Modeling the water balance of sloped vineyards under various climate change scenarios

Grapes for wine production are a highly climate sensitive crop and vineyard water budget is a decisive factor in quality formation. In order to conduct risk assessments for climate change effects in viticulture, models are needed which can be applied to complete growing regions. We first modified an...

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Main Authors: Hofmann Marco, Schultz Hans R.
Format: Article
Language:English
Published: EDP Sciences 2015-01-01
Series:BIO Web of Conferences
Online Access:http://dx.doi.org/10.1051/bioconf/20150501026
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spelling doaj-48544090df204c5aac39ef6e68c3f4792021-04-02T18:53:19ZengEDP SciencesBIO Web of Conferences2117-44582015-01-0150102610.1051/bioconf/20150501026bioconf-oiv2015_01026Modeling the water balance of sloped vineyards under various climate change scenariosHofmann MarcoSchultz Hans R.Grapes for wine production are a highly climate sensitive crop and vineyard water budget is a decisive factor in quality formation. In order to conduct risk assessments for climate change effects in viticulture, models are needed which can be applied to complete growing regions. We first modified an existing simplified geometric vineyard model of radiation interception and resulting water use to incorporate numerical Monte Carlo simulations and the physical aspects of radiation interactions between canopy and vineyard slope and azimuth. We then used four regional climate models to assess for possible effects on the water budget of selected vineyard sites up to 2100. The model was developed to describe the partitioning of short-wave radiation between grapevine canopy and soil surface, respectively green cover, necessary to calculate vineyard evapotranspiration. Soil water storage was allocated to two sub reservoirs. The model was adopted for steep slope vineyards based on coordinate transformation and validated against measurements of grapevine sap flow and soil water content determined down to 1.6 m depth at three different sites over two years. The results showed good agreement of modelled and observed soil water dynamics of vineyards with large variations in site specific soil water holding capacity and viticultural management. Simulated sap flow was in overall good agreement with measured sap flow but site-specific responses of sap flow to potential evapotranspiration were observed. The analyses of climate change impacts on vineyard water budget demonstrated the importance of site-specific assessment due to natural variations in soil water holding capacity. The model was capable of describing seasonal and site-specific dynamics in soil water content and could be used in an amended version to estimate changes in the water budget of entire grape growing areas due to evolving climatic changes.http://dx.doi.org/10.1051/bioconf/20150501026
collection DOAJ
language English
format Article
sources DOAJ
author Hofmann Marco
Schultz Hans R.
spellingShingle Hofmann Marco
Schultz Hans R.
Modeling the water balance of sloped vineyards under various climate change scenarios
BIO Web of Conferences
author_facet Hofmann Marco
Schultz Hans R.
author_sort Hofmann Marco
title Modeling the water balance of sloped vineyards under various climate change scenarios
title_short Modeling the water balance of sloped vineyards under various climate change scenarios
title_full Modeling the water balance of sloped vineyards under various climate change scenarios
title_fullStr Modeling the water balance of sloped vineyards under various climate change scenarios
title_full_unstemmed Modeling the water balance of sloped vineyards under various climate change scenarios
title_sort modeling the water balance of sloped vineyards under various climate change scenarios
publisher EDP Sciences
series BIO Web of Conferences
issn 2117-4458
publishDate 2015-01-01
description Grapes for wine production are a highly climate sensitive crop and vineyard water budget is a decisive factor in quality formation. In order to conduct risk assessments for climate change effects in viticulture, models are needed which can be applied to complete growing regions. We first modified an existing simplified geometric vineyard model of radiation interception and resulting water use to incorporate numerical Monte Carlo simulations and the physical aspects of radiation interactions between canopy and vineyard slope and azimuth. We then used four regional climate models to assess for possible effects on the water budget of selected vineyard sites up to 2100. The model was developed to describe the partitioning of short-wave radiation between grapevine canopy and soil surface, respectively green cover, necessary to calculate vineyard evapotranspiration. Soil water storage was allocated to two sub reservoirs. The model was adopted for steep slope vineyards based on coordinate transformation and validated against measurements of grapevine sap flow and soil water content determined down to 1.6 m depth at three different sites over two years. The results showed good agreement of modelled and observed soil water dynamics of vineyards with large variations in site specific soil water holding capacity and viticultural management. Simulated sap flow was in overall good agreement with measured sap flow but site-specific responses of sap flow to potential evapotranspiration were observed. The analyses of climate change impacts on vineyard water budget demonstrated the importance of site-specific assessment due to natural variations in soil water holding capacity. The model was capable of describing seasonal and site-specific dynamics in soil water content and could be used in an amended version to estimate changes in the water budget of entire grape growing areas due to evolving climatic changes.
url http://dx.doi.org/10.1051/bioconf/20150501026
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