In this study, the snow conditions of South-Central Slovakia (Inner Western Carpathians; temperate zone) were analyzed to assess the suitability for ski slope operations without snow production under 1000 m a.s.l. For the study site of the Košútka Ski Centre, meteorological conditions for snowmaking, snowpack characteristics, and snow water equivalent (SWE) compared with seasonal precipitation were identified. To identify the months suitable for snowmaking, the number of potential snowmaking days (PSD) and the required number of snowmaking days (RNSD) were calculated for six winter seasons from 2010-2011 to 2015-2016. The results showed that the conditions of natural snow cover were not appropriate for ski slope operation because of a low natural snow depth. For the Košútka Ski Centre, it was concluded that the essential base layer snowmaking for ski slope operation is possible only for a few days in the winter season because of the increasing mean value of the mean average daily temperature and the consequently higher occurrence of liquid precipitation in the winter season. Essential high snow production results in the heterogeneous distribution of snow on the ski slope, and in high snow depth, density, and SWE of the ski slope snowpack, and in prolonged melting.
In our paper we deal with the changes in the rainfall interception process of a climax spruce forest in the growing season (approximately from May to October) during its die-back. Experimental data were collected at the research plot of Červenec situated in the West Tatras at an elevation of 1,420 m a.s.l. in the years from 2013 to 2015. Net precipitation was monitored at three localities in both living and dead forests: canopy gap, dripping zone at crown periphery and central zone of a crown. Gross precipitation was recorded at an open forest area (with a diameter of 1–2 tree heights). The comparison of net precipitation in the stands revealed the highest values in the dripping zone at crown periphery of the living forest due to its increase by occult (horizontal) precipitation and transport of rainfall captured in the crown to its periphery. The values in the growing season of 2014 exceeded also gross precipitation. The total interception loss (total gross – net precipitation in % of gross precipitation) the canopy gap during the monitored period was 10.1% in the living and 18.3% in the dead stand, in the dripping zone at crown periphery it was 1.7% in the living and 20.5% in the dead stand, and in the central zone of a crown it was 70.6% in the living and 59.9% in the dead stand. Forest die-back had an effect on the distribution of precipitation under canopy. The comparison of mean interception values at three localities of the living and dead stands revealed significant differences between the stands in all cases (
Snow production results in high volume of snow that is remaining on the low-elevation ski pistes after snowmelt of natural snow on the off-piste sites. The aim of this study was to identify snow/ice depth, snow density, and snow water equivalent of remaining ski piste snowpack to calculate and to compare snow ablation water volume with potential infiltration on the ski piste area at South-Central Slovak ski center Košútka (Inner Western Carpathians; temperate zone). Snow ablation water volume was calculated from manual snow depth and density measurements, which were performed at the end of five winter seasons 2010–2011 to 2015–2016, except for season 2013–2014. The laser diffraction analyzes were carried out to identify soil grain size and subsequently the hydraulic conductivity of soil to calculate the infiltration. The average rate of water movement through soil was seven times as high as five seasons’ average ablation rate of ski piste snowpack; nevertheless, the ski piste area was potentially able to infiltrate only 47% of snow ablation water volume on average. Limitation for infiltration was frozen soil and ice layers below the ski piste snowpack and low snow-free area at the beginning of the studied ablation period.
Presented paper deals with the quantification of greenhouse gas emissions from forest fires. The investigation was based on the inventory methodology of the Intergovernmental Panel on Climate Change from the year 2006. We describe the proposal of our methodology for estimating the required biomass for modelling (using the available literature as well as Sibyla growth simulator), and subsequently we describe the modelling process with fuel models (using FCCS model) as well as the resulting greenhouse gas emissions (using FARSITE and CONSUME model) for the selected site called Krompľa -Tri Kopce in the Slovak Paradise National Park in the cadastral area of Hrabušice, in which fire destroyed an area of 80 ha in the year 2000. From the forest typology point of view, following groups of forest types are dominant at the site: Fagetum dealpinum (Limestone beech forests); Fageto-Abietum (Neutrophilous beech forests), Pinetum dealpinum (Carpathian relict calcicolous Scots pine forests), Fagetum typicum (Limestone beech forests), Fageto-Aceretum (Mixed ravine and slope forests). The results indicate that the conceptions differ in the quantification of biomass available for burning, which was underestimated in the case of TIER 1 conception in comparison to TIER 2 and TIER 3, and also in the quantification of emissions. The emissions produced during the flameless burning phase were underestimated, while the CO2 emissions were slightly overestimated when comparing TIER 2 and TIER 3 approaches. The final assessment of the whole process points out at the problematic issues in the calculations of GHG emissions.
Climate change affects snowpack properties indirectly through the greater need for artificial snow production for ski centers. The seasonal snowpacks at five ski centers in Central Slovakia were examined over the course of three winter seasons to identify and compare the seasonal development and inter-seasonal and spatial variability of depth average snow density of ski piste snow and uncompacted natural snow. The spatial variability in the ski piste snow density was analyzed in relation to the snow depth and snow lances at the Košútka ski center using GIS. A special snow tube for high-density snowpack sampling was developed (named the MM snow tube) and tested against the commonly used VS-43 snow tube. Measurements showed that the MM snow tube was constructed appropriately and had comparable precision. Significant differences in mean snow density were identified for the studied snow types. The similar rates of increase for the densities of the ski piste snow and uncompacted natural snow suggested that the key density differences stem from the artificial (machine-made) versus natural snow versus processes after and not densification due to snow grooming machines and skiers, which was relevant only for ski piste snow. The ski piste snow density increased on slope with decreasing snow depth (18 kg/m³ per each 10 cm), while snow depth decreased 2 cm per each meter from the center of snow lances. Mean three seasons maximal measured density of ski piste snow was 917 ± 58 kg/m³ the density of ice. This study increases the understanding of the snowpack development processes in a manipulated mountainous environment through examinations of temporal and spatial variability in snow densities and an investigation into the development of natural and ski piste snow densities over the winter season.
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