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首页> 外文期刊>American journal of enology & viticulture >Spatial and Temporal Study of Climatic Variability on Grape Production in Southwestern Michigan
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Spatial and Temporal Study of Climatic Variability on Grape Production in Southwestern Michigan

机译:密歇根州西南部葡萄生产的气候变化时空研究

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摘要

Daily climatic data were obtained from several sources to calculate growing degree days (GDD) for multiple sites in southwest Michigan, which contains the Lake Michigan Shore American Viticultural Area. The data were examined for spatial and temporal (1950 to 2011) patterns and trends over the region in order to better quantify the role of Michigan climate on juice grape production. The occurrence and severity of frost and freezing temperatures were also considered in this study, as subfreezing temperatures in late spring and early fall can have severe impacts on the region's juice grape production and fruit quality at harvest. Michigan's cool-cold climate has warmed in recent decades, particularly since 1980, with an average increase over the region of more than 3.7 GDD (base 10℃) per year. Southwestern Michigan was also found to have higher seasonal temperature variability when compared with Napa Valley (California). Since 1980, the season-to-season variability in Michigan has increased at a more rapid pace. The impacts of the increasing GDD have been positive for fruit quality, with a strong positive correlation between seasonal GDD and fruit maturation, indexed as total soluble solids (Brix). The growing season has also increased by 28 days in length since 1971. However, despite warmer temperatures, the number of days of potential frost and their seasonal variability in southwestern Michigan have remain unchanged, which continues to pose a risk for grapegrowers in the region. While it has become warmer in Michigan, and the spring warm-up is typically arriving earlier in the year, the number of days with damaging frost still has a profound impact on overall climate-related risk for grape production.
机译:从数个来源获取每日气候数据,以计算密歇根州西南部多个地点的生长度日(GDD),其中包括密歇根湖岸美国葡萄栽培区。为了更好地量化密歇根州气候在果汁葡萄生产中的作用,对数据进行了时空(1950年至2011年)模式和区域趋势的检验。这项研究还考虑了霜冻和冰冻温度的发生和严重程度,因为春末和初秋的亚冰点温度可能对该地区的果汁葡萄产量和收获时的果实品质产生严重影响。密歇根州的凉冷气候在最近几十年里一直在变暖,特别是自1980年以来,该地区平均每年平均增加3.7 GDD(以10℃为基准)。与纳帕谷(加利福尼亚州)相比,密歇根州西南部的季节性温度变化也更大。自1980年以来,密歇根州的季节变化性以更快的速度增长。 GDD增加对水果质量的影响是积极的,季节性GDD和果实成熟度之间有很强的正相关关系,以总可溶性固形物(白利糖度)为指标。自1971年以来,生长季节的长度也增加了28天。然而,尽管温度升高,密歇根州西南部的潜在霜冻天数及其季节性变化仍保持不变,这继续对该地区的葡萄种植者构成风险。虽然密歇根州的天气变暖了,春季的暖身通常会在一年的早些时候到来,但霜冻破坏的天数仍然对与气候相关的葡萄生产风险产生深远影响。

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