Human influence on growing-period frosts like in early April 2021 in central France

In: Natural hazards and earth system sciences: NHESS, Band 23, Heft 3, S. 1045-1058

Open Access

Abstract

Abstract. In early April 2021 several days of harsh frost affected central Europe. This led to very severe damage in grapevine and fruit trees
in France, in regions where young leaves had already unfolded due to
unusually warm temperatures in the preceding month (March 2021). We analysed
with observations and 172 climate model simulations how human-induced
climate change affected this event over central France, where many vineyards are located. We found that, without human-caused climate change, such temperatures in April or later in spring would have been even lower by
1.2 ∘C (0.75 to 1.7 ∘C). However, climate
change also caused an earlier occurrence of bud burst that we characterized in this study by a growing degree day index value. This shift leaves young leaves exposed to more winter-like conditions with lower minimum temperatures and longer nights, an effect that overcompensates the warming effect. Extreme cold temperatures occurring after the start of the growing season such as those of April 2021 are now 2 ∘C colder
(0.5 to 3.3 ∘C) than in preindustrial conditions, according to observations. This observed intensification of growing-period frosts is attributable, at least in part, to human-caused climate change with each of the five climate model ensembles used here simulating a cooling of growing-period annual temperature minima of 0.41 ∘C (0.22 to 0.60 ∘C) since preindustrial conditions. The 2021 growing-period frost event has become 50 % more likely (10 %–110 %). Models accurately simulate the observed warming in extreme lowest spring temperatures but underestimate the observed trends in growing-period frost intensities, a fact that yet remains to be explained. Model ensembles all simulate a further intensification of yearly minimum temperatures occurring in the growing period for future decades and a significant probability increase for such events of about 30 % (20 %–40 %) in a climate with global warming of 2 ∘C.