Research activity on Level II plots comprises visual assessment of crown condition, soil and soil solution analysis, foliar nutrient contents, forest growth and increment, atmospheric deposition, including passive sampling of air pollutants, meteorological monitoring and phenology, inventory of ground vegetation, visual ozone injury assessment, and other studies related to biodiversity, vitality and climate change.
The main objectives of the deposition measurements are to obtain an accurate knowledge about the deposition process in forest ecosystems and to give information for the mapping of critical loads. Samples obtained in throughfall and stemflow collectors supply long series of data about pH, conductivity, base cations, several anions, alkalinity and N total. Also Al, Mn, Fe and heavy metals are analyzed. There are available data from 1997, on average in 15‐
day periods.
Results show the variation in the atmospheric deposition data assessed in 13 Spanish plots, ranging from a wet temperate northwestern forest on acidic subtract (Galicia) to arid Mediterranean pure calcareous ecosystems (Alicante). The analysis of the results links the short‐term meteorological data variations, mainly rainfall and temperature, with vegetation cover, taking account quality and quantity of atmospheric deposition in several elements, studying in addition variation in time and possible trends in a possible climate change scenario.
INIA‐ CIFOR, Spain
87 Corresponding author: Minaya, Mayte (minaya@inia.es)
In: Kaennel Dobbertin, M. (Ed) 2009. Long‐term ecosystem research: Understanding the present to shape the future.
Int. Conference Zurich, Switzerland, 7‐10 Sept 2009. Abstracts. Birmensdorf, Swiss Federal Research Institute WSL. 118 pp.
Level II plots in Spain : atmospheric deposition
Poster session
1900
Daniel Lawrence Morovitz, Hans‐Peter Dietrich
A literature analysis of annual estimates on the spatial and temporal variability of mast production for Norway Spruce and European Beech trees in Bavaria was carried out for the years 1893–2008. The major objective of the study is to detect climate change effects on forests and the influence of reproduction on their growth and vitality measured in the long‐
term forest monitoring program in Bavaria (Level II).
Over the 115 year time span of the analysis four literary sources were used in order to create the timeline which clearly shows how masting behavior changes over time and space in the genetic provenances of Bavaria. In the literature, the production of mast has been shown to be dependent on climatic variables during the previous and current year of a masting event and the timeline can be used to make cautious inferences about weather patterns. Although the climatic conditions which induce masting are complex and vary among tree species, generalizations can be made. A warm and dry climate in the previous growing season during bud development can trigger a masting event in addition to a lack of damage from frost damage in spring plus warm, dry and windy conditions during the time of pollination. As a result of the increase in temperatures during the last 20 years it is not surprising that the timeline shows an increase in the production of mast since the early 1990s for both Norway spruce and European beech. The timeline also shows a notable absence in the mast production for European beech in southern Bavaria from the 1960s to the late 1980s. A similar decrease in mast production for Norway spruce was also seen but only starting during the 1970s.
Although the quality of the data throughout the years has significantly improved, the early values for the timeline should be cautiously interpreted as the format, methodology, and changing provenance borders of the masting reports have changed a number of times throughout the time span, thus causing some inaccuracies. Additionally, values for the timeline are generalizations for sometimes very large geographic regions and may not be representative for every location inside the provenance.
Despite these shortcomings, the timeline value in displaying masting data for such an unprecedented time frame is unquestionable and timelines of this length and geographic detail are not often found in the literature. Data from this timeline will be especially useful for those studying climate change effects on forests, forest growth and animal population dynamics.
Hans‐Peter Dietrich
Daniel Lawrence Morovitz
LWF, Freising, Germany
Corresponding author: Dietrich, Hans‐Peter (hans‐peter.dietrich@lwf.bayern.de)
Spatial and temporal variation in mast production estimates in Bavaria in 1893–2008 as an indicator for climate change
88 Poster session
In: Kaennel Dobbertin, M. (Ed) 2009. Long‐term ecosystem research: Understanding the present to shape the future.
Int. Conference Zurich, Switzerland, 7‐10 Sept 2009. Abstracts. Birmensdorf, Swiss Federal Research Institute WSL. 118 pp.
Radek Novotný, Vít Šrámek, Bohumír Lomský
Forests in the Czech Republic were significantly influenced by the anthropogenic air pollution. The negative influence of industrial production and electricity production based on fossil fuels resulted in vast damage to forest ecosystems. The decline peaked in the 1980s, mainly in the northern mountain regions – Ore Mountains, Lužické Mountains, Iser Mountains or Adler Mountains.
Regular assessment of defoliation and nutrition of young Norway spruce stands in the Ore Mountains was initiated in 1994. The main goal was to evaluate potential risks of sudden changes in large areas of even‐aged forests growing in regions historically damaged by air pollution, regularly influenced by climatic stresses and also stressed by low forest soil quality.
