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Phenological modeling reveals divergent shifts in sap onset and ending in sugar maple under warming, indicating a shortened harvesting window and heightened risks for syrup producers.
Climate change raises concerns for the maple syrup industry, mainly regarding the expected changes in the timings of the sugar season and the resulting uncertainty of sap yield. This study investigates the temporal relationships between the environmental factors and sap phenology (i.e., timings of the onset and ending of sap season) in sugar maple ( Acer saccharum Marsh.) during 2018-2022 at the northern limit of the species in Quebec, Canada, and predicts the impact of warming under greenhouse gas emission scenarios (RCP 2.6, 4.5, and 8.5). March and April temperatures are correlated to the onset and ending of sap exudation, occurring on average on DOY (day of the year) 86 and 133, respectively. Sap exudation corresponds with the start of snowmelt and the consequent increase in soil water content. Complete snowmelt and the increase in soil temperature coincide with the ending of sap exudation. Our partial least squares regressions estimate an advancement of up to 20 days for the start and 26 days for the end of sap production by 2100 at RCP 8.5. The predictions suggest a divergent advancement of the onset and ending of sap production under warming, resulting in a shorter duration of the sugar season. The earlier sap season represents an important challenge for producers, who will need to adjust their activities in the sugarbushes to match the warmer conditions predicted for late winter and early spring. Any delay in tapping will increase the risk of substantial losses in production, especially in the context of a shorter sap season.
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Kurokawa et al. (2025) studied this question.
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