Climate-growth relationships of Norway Spruce and silver fir in primary forests of the Croatian Dinaric mountains

2020 ◽  
Vol 288-289 ◽  
pp. 108000
Author(s):  
Krešimir Begović ◽  
Miloš Rydval ◽  
Stjepan Mikac ◽  
Stipan Čupić ◽  
Kristyna Svobodova ◽  
...  
Forests ◽  
2021 ◽  
Vol 12 (7) ◽  
pp. 823
Author(s):  
Anna Zielonka ◽  
Marek Drewnik ◽  
Łukasz Musielok ◽  
Marcin K. Dyderski ◽  
Dariusz Struzik ◽  
...  

Forest ecosystems significantly contribute to the global organic carbon (OC) pool, exhibiting high spatial heterogeneity in this respect. Some of the components of the OC pool in a forest (woody aboveground biomass (wAGB), coarse root biomass (CRB)) can be relatively easily estimated using readily available data from land observation and forest inventories, while some of the components of the OC pool are very difficult to determine (fine root biomass (FRB) and soil organic matter (SOM) stock). The main objectives of our study were to: (1) estimate the SOM stock; (2) estimate FRB; and (3) assess the relationship between both biotic (wAGB, forest age, foliage, stand density) and abiotic factors (climatic conditions, relief, soil properties) and SOM stocks and FRB in temperate forests in the Western Carpathians consisting of European beech, Norway spruce, and silver fir (32 forest inventory plots in total). We uncovered the highest wAGB in beech forests and highest SOM stocks under beech forest. FRB was the highest under fir forest. We noted a considerable impact of stand density on SOM stocks, particularly in beech and spruce forests. FRB content was mostly impacted by stand density only in beech forests without any discernible effects on other forest characteristics. We discovered significant impacts of relief-dependent factors and SOM stocks at all the studied sites. Our biomass and carbon models informed by more detailed environmental data led to reduce the uncertainty in over- and underestimation in Cambisols under beech, spruce, and fir forests for mountain temperate forest carbon pools.


2013 ◽  
Vol 377 (1-2) ◽  
pp. 63-81 ◽  
Author(s):  
C. Vergani ◽  
E. A. Chiaradia ◽  
C. Bassanelli ◽  
G. B. Bischetti

Author(s):  
G. Landmann ◽  
G. D. Bert ◽  
J. C. Pierrat ◽  
M. Becker ◽  
M. Bonneau ◽  
...  
Keyword(s):  

2017 ◽  
Vol 63 (No. 2) ◽  
pp. 75-87 ◽  
Author(s):  
Fulín Martin ◽  
Novotný Petr ◽  
Podrázský Vilém ◽  
Beran František ◽  
Dostál Jaroslav ◽  
...  

The article aims to evaluate the research provenance plot established in 1980 in locality No. 214 – Hrubá Skála (in the north of the Czech Republic), where nine provenances of grand fir (Abies grandis (Douglas ex D. Don) Lindley) provided in the framework of the International Union of Forest Research Organizations project, and one provenance of grand fir, Norway spruce, silver fir and Douglas-fir from a standard commercial source are tested. We present the results of tree height, stem DBH, stem volume production and health status after 36 years. The results correspond with similar experiments in the Czech Republic and abroad and suggest that grand fir provenances from Vancouver Island (British Columbia, Canada) and the Washington (USA) State coastal region show the best production features, while the Oregon Cascades, Idaho and Montana provenances grow more slowly. Comparison with other tree species indicates that the production of grand fir at the investigated age exceeds the production of both Norway spruce and silver fir, and equalizes or gently exceeds even Douglas-fir.