The survey is currently carried out on 20 plots in the mountain range area along a transect of more than 120 km.
The article presents the results of defoliation and nutrient contents for the period of 1994–
2008. It includes the evaluation of trends and prognoses of future development. The results show slight positive effects on crown defoliation and the decreasing influence of sulphur dioxide. On the other hand, problems with potassium, phosphorus or magnesium may occur in some locations in the future.
Bohumír Lomský
Radek Novotný
Vit Šrámek Forestry and Game Management Research Institute, Czech Republic
89 Corresponding author: Novotný, Radek (novotny@vulhm.cz)
In: Kaennel Dobbertin, M. (Ed) 2009. Long‐term ecosystem research: Understanding the present to shape the future.
Int. Conference Zurich, Switzerland, 7‐10 Sept 2009. Abstracts. Birmensdorf, Swiss Federal Research Institute WSL. 118 pp.
Vitality and nutrition of the young Norway spruce stands in the Ore Mountains
Poster session
1260
Walter Oberhuber, Andreas Gruber
Radial growth indices of trees are valuable long‐term proxy‐data of tree vitality. Several tree ring studies conducted in dry inner Alpine valleys have shown that precipitation in spring limits increment growth of Pinus sylvestris and severe drought during the growing season results in abrupt growth reductions and increased tree mortality of less competitive trees.
However, within the dry inner Alpine valley of the Inn river (Tyrol, Austria; mean annual precipitation and temperature 716 mm and 7.3°C, respectively) the record‐breaking heat‐
wave in summer 2003 had minor impact on tree growth. Therefore, repeated cellular analyses of cambial dynamics and xylogenesis were conducted to identify the time period, when climate factors primarily limit wood formation and cause reduced tree vigor. Wood formation dynamics was monitored by repeatedly taking small punched cores of the outermost tree rings (microcores) in weekly to 10 day intervals. Additionally, long‐term study plots were established at two sites differing in soil moisture characteristics, i.e., a xeric and dry‐mesic site, to focus on response of Pinus sylvestris to short‐term (intra‐annual) and long‐
term (inter‐annual) dynamics and changes of meteorological variables and to assess the impact of lag effects of both, favourable and unfavourable climate conditions, on tree growth.
First results obtained in 2007 and 2008 revealed that (i) Pinus sylvestris shows a high interannual variability in onset of cambial activity, varying from early to late April and (ii) maximum daily growth rates were reached about 2 weeks earlier at the xeric than at the dry‐
mesic site, peaking at the former site around early and mid May in 2007 and 2008, respectively. We assume that start of wood formation is triggered by air temperature in early spring, whereas temporal dynamics of xylem development is controlled by water availability throughout the growing season.
Climate warming is expected to cause an increase in the frequency and intensity of drought periods throughout the growing season and changes in the seasonal precipitation pattern in the future. Therefore, a combination of intra‐annual wood anatomical studies and long‐term monitoring of stem growth is required to evaluate plasticity of radial growth (onset, period of maximum growth, duration) to changing climate conditions and to detect lag effects of climate extremes (e.g., heat waves, drought, moist winter‐spring periods) on tree growth and mortality within dry inner Alpine valleys.
Andreas Gruber
Walter Oberhuber
University of Innsbruck, Austria
Corresponding author: Oberhuber, Walter (walter.oberhuber@uibk.ac.at)
Combining long‐ and short‐term approaches to evaluate impact of climate change on growth and mortality of Pinus sylvestris in an inner Alpine dry valley
90 Poster session
In: Kaennel Dobbertin, M. (Ed) 2009. Long‐term ecosystem research: Understanding the present to shape the future.
Int. Conference Zurich, Switzerland, 7‐10 Sept 2009. Abstracts. Birmensdorf, Swiss Federal Research Institute WSL. 118 pp.
Rock Ouimet, Louis Duchesne, Catherine Périé, Daniel Houle, Sylvie Tremblay
The Quebec Forest Ecosystem Study and Monitoring Network was initiated in 1986 when sugar maple dieback was observed in many forest stands throughout southern Quebec. A total of 31 monitoring plots distributed throughout the commercial forest are making up the network. They are generally located close to meteorological and air quality monitoring stations. Plots vary between 0.25 and 0.5 ha in size and are surrounded by a buffer strip of at least 100 m wide. Three forest watersheds representative of the three main bioclimatic domains of the Quebec province are also being intensively monitored.
This high‐level intensive monitoring network is unique in Canada. It also complete the other more extensive forest inventory networks in the province of Quebec. After 20 years of weather, atmospheric depositions, forest vegetation, and soils monitoring, several changes in forest growth and composition have been observed. These changes can be explained, at least partly, by detection of the impacts of predisposing (e.g., atmospheric acid deposition) or triggering (e.g., extreme weather events) environmental stress factors.
