Abstract

The Arctic is one of the ecosystems most affected by climate change; in particular, winter temperatures and precipitation are predicted to increase with consequent changes to snow cover depth and duration. Whether the snow-free period will be shortened or prolonged depends on the extent and temporal patterns of the temperature and precipitation rise; resulting changes will likely affect plant growth with cascading effects throughout the ecosystem. We experimentally manipulated snow regimes using snow fences and shoveling and assessed aboveground size of eight common high arctic plant species weekly throughout the summer. We demonstrated that plant growth responded to snow regime, and that air temperature sum during the snow free period was the best predictor for plant size. The majority of our studied species showed periodic growth; increases in plant size stopped after certain cumulative temperatures were obtained. Plants in early snow-free treatments without additional spring warming were smaller than controls. Response to deeper snow with later melt-out varied between species and categorizing responses by growth forms or habitat associations did not reveal generic trends. We therefore stress the importance of examining responses at the species level, since generalized predictions of aboveground growth responses to changing snow regimes cannot be made.

Highlights

  • Snow depth is one of the drivers governing growing season length in the Arctic [1,2,3,4]

  • Chapin and Shaver [36] concluded that growth of different species is limited by speciesspecific adaptations and competition, probably leading to observed individualistic responses to environmental manipulations which could not be explained by growth form, as was the case in our study

  • We demonstrated that air temperature sums since melt-out best explained aboveground growth for all species in most snow regimes

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Summary

Introduction

Snow depth is one of the drivers governing growing season length in the Arctic [1,2,3,4] It affects winter soil temperatures through thermal insulation of soil and vegetation, controlling nutrient turnover rates and availability [5], as well as soil moisture during the early growing season [3,4]. These are all factors influencing plant growth [6], and the carbon sink capacity of arctic ecosystems which are nutrient, moisture, and light (i.e. snow-free season) limited [7,8,9,10]. The Intergovernmental Panel on Climate Change (IPCC) emphasizes an increase of winter precipitation and winter temperatures in the Arctic in its Fourth Assessment Report [13], and these findings are backed up by their 2013 report

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