冬季解冻实验揭示了加拿大魁北克北温带森林黄桦花蕾死亡率和物候学的临界点

Benjamin Marquis , Geneviève Lajoie
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摘要

气候变化预计会增加冬季解冻的频率和强度,从而影响叶片的物候期。叶片的物候期可能会通过加速强迫积累或冷冻完成而提前,也可能会通过与气温升高相关的冷冻减少而推迟。我们在实验室将 300 株糖槭树和黄桦树插条置于五种不同频率和持续时间的冬季融冻中,测试了冬季融冻对萌芽物候的影响。春季,一半的插条暴露在两个城市+ 2.0 °C的气温梯度下,以模拟当前气候变暖的情况,并每周监测三次萌芽物候。无论采用哪种解冻处理,气温较高城市的黄桦树芽的物候期都较早,这表明春季气温在触发芽萌发方面的重要性。解冻频率最高、持续时间最长的处理方法会增加花蕾的死亡率,推迟春季萌芽的开始时间,而解冻频率低的处理方法则不会,从而确定了冬季解冻对花蕾物候影响的临界点(每月两次,每次 3 天)。过了这个临界点,冬季融冻可能会减缓春季温度升高引起的芽的表观期,并通过延迟冠层的闭合来限制碳吸收。CMIP6 加拿大降尺度气候情景预测的气候变化模拟显示,冬季融冻的频率将增加。
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Experimental exposure to winter thaws reveals tipping point in yellow birch bud mortality and phenology in the northern temperate forest of Québec, Canada

Climate change is expected to increase the frequency and intensity of winter thaws, which could affect leaf phenology. Phenology could either be advanced through the acceleration of forcing accumulation or chilling completion, or be postponed through a reduction in chilling associated with warming air temperature. We tested the influence of winter thaws on budburst phenology by exposing 300 tree cuttings of sugar maple and yellow birch trees to five different frequencies and durations of winter thaws in the lab. In spring, half of the cuttings were exposed to air temperature in two cities representing an air temperature gradient of + 2.0 °C to mimic the ongoing climate warming and bud phenology was monitored three times a week. Irrespective of thaw treatment, yellow birch bud phenology occurred earlier in the warmer city, showing the importance of spring temperature in triggering budburst. The treatment with the highest frequency and duration of thawing increased bud mortality and delayed the onset of spring budburst whereas low frequency treatments did not, thereby identifying a tipping point (3 days twice a month) in the impact of winter thaws on bud phenology. Past this point, winter thaws could slow down bud phenology induced by warmer spring temperature and limit carbon uptake by delaying the closure of the canopy. Climate change simulations projected by the CMIP6 Canadian downscaled climate scenario show that winter thaws will increase in frequency Hence the expected advance in spring leaf emergence associated with warmer spring is not necessarily as straightforward as previously thought.

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