Selected examples, including changes in sugar maple stand structure and composition, assessment of forest resilience to acid deposition, and assessment of potential impacts of forest harvesting and of climatic events will be shown to demonstrate the capacity of field monitoring for detecting the impact of environmental stresses on forest growth, dynamics, and resilience.
Louis Duchesne
Rock Ouimet Ministry of Natural Resources and Fauna, Quebec, Canada
91 Corresponding author: Ouimet, Rock (rock.ouimet@mrnf.gouv.qc.ca)
In: Kaennel Dobbertin, M. (Ed) 2009. Long‐term ecosystem research: Understanding the present to shape the future.
Int. Conference Zurich, Switzerland, 7‐10 Sept 2009. Abstracts. Birmensdorf, Swiss Federal Research Institute WSL. 118 pp.
Regional monitoring with plot networks: a practical tool for implementing research and reporting on forest ecosystem changes and their causes in Quebec, Canada
Poster session
1503
Roland Pesch, Winfried Schröder, Marcel Holy
The presented study focuses on the spatiotemporal analysis of atmospheric metal bioaccumulation in German mosses. Since 1990 such data has been collected within the UN ECE Heavy Metals in Mosses Surveys in order to map the cross border patterns of heavy metal bioaccumulation across Europe. The study furthermore analyses the spatial variance of metal bioaccumulation with regard to local and regional site properties. Special focus hereby lies on the correlation of metal concentration in mosses and in depositions.
In the German moss surveys of 1990, 1995, 2000 and 2005 all sampling sites were described with regard to aspects seen as relevant in the mandatory guideline (e.g., topography, vegetation and proximity of emission sources). Together with the measurements on up to 40 trace elements these metadata were combined with surface information on land use, precipitation, and soil in a GIS environment. The spatial structure of metal bioaccumulation was analysed and modelled by variogram analyses and then mapped by different kriging techniques. Furthermore, different types of multi metal indices (MMI) were derived from both measurements and estimated raster data with help of percentile statistics. The statistical association of the metal bioaccumulation and local or regional characteristics was analysed by bivariate correlation analysis and decision tree models.
The results of the quality controlled chemical analyses show a significant decrease of the metal bioaccumulation in Germany from 1990 to 2000. From 2000 to 2005 a further decrease can be stated for Hg, Pb and Ti. However, a significant increase for Cd, Cr, Cu, Sb and Zn can be observed. This especially holds true for Cr (+160%) that almost reaches concentrations in mosses as high as in 1990. Except for Cr the metal loads in the 2005 survey show spatial distributions similar to those in 1990, 1995 and 2000. Hot spots are mostly found in the urbanised and industrially influenced Ruhr Area, the densely populated Rhein‐Main region and in the industrially influenced regions of former East Germany (e.g., Halle‐Leipzig region).
The spatial variance of the metal bioaccumulation can mainly be explained by site‐specific (moss species, canopy drip effects) and site‐surrounding (land use, depositions, emissions) characteristics.
Compared to other environmental monitoring and modelling programmes the moss surveys registered increasing concentrations of toxic metal elements between 1990 and 2005.
Contrary to deposition measurements that exhibit a higher temporal resolution the moss surveys provide measurement data on a wide range of elements with a high spatial resolution.
Marcel Holy
Roland Pesch
Winfried Schröder
University of Vechta, Germany
Corresponding author: Holy, Marcel (mholy@iuw.uni‐vechta.de)
Trends in metal bioaccumulation from 1990 to 2005 in Germany
92 Poster session
In: Kaennel Dobbertin, M. (Ed) 2009. Long‐term ecosystem research: Understanding the present to shape the future.
Int. Conference Zurich, Switzerland, 7‐10 Sept 2009. Abstracts. Birmensdorf, Swiss Federal Research Institute WSL. 118 pp.
Martine Rebetez, Valentine Renaud
LWF (Long‐term Forest Ecosystem Research) meteorological data have been collected since 1997 in 17 plots in Switzerland, 14 of which are used for the present research. They represent different locations, orientations and elevations, from the Jura Mountains to the southern side of the Alps, composed of deciduous, coniferous and mixed forests. Each of these regions is distinguished by its flora and fauna, determined by climate, environment (relief, exposition, altitude, ground, soil, etc.), evolution and human presence.
Meteorological measurements were carried out under the canopy at the observation plots, and in an open field outside the plots. For the latter, the meteorological station was always located less than two km from the plot, in a region of similar topography (altitude, slope orientation, distance from the bottom of a valley, etc.). The measurements for each site, available in real time, have been stored and treated in a database.
