Scandinavian winters are getting shorter at a rapid pace
Season lengths are changing
Climate change is affecting the length of summer and winter in northern Europa. Observations show that winter has shortened by 29 days in southern Estonia between 1891 and 2003, and by nearly 40 days in Poland in the period 1951-2010. Likewise summer has become longer in these periods by 11 days in southern Estonia and by nearly 20 days in Poland.
These trends will continue into future decades. For northern Europe, season lengths have been quantified for the period 2040-2069, under a moderate scenario of climate change and based on a large number of global climate models. Changes have been compared with the seasons in 1971-2000 for reference. This scenario corresponds to 2°C global warming in 2040-2069 relative to the preindustrial climate. In northern Europe, warming exceeds this global mean substantially, however.
Longer summers, shorter winters
According to these model projections, the summer (daily mean temperature > 10°C) will last about a month longer by mid-century in most of Northern Europe. The summer is projected to start 2 weeks earlier and last two weeks longer. In the very coldest areas, the mountains, northern Lapland and the coasts of the Arctic Ocean, summer lengthening may be even more than 30 days.
Concurrently, the projections show that winter (daily mean temperature < 0°C) will become shorter by 30-60 days. Winters are projected to start 15-30 days later and end 15-30 days earlier. Changes are largest near the coasts of the Arctic Ocean and the Baltic Sea, and relatively modest in the northern inland areas.
Standard deviations of the model projections are about 10 days for the lengths of the spring, summer and autumn, and 10-25 days for winter length. In Denmark and southernmost Sweden, the average winter is already quite short now and there is little room for further shortening. By mid-century, the probability of missing winters will increase considerably, particularly in southern Sweden and the Baltic countries.
Source: Ruosteenoja et al., 2020. International Journal of Climatology 40: 4444 - 4462.