EGU26-10758, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-10758
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Friday, 08 May, 10:45–12:30 (CEST), Display time Friday, 08 May, 08:30–12:30
 
Hall X1, X1.5
Negative effects of false spring on P. cembra in the alpine treeline ecotone of the High Tatras, Slovakia
Veronika Lukasová1, Svetlana Varšová1, and Jaroslav Škvarenina2
Veronika Lukasová et al.
  • 1Earth Science Institute, Slovak Academy of Sciences, Bratislava, Slovakia (geofluka@savba.sk)
  • 2Faculty of Forestry, Technical University in Zvolen, Zvolen, Slovakia

Trees growing in mountain regions have evolved adaptations to withstand extreme winter conditions, primarily through dormancy and frost-avoidance mechanisms. However, frost events occurring after the growing season begins pose a substantial risk, as ice formation can damage newly developing tissues. A warm episode in late winter or early spring that triggers premature growth, followed by a subsequent hard freeze, is termed a false spring.

In the alpine treeline ecotone in the High Tatras, Pinus cembra, a native, long-lived mountain conifer, experienced such a false spring in 2024. Weather conditions in late winter led to an unusually early bursting of vegetative buds, which was interrupted by an 11-day cold spell. During this period, minimum air temperatures dropped to −8.3 °C, with a mean daily temperature of −2.0 °C, as recorded at the Skalnaté Pleso Observatory (1778 m a.s.l.). This freezing event occurred shortly after vegetative buds had lost their protective resin layer and begun to burst. The aim of this study was to assess the impact of this event on the life cycle of P. cembra.

In the weeks following the false spring, affected individuals exhibited pronounced needle yellowing and defoliation. While senescence and shedding of older needles typically occur between August and September, frost-induced stress led to the premature loss of approximately one-third of needles as early as May, at the beginning of the growing season. Although new shoots and needles developed normally, reproductive organs were severely affected. Cone bud formation was observed approximately two months after vegetative budburst; however, male (pollen) cones were degenerated and showed minimal pollination potential. Following the false spring, P. cembra individuals developed several seed cones, which subsequently abscised between July and August 2025. These cones were immature, small, and deformed.

Our results demonstrate that false spring events associated with ongoing climate change can disrupt the life cycles of P. cemba, substantially limiting its reproductive potential in the alpine treeline ecotone of the High Tatras.

Acknowledgement: This study was funded by the project VEGA 2/0048/25.

How to cite: Lukasová, V., Varšová, S., and Škvarenina, J.: Negative effects of false spring on P. cembra in the alpine treeline ecotone of the High Tatras, Slovakia, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-10758, https://doi.org/10.5194/egusphere-egu26-10758, 2026.