Abstract

Global warming is considered as a phenomenon having a negative effect on animals living in cold climate. However, herbivorous species inhabiting cold zones may potentially benefit from increase of temperature as this influence duration of vegetation period and increase food resources. In this study, we analyze the impact of climate factors on the long-term dynamics of an isolated and unhunted population of the Tatra chamois Rupicapra rupicapra tatrica. The population growth rate, based on autumnal chamois counting carried out from 1957 to 2016, were correlated with a set of climatic variables. We tested the hypothesis that high temperatures in summer could have a positive impact on the population, since they influence vegetation growth, which ensure food resources. On the other hand, heavy falls of snow and long-lasting and deep snow cover could adversely affect the population by reducing population survival during the winter. The results of this study indicate that climatic variables best explaining the autoregressed population growth rate (from the autumn of year t-1 to the autumn of year t) were the mean summer temperature of year t-1: the population increase was greater following a warmer summer in year t-1 and, in lower extent, the total precipitation during winter: the population decrease was greater following a winter with heavy snowfall. Duration and thickness of snow cover have no negative effect on population growth rate. The results indicate that the population dynamic of the Tatra chamois is determined in the long term by weather conditions, mainly by temperature, when kids are birthing and growing. The results of this work highlight that climatic changes may be responsible for the population dynamic of high-mountain species. Climate warming may lead to increase in duration of vegetation period in cold climatic zones, what may in turn have positive effect on herbivorous species, which relay upon food resources limited by low temperatures within vegetation period.

Highlights

  • During the last 100 years, the mean global temperature has risen by about 0.6 °C and this has had a significant effect on the phenology of plant flowering, the functioning of populations, and the migration of animals (Root et al 2003; Karl and Electronic supplementary material The online version of this article contains supplementary material, which is available to authorized users.Trenberth 2003)

  • The fauna of mountains is associated with specific vegetation zones, and the presence of these is determined by climatic conditions

  • From the start of Tatra chamois counts until the turn of the century, despite high variation, the long-term trend of population growth rate was stable (Fig. 2)

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Summary

Introduction

Current scenarios predict a further increase in temperature, which may lead to the synergism of rapid temperature rise and other stresses, in particular, habitat destruction. Species associated with high mountain environments and the Arctic region are most at risk in the context of these forecast climate changes (Beniston et al 1997; Lemoine et al 2007). The fauna of mountains is associated with specific vegetation zones, and the presence of these is determined by climatic conditions. Ongoing global warming will presumably cause the elevation of the upper limits of vegetation layers to rise, in consequence leading to the disappearance of species associated with specific zonal habitat conditions (Beniston et al 1997; Thomas et al 2004)

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