In the present research, we compare open‐site and below‐canopy climatic conditions from these 14 forest sites. We compare open‐site and below‐canopy measurements of air temperature [C°], PAR (Photosynthetically Active Radiation [W/m2]), relative humidity [%] and wind speed [m/s]. We analyze minimum, maximum and average daily values for air temperature and humidity, maximum values for wind and PAR.
We show clear differences between below‐canopy and open‐site climate. These differences can be explained by several factors such as the vegetation type, the orientation (i.e., north‐
or south‐oriented slope), the season, the soil type or the absolute temperature value.
Martine Rebetez
Valentine Renaud Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Switzerland
93 Corresponding author: Rebetez, Martine (rebetez@wsl.ch)
In: Kaennel Dobbertin, M. (Ed) 2009. Long‐term ecosystem research: Understanding the present to shape the future.
Int. Conference Zurich, Switzerland, 7‐10 Sept 2009. Abstracts. Birmensdorf, Swiss Federal Research Institute WSL. 118 pp.
Climate at Swiss LWF forest sites
Poster session
1628
Cristina Salvadori (1), Giorgio Maresi (1), Mauro Confalonieri (2), Stefano Minerbi (3)
In a typically alpine region such as Trentino‐South Tyrol (North Italy), forests cover more than 50% of land and affect economy, landscape and culture. Therefore the monitoring and the evaluation of forest health is extremely important. Enhanced by the general concern about forest decline, woodland protection studies started in the 1980s with the first observations on crown defoliation and discoloration. Furthermore, in the last two decades an extensive survey of known damages has been carried out in both the Autonomous Provinces of Bolzano and Trento.
In 1992 the two Provinces joined the International Co‐operative Programme of Integrated Monitoring (ICP‐IM, UN‐ECE) with four selected areas – two in subalpine Norway spruce woodland (Renon and Lavazè Pass, respectively IT01 and IT03), and two in thermophilous oak woodland (Monticolo and Pomarolo, respectively IT02 and IT04). This monitoring aimed to investigate the state and the biodiversity of alpine nature‐like structured forests in relation to air pollution effects, anthropogenic stresses and climate changes.
During the survey period air quality investigation reported a reduced presence of SO2 and NO2 and high values of O3, but without associated damage. In the areas pollution factors were not detected and pH values showed a clear increasing trend in the last years. Crown condition assessment has been pointing out a good status during the observation period: the trees ranged mainly in the classes 0–1 with single cases in class 2 or 3, without any negative trend and with several recovering episodes. In all the plots pests and pathogens were regularly monitored. Deciduous species in IT02 and IT04 were more affected both by biotic agents and by abiotic stress such as drought, especially after the 2003 summer; at IT01 and IT03 mechanical and unknown damages were more common.
One of the most important topics is the evaluation of biodiversity in the target areas. The high number of collected species allowed estimating the similarity of structure of the studied communities, which as expected was low between thermophilous and subalpine coenosis.
Moreover, in the last years many studies have pointed out the role of several organisms as bioindicators for evaluating health condition of ecosystems.
Anomalous weather behaviours were the most effective in producing stress on trees. So, climate change could be considered as the major constraining factor for forest health, both in the short and the long term. In this context, continuous intensive and extensive monitoring allows to assess the real role of the stress agents (pathogens, pests, drought etc.), which could affect wood development and stability, emphasizing also ageing process in many stands. Long‐term biodiversity investigations, i.e., on arthropods and macromycetes, and the use of bioindication methods could help better understand ecological mechanisms involved in forest homeostasis.
Walter Seidling, Wolfgang Beck, Daniel Ziche
Crown condition is an easily recorded and commonly used indicator of tree performance.
Due to its extensive lack of specificity towards any environmental factor its temporal, spatial and species specific variation cannot be simply explained. Additionally, still some methodological uncertainties with respect to its visual assessment have to be considered over large areas and/or over time.
In contrast, annual radial increment of stem wood can accurately be measured if – at least – cores are available. However, wood increment is controlled by a variety of environmental conditions. Especially the impact of climate has widely been explored in dendroecological approaches over the last decades.
Data collected within the frame of the transnational monitoring of ICP‐Forests are a vast source of defoliation estimates under a broad variety of environmental conditions. In addition, at Level II plots, continuously collected data on different ecosystem compartments provide relevant information on environmental conditions. Between 2005 and 2008 at almost all German Level II sites two increment cores from 20 individuals were taken and analysed.
These data are jointly investigated within different cross‐cut and longitudinal approaches. In connection with large‐scale inventories, the results may bear considerable prospects for up‐
scaling approaches.
The investigated main hypotheses are:
‐ Are there general relationships between the degree of defoliation and the level of stem
‐ Are there general relationships between the degree of defoliation and the level of stem