scholarly journals Spatial variability of close-to-primeval Fagus–Abies–Picea forests in the Western Carpathians (Central Europe): a step towards a generalised pattern

2014 ◽  
Vol 134 (2) ◽  
pp. 235-246 ◽  
Author(s):  
Jarosław G. Paluch ◽  
Zbigniew Kołodziej ◽  
Maciej Pach ◽  
Rafał Jastrzębski
Geomorphology ◽  
2020 ◽  
Vol 364 ◽  
pp. 107248 ◽  
Author(s):  
Tomáš Pánek ◽  
Jozef Minár ◽  
Ladislav Vitovič ◽  
Michal Břežný

2018 ◽  
Vol 19 (6) ◽  
pp. 1007-1025 ◽  
Author(s):  
Joël Arnault ◽  
Thomas Rummler ◽  
Florian Baur ◽  
Sebastian Lerch ◽  
Sven Wagner ◽  
...  

Abstract Precipitation is affected by soil moisture spatial variability. However, this variability is not well represented in atmospheric models that do not consider soil moisture transport as a three-dimensional process. This study investigates the sensitivity of precipitation to the uncertainty in the representation of terrestrial water flow. The tools used for this investigation are the Weather Research and Forecasting (WRF) Model and its hydrologically enhanced version, WRF-Hydro, applied over central Europe during April–October 2008. The model grid is convection permitting, with a horizontal spacing of 2.8 km. The WRF-Hydro subgrid employs a 280-m resolution to resolve lateral terrestrial water flow. A WRF/WRF-Hydro ensemble is constructed by modifying the parameter controlling the partitioning between surface runoff and infiltration and by varying the planetary boundary layer (PBL) scheme. This ensemble represents terrestrial water flow uncertainty originating from the consideration of resolved lateral flow, terrestrial water flow uncertainty in the vertical direction, and turbulence parameterization uncertainty. The uncertainty of terrestrial water flow noticeably increases the normalized ensemble spread of daily precipitation where topography is moderate, surface flux spatial variability is high, and the weather regime is dominated by local processes. The adjusted continuous ranked probability score shows that the PBL uncertainty improves the skill of an ensemble subset in reproducing daily precipitation from the E-OBS observational product by 16%–20%. In comparison to WRF, WRF-Hydro improves this skill by 0.4%–0.7%. The reproduction of observed daily discharge with Nash–Sutcliffe model efficiency coefficients generally above 0.3 demonstrates the potential of WRF-Hydro in hydrological science.


Zootaxa ◽  
2017 ◽  
Vol 4238 (4) ◽  
pp. 597 ◽  
Author(s):  
FABIO CIANFERONI ◽  
MARGHERITA NORBIATO ◽  
MARCO DOGLIOTTI

Salda henschii (Reuter, 1891) is a boreo-montane species of Saldidae (Hemiptera: Heteroptera) restricted to mountain bogs and streams in central Europe (e.g., Western Carpathians, Alps) and to freshwater wetlands in lowland coastal areas in northern Europe (Fennoscandia); it is a vicariant of the arctic (Holarctic) element S. sahlbergi Reuter, 1875 (Hoberlandt 1977; Schuh et al. 1987; Péricart 1990; Lindskog 1991; Vinokurov 2010). 


Volcanica ◽  
2021 ◽  
pp. 149-187
Author(s):  
Jacky Bouloton

Almandine-rich garnets from a Neogene andesite of Slovakia can be divided into two main types. Garnet megacrysts are magmatic and form a chemically homogeneous group that contains, on average, about 5 wt% CaO and 4.5 wt% MgO as petrogenetically significant components. Garnets occurring in lithic fragments and garnets aggregated in garnetite lenses are characterised by Ca-poor cores (CaO <= 2 wt%) that testify for a two-step history and correspond respectively to inherited pre-anatectic and peritectic garnets. Available experimental data show that the composition of magmatic garnet megacrysts is compatible with a peritectic origin, through the fluid-absent melting of an immature metasedimentary protolith or a tonalitic gneiss. However, thermal evolution evidenced by zircons shielded in garnet rather suggests that garnet nucleated and grew by cooling of a hybrid magma pool, resulting from the complete mixing of crust- and mantle-derived melts.


