fruit from higher latitudes or elevations if they wish to retain their current mix of varieties and wine styles.

Climate projections over France wine-growing region and its potential impact on phenology

Climate change represents a major challenge for the French wine industry. Climatic conditions in French vineyards have already changed and will continue to evolve. One of the notable effects on grapevine is the advancing growing season. The aim of this study is to characterise the evolution of agroclimatic indicators (Huglin index, number of hot days, mean temperature, cumulative rainfall and number of rainy days during the growing season) at French wine-growing regions scale between 1980 and 2019 using gridded data (8 km resolution, SAFRAN) and for the middle of the 21th century (2046-2065) with 21 GCMs statistically debiased and downscaled at 8 km. A set of three phenological models were used to simulate the budburst (BRIN, Smoothed-Utah), flowering, veraison and theoretical maturity (GFV and GSR) stages for two grape varieties (Chardonnay and Cabernet-Sauvignon) over the whole period studied. All the French wine-growing regions show an increase in both temperatures during the growing season and Huglin index. This increase is accompanied by an advance in the simulated flowering (+3 to +9 days), veraison (+6 to +13 days) and theoretical maturity (+6 to +16 days) stages, which are more noticeable in the north-eastern part of France. The climate projections unanimously show, for all the GCMs considered, a clear increase in the Huglin index (+662 to 771 °C.days compared to the 1980-1999 period) and in the number of hot days (+5.6 to 22.6 days) in all the wine regions studied. Regarding rainfall, the expected evolution remains very uncertain due to the heterogeneity of the climates simulated by the 21 models. Only 4 regions out of 21 have a significant decrease in the number of rainy days during the growing season. The two budburst models show a strong divergence in the evolution of this stage with an average difference of 18 days between the two models on all grapevine regions. The theoretical maturity is the most impacted stage with a potential advance between 40 and 23 days according to wine-growing regions.

Bioclimatic shifts and land use options for Viticulture in Portugal

Land use, plays a relevant role in the climatic system. It endows means for agriculture practices thus contributing to the food supply. Since climate and land are closely intertwined through multiple interface processes, climate change may lead to significant impacts in land use. In this study, 1-km observational gridded datasets are used to assess changes in the Köppen–Geiger and Worldwide Bioclimatic (WBCS)

Simulating climate change impact on viticultural systems in historical and emergent vineyards

Global climate change affects regional climates and hold implications for wine growing regions worldwide. Although winegrowers are constantly adapting to internal and external factors, it seems relevant to develop tools, which will allow them to better define actual and future agro-climatic potentials. Within this context, we develop a modelling approach, able to simulate the impact of environmental conditions and constraints on vine behaviour and to highlight potential adaptation strategies according to different climate change scenarios. Our modeling approach, named SEVE (Simulating Environmental impacts on Viticultural Ecosystems), provides a generic modeling framework for simulating grapevine growth and berry ripening under different conditions and constraints (slope, aspect, soil type, climate variability…) as well as production strategies and adaptation rules according to climate change scenarios. Each activity is represented by an autonomous agent able to react and adapt its reaction to the variability of environmental constraints. Using this model, we have recently analyzed the evolution of vineyards’ exposure to climatic risks (frost, pathogen risk, heat wave) and the adaptation strategies potentially implemented by the winegrowers. This approach, implemented for two climate change scenarios, has been initiated in France on traditional (Loire Valley) and emerging (Brittany) vineyards. The objective is to identify the time horizons of adaptations and new opportunities in these two regions. Carried out in collaboration with wine growers, this approach aims to better understand the variability of climate change impacts at local scale in the medium and long term.