Climate influences on the phenology of tree and shrub species

In this project phenological observations of various tree and shrub species in Switzerland are investigated, that have been recorded by MeteoSwiss since 1951. The ca. 200’000 observations cover various phenophases such as leaf unfolding/needle appearance, flowering, fruit ripening, leaf/needle coloring, and leaf/needle fall.

In the first part of the project, we investigated whether the frost risk during leaf unfolding and needle appearance, respectively, of 13 tree and shrub species has changed from 1951 to 2014 (Fig. 1). A total of 48'000 observations at 264 stations from the phenological network of MeteoSwiss were investigated. To assess whether the trends of leaf unfolding and frost risk change, "state-space models" were used (Fig. 2). All investigated species show increasingly earlier dates of leaf unfolding, particularly above 800 m a.s.l. and since the 1980s, which may be attributed to the higher spring temperatures. Currently, trees and shrubs have a relatively large safety margin between the last critical frost and the timing of leaf unfolding. However, frost risk increases in early-leafing species (e.g. larch, horse chestnut, hazel, silver birch, rowan) and with increasing elevation. The frost risk tended to decrease during the cool 1950s and 1960s, while it has been increasing since the 2000s due to climate warming.

The study has been published as external pageBigler and Bugmann (2018).

Enlarged view: Frost damage
Figure 1. Frost damage on young needles of Norway spruce following the severe frosts in April 2017 (picture: C. Bigler)
Enlarged view: Trend analysis
Figure 2. Trend analysis of leaf-out dates based on dynamic linear model (DLM) and linear model (LM). Data for beech at the station La Valsainte. (a) Observed dates of leaf unfolding, smoothed levels based on DLM, and regression line based on LM, (b) smoothed slopes based on DLM and slope based on LM. The DLM indicates a positive slope in 1960 (0.53 days/year) and a negative slope in 2010 (−0.46 days/year), whereas the LM suggests a constant negative slope (−0.20 days/year).

In the second part of the project, we investigated how daily weather influences affect leaf unfolding and needle appearance, respectively, of five deciduous and conifer species (larch, horse chestnut, hazel, beech, Norway spruce). Since daily weather influences such as the maximum temperature have an impact over several weeks and months, we quantified the relationship between weather influences and leaf unfolding using "distributed lag models" (Fig. 3).

The study was published as external pageBigler and Vitasse (2019).

Enlarged view: Distributed lag model
Figure 3. Visualization of a distributed lag model. The figure shows the odds ratio for leaf unfolding of beech at the phenological station Liestal (350 m a.s.l.) in Switzerland depending on maximum daily temperature and the lag (number of days before leaf unfolding).

In the third part of the project, we investigate under which climatic conditions exceptionally early leaf discoloration of trees occurs. We analyze 16385 observations of leaf discoloration of beech, birch, horse chestnut, larch, large-leaved linden, rowan, small-leaved lime, sweet chestnut and sycamore at 222 phenological stations in Switzerland. In years with exceptionally early leaf discoloration, the growing-degree days in May and June were significantly higher and the climatic water balance in June was significantly lower than in the other years, particularly for drought-sensitive species such as beech (Fig. 4). Also very low minimum temperatures in September caused exceptionally early leaf discoloration.

A manuscript is in review: Bigler C. and Vitasse Y. 2021. Premature leaf discoloration of European deciduous trees is caused by drought and heat in late spring and cold spells in early fall.

Enlarged view: LMM
Figure 4. Effects of monthly climatic water balance and growing-degree days based on linear mixed-effects models (red dots: P ≤ 0.05; red-bordered white dots: P ≤ 0.01; black dots: P > 0.1; 95% confidence intervals were drawn as horizontal lines). Example: A negative effect of water balance in June for beech suggests that in years with exceptionally early leaf discoloration the water balance was lower than in other years.

Funding

ETH Zurich

Status of the project

The project started in February 2015.

Contact

Please contact Christof Bigler for more information.

Enlarged view: Prunus spinosa
Flowering of Prunus spinosa (picture: C. Bigler)
Enlarged view: Picea abies
Needle appearance of Picea abies (picture: C. Bigler)
Enlarged view: Sorbus aucuparia
Fruit ripening of Sorbus aucuparia (picture: C. Bigler)
Enlarged view: Fagus sylvatica
Leaf coloring of Fagus sylvatica (picture: C. Bigler)
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