2012 ◽  
Vol 30 (2) ◽  
pp. 73-83 ◽  
Author(s):  
Christoph Dittmar ◽  
Thomas Eißing ◽  
Andreas Rothe

2009 ◽  
Vol 33 (-1) ◽  
pp. 49-57 ◽  
Author(s):  
Edward Feliksik ◽  
Sławomir Wilczyński

The Effect of Climate on Tree-Ring Chronologies of Native and Nonnative Tree Species Growing Under Homogenous Site ConditionsDendroclimatic studies were carried out in the experimental stands composed of many tree species situated in the Polish part of the Baltic sea-coast. Increment cores were taken from a 100-years old trees of 2 native species: Norway spruce (Picea abies (L.) Karst.), and Scots pine (Pinus sylvestrisL.) and 3 nonnative species: Douglas fir (Pseudotsuga menziesii(Mirb.) Franco), Sitka spruce (Picea sitchensis(Bong.) Carr.) and Silver fir (Abies albaMill.). Thirty trees of each species were cored. The relationships between the diameter increment and the thermal and pluvial conditions during the period from 1925 to 2005 were analyzed on the basis of standardized tree-ring chronologies and climatic data. It was found that precipitation and temperature of the growing season and months preceding that season affected the annual diameter increment of all investigated tree species. The current year winter and early spring temperatures as well as February and August precipitation had a similar effect on the variation of diameter increment of trees. On the other hand thermal and pluvial conditions of the current year June differentiated the increment rhythm of individual species. A very strong negative effect on diameter growth of trees was observed in the case of winter and early spring frosts. Norway spruce turned out to be a species most resistant to low temperatures. The investigated tree species, especially Norway spruce, was susceptible to water deficiency in the soil during spring and summer. In the case of Scots pine a high precipitation in June stimulated its growth. The diameter increments of Douglas fir, Sitka spruce, Scots pine, and Silver fir were more strongly connected with air temperature than with precipitation. So called all-species chronology of tree-ring width, constructed during this study, permitted to verify the factors having a similar effect on growth response of the investigated tree species. It reflected the mutual characteristics of diameter increments of trees of various species.


2012 ◽  
Vol 274 ◽  
pp. 99-107 ◽  
Author(s):  
Berthold Metzler ◽  
Ulrike Hecht ◽  
Michael Nill ◽  
Franka Brüchert ◽  
Siegfried Fink ◽  
...  
Keyword(s):  

2012 ◽  
Vol 163 (6) ◽  
pp. 210-221 ◽  
Author(s):  
Caroline Heiri ◽  
Urs-Beat Brändli ◽  
Harald Bugmann ◽  
Peter Brang

Do strict forest reserves feature more naturalness than the Swiss forest? In natural forest reserves (NFR), forests develop in the absence of direct human interference, primarily management. This increases their naturalness and should – in the long run – allow forests to regain primeval attributes. Based on stand structural data from the third National Forest Inventory (NFI) and 25 NFR in Switzerland, we investigate 1) whether NFR feature more naturalness than managed forests, 2) whether the naturalness of Swiss forests increases with the time elapsed since the cessation of management, and 3) to what extent NFR differ from Swiss forests that have not been managed during several decades. Thereby, we focus on the four main forest types beech, silver fir-beech, silver fir-Norway spruce and Norway spruce forests, and furthermore group the data according to the time since the last intervention (0–20, 21–50 and > 50 years.). The structural features investigated differ only slightly between NFR and managed forest (0–20 years). NFR feature a higher abundance of “giant” trees (dbh ≥ 80 cm), higher stem numbers and greater basal area, and thus a higher growing stock. The abundance of snags, however, is indistinguishable between the two types of forests. Naturalness in Swiss forests increases only slightly with time since the last intervention, indicated by a higher abundance of small snags and a slightly higher number of giant trees. By contrast, clear differences can be seen between NFR in which no intervention has taken place for at least 50 years, and other forests abandoned for a similarly long time, with NFR showing lower stem numbers, greater basal area and higher numbers of giant trees. Many of the investigated reserves are still affected by former management and are – from the point of view of primeval forest dynamics – still quite “young”. According to their naturalness, the NFR range between managed and primeval forests, although to date they are still closer to the former. Nevertheless, the differences found in our study indicate a steady development of the NFR towards stand structures that are characteristic of primeval forests.


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