Palynology ◽  
2019 ◽  
Vol 44 (2) ◽  
pp. 355-368 ◽  
Author(s):  
Sambor Czerwiński ◽  
Włodzimierz Margielewski ◽  
Mariusz Gałka ◽  
Piotr Kołaczek

The Holocene ◽  
2017 ◽  
Vol 28 (4) ◽  
pp. 595-608 ◽  
Author(s):  
Piotr Kołaczek ◽  
Monika Karpińska-Kołaczek ◽  
Katarzyna Marcisz ◽  
Mariusz Gałka ◽  
Mariusz Lamentowicz

2011 ◽  
Vol 60 (2) ◽  
pp. 185-189 ◽  
Author(s):  
Vítězslav Plášek ◽  
Eva Novozámská

Historical and recent occurrence of epixylous moss Buxbaumia viridis in the Javorníky Mts. and the Vsetínské vrchy hills (Western Carpathians) The epixylous moss Buxbaumia viridis (Moug. ex Lam. & DC.) Brid. ex Moug. & Nestl. is considered an endangered or vulnerable species in all countries in the Central Europe. In the Czech part of the Western Carpathians the species was recorded very occasionally in the twentieth century. In 2011 field monitoring of the species on historically known localities in Javorníky Mts. and the Vsetínské vrchy hills was carried out. As a result, six localities of B. viridis have been recorded in this region. Precise localization, number of and ecological data are given.


2018 ◽  
Vol 49 (1) ◽  
pp. 243-246
Author(s):  
Andrea Lešová ◽  
Peter Lešo ◽  
Rudolf Kropil

Abstract A dead individual of C. leucodon was found in the Lower Tatra Mts. (Central Slovakia, Western Carpathians). The site is situated in the westernmost part of the main ridge of this mountain range at the altitude of 1,150 m a. s. l. The prevaling habitat is a mountain meadow surrounded by spruce and beach-maple forests. In Central Europe, the species usually occurs in lowland and hilly areas, records above 600 m a. s. l. are very rare. The finding of C. leucodon in the mountain ridge at this extraordinary altitude is the highest documented occurrence of the species in the Western Carpathians and Central Europe as well. It is probably related to expansion of the species range in the recent decades and its spreading to higher altitudes, which is more common at the southern border of its distribution area.


2021 ◽  
Vol 55 (2) ◽  
Author(s):  
Piotr Mleczko ◽  
Maciej Kozak ◽  
Filip Karpowicz

Investigations carried out in recent years have provided new data on the localities of some rare hypogeous fungi in Central Europe. In this study, we present new localities of <em>Leucangium carthusianum</em>, <em>Melanogaster luteus</em>, and <em>Rhizopogon </em><em>melanogastroides</em>, two of which are new for Poland. Sporocarps of <em>L. carthusianum </em>were found in seven new localities in mixed and coniferous forests in the Western Carpathians as well as in Sudetes. In Poland, the species was also recorded in a mixed forest in the Kraków-Częstochowa Upland. Fir, <em>Abies alba</em>, accompanied the fungus in almost all known localities. Three localities of <em>M. luteus </em>were found in the Polish Western and Eastern Carpathians in <em>Alnus incana </em>communities mostly associated with streams. Knowledge of the distribution of this species in Europe is incomplete due to the complicated taxonomic history; nevertheless, it is regarded as rare, despite its wide distribution. One new locality of <em>R. melanogastroides </em>recorded in the Tatra Mts, Western Carpathians, is the fourth known to date. This species is mostly associated with <em>Pinus mugo </em>in high mountain localities (the Alps, the Tatra Mts). In this study, detailed descriptions and illustrations of the macro- and micromorphological features of the species are provided.


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