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Increased spring freezing vulnerability for alpine shrubs under early snowmelt
J A Wheeler1, G Hoch, A J Cortés
1WSL Institute for Snow and Avalanche Research SLF, 7260, Davos, Switzerland, julia.wheeler@slf.ch.
Oecologia
|January 18, 2014
Summary
Early snowmelt in alpine regions does not boost shrub growth but heightens the risk of lethal freezing damage for less resistant species. This impacts alpine dwarf shrub communities and their seasonal growth.
Area of Science:
- Ecology
- Plant Physiology
- Climate Change Biology
Background:
- Alpine dwarf shrubs are sensitive to snowmelt timing, with early exposure risking frost damage and reduced growth.
- Environmental factors like snow cover duration and elevation influence shrub phenology and vulnerability to spring freezes.
Purpose of the Study:
- To investigate how snow cover duration and elevation affect alpine shrub size and susceptibility to spring freezing.
- To model the frequency of spring freezing events for dominant alpine shrubs across elevational and snow microhabitat gradients.
Main Methods:
- Measured shrub biomass and size (Salix herbacea, Vaccinium myrtillus, V. uliginosum, Loiseleuria procumbens) in late spring.
- Determined species-specific freezing tolerance by exposing leaves to sub-zero temperatures.
- Extrapolated the frequency of lethal freezing events over 37 years using site-specific snowmelt data and long-term climate records.
Main Results:
- Shrub growth decreased with elevation but was not significantly affected by earlier snowmelt.
- Freezing resistance varied by species but not by elevation or snowmelt gradient.
- Potentially lethal freezing events occurred for three of four species, increasing with earlier snowmelt and higher elevation, especially on early snowbeds.
Conclusions:
- Earlier snowmelt in alpine environments increases the risk of lethal spring freezing for less cold-hardy dwarf shrub species.
- Snow microhabitat, not elevation, significantly drives snowmelt timing.
- Findings highlight the complex interactions between climate change, snow dynamics, and alpine plant vulnerability.
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