Weather conditions associated with grape production in the Okanagan Valley of British Columbia and potential impact of climate change

An iterative χ 2 method applied to 60 yr of records in the Okanagan Valley of British Columbia (1930–1989) revealed that the main climatic factor limiting grape production (Vitis spp. and Vitis vinifera L.) was low temperatures (critical value range, ≤–6°C to ≤–23°C) occurring during late October, N...

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Published in:Canadian Journal of Plant Science
Main Authors: Caprio, J. M., Quamme, H. A.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2002
Subjects:
Online Access:http://dx.doi.org/10.4141/p01-160
http://www.nrcresearchpress.com/doi/pdf/10.4141/P01-160
id crcansciencepubl:10.4141/p01-160
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spelling crcansciencepubl:10.4141/p01-160 2024-05-19T07:36:33+00:00 Weather conditions associated with grape production in the Okanagan Valley of British Columbia and potential impact of climate change Caprio, J. M. Quamme, H. A. 2002 http://dx.doi.org/10.4141/p01-160 http://www.nrcresearchpress.com/doi/pdf/10.4141/P01-160 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Plant Science volume 82, issue 4, page 755-763 ISSN 0008-4220 1918-1833 journal-article 2002 crcansciencepubl https://doi.org/10.4141/p01-160 2024-04-25T06:52:00Z An iterative χ 2 method applied to 60 yr of records in the Okanagan Valley of British Columbia (1930–1989) revealed that the main climatic factor limiting grape production (Vitis spp. and Vitis vinifera L.) was low temperatures (critical value range, ≤–6°C to ≤–23°C) occurring during late October, November, December and February. Daytime temperatures ≤–9°C during late November and early December benefited grape production, probably because it prevented vine de-acclimation. Detrimental effects of precipitation during late October were probably associated with the early movement of Arctic fronts into the region. Beneficial effects of precipitation in the form of snow were observed in January. During the pre-harvest growing season, except for a 2-wk period in July, high temperatures (≥26°C) were associated with good production, probably because warm temperatures are required for flower bud initiation and development. In contrast, higher-than-normal temperatures were not beneficial to production during the harvest year. Detrimental effects of high temperature were observed during July of the pre-harvest year and July (≥32°C) and early August of the harvest year (≥28°C). During the growing season, rainfall was sometimes unfavourable for grape production under irrigation, either because of associated cool weather or greater disease occurrence. Both temperature and precipitation were greater in the last 18 yr of the study than the prior 36 yr, especially during the late winter and early spring. The anticipated climatic change appears to favour grape production in the Okanagan Valley. Key words: grape, climate change, heat stress, winter injury Article in Journal/Newspaper Arctic Climate change Canadian Science Publishing Canadian Journal of Plant Science 82 4 755 763
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
description An iterative χ 2 method applied to 60 yr of records in the Okanagan Valley of British Columbia (1930–1989) revealed that the main climatic factor limiting grape production (Vitis spp. and Vitis vinifera L.) was low temperatures (critical value range, ≤–6°C to ≤–23°C) occurring during late October, November, December and February. Daytime temperatures ≤–9°C during late November and early December benefited grape production, probably because it prevented vine de-acclimation. Detrimental effects of precipitation during late October were probably associated with the early movement of Arctic fronts into the region. Beneficial effects of precipitation in the form of snow were observed in January. During the pre-harvest growing season, except for a 2-wk period in July, high temperatures (≥26°C) were associated with good production, probably because warm temperatures are required for flower bud initiation and development. In contrast, higher-than-normal temperatures were not beneficial to production during the harvest year. Detrimental effects of high temperature were observed during July of the pre-harvest year and July (≥32°C) and early August of the harvest year (≥28°C). During the growing season, rainfall was sometimes unfavourable for grape production under irrigation, either because of associated cool weather or greater disease occurrence. Both temperature and precipitation were greater in the last 18 yr of the study than the prior 36 yr, especially during the late winter and early spring. The anticipated climatic change appears to favour grape production in the Okanagan Valley. Key words: grape, climate change, heat stress, winter injury
format Article in Journal/Newspaper
author Caprio, J. M.
Quamme, H. A.
spellingShingle Caprio, J. M.
Quamme, H. A.
Weather conditions associated with grape production in the Okanagan Valley of British Columbia and potential impact of climate change
author_facet Caprio, J. M.
Quamme, H. A.
author_sort Caprio, J. M.
title Weather conditions associated with grape production in the Okanagan Valley of British Columbia and potential impact of climate change
title_short Weather conditions associated with grape production in the Okanagan Valley of British Columbia and potential impact of climate change
title_full Weather conditions associated with grape production in the Okanagan Valley of British Columbia and potential impact of climate change
title_fullStr Weather conditions associated with grape production in the Okanagan Valley of British Columbia and potential impact of climate change
title_full_unstemmed Weather conditions associated with grape production in the Okanagan Valley of British Columbia and potential impact of climate change
title_sort weather conditions associated with grape production in the okanagan valley of british columbia and potential impact of climate change
publisher Canadian Science Publishing
publishDate 2002
url http://dx.doi.org/10.4141/p01-160
http://www.nrcresearchpress.com/doi/pdf/10.4141/P01-160
genre Arctic
Climate change
genre_facet Arctic
Climate change
op_source Canadian Journal of Plant Science
volume 82, issue 4, page 755-763
ISSN 0008-4220 1918-1833
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.4141/p01-160
container_title Canadian Journal of Plant Science
container_volume 82
container_issue 4
container_start_page 755
op_container_end_page 763
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