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För klimatet spelar skogen en viktig roll eftersom den binder in koldioxid från atmosfären. Genom fotosyntes binds kolet in i biomassan och när organiskt material bryts ned bidrar det till kolinlagringar i marken. Idag finns det många studier om skogens kolinlagringar, men de undersöker endast nettoinbindningen av kolet i skogen och få studier visar hur mycket kol som totalt är inlagrat i en skog. Det finns inga studier om hur det ser ut i Sverige och det finns få studier som visar på skillnaden i kolinlagring mellan en produktionsskog och en urskog. I den här litteraturstudien presenterar jag hur mycket kol som är inbundet i den svenska skogen och hur det skiljer sig mellan produktionsskog och urskog. Genom att applicera data från en studie som undersökte hur mycket kol som är inbundet i skogen i Kanada på den svenska skogen kom jag fram till att det finns totalt mellan 5 413 och 6 798 miljoner ton kol inlagrat i den svenska skogen, men mer kol skulle kunna lagras. Medelåldern för när träd slutavverkas är i Sverige 101 år. Jag kom fram till att det lagras in ungefär 53 till 75 ton mer kol per hektar i en skog som är äldre än 140 år än i en skog som är mellan 101 och 120 år. Resultatet visar att det binds in mer kol i en urskog än i en produktionsskog och att det är viktigt att bevara de urskogar som idag finns för att kunna möta de klimatproblem vi står inför. / For the climate, the forest plays an important role because it binds carbon dioxide from the atmosphere. Through photosynthesis, carbon is bound into the biomass and degradable organic material contributes to carbon storage in the soil. There are many studies on the forest carbon deposits, but they only examine the net binding of carbon, and few studies show how much carbon is stored in total. There are no studies on what carbon storage looks like in Sweden and few studies that show the difference in carbon storage between production forests and old-growth forests. In this literature study, I present how much carbon is bound in Swedish forests and how it differs between production forest and old-growth forest. By applying data from a study that examined how much carbon is bound in Canadian forests on Swedish forests, I concluded that there is a total of between 5 413 and 6 798 million tonnes of carbon stored in Swedish forests, but more carbon could be stored. In Sweden, the average age for when trees are felled is 101 years. I concluded that approximately between 53 and 75 tonnes more carbon per hectare is stored in a forest that is older than 140 years than in a forest that is between 101 and 120 years. The results show that more carbon is bound in an old-growth forest than in a production forest and that it is important to preserve the old-growth forests to reduce the climate problems we face.

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In the Pacific Northwest (PNW), concern about the impacts of climate and land cover change on water resources, flood-generating processes, and ecosystem dynamics emphasize the need for a mechanistic understanding of the interactions between forest canopies and hydrological processes. A detailed measurement and modeling program during the 1999 and 2000 hydrologic years characterized hydrological conditions and processes in a 500-600 year old Douglas fir-western hemlock seasonal temperate rainforest. The measurement program included sub-canopy arrays of radiometers, tipping bucket rain gauges, and soil temperature and moisture probes, to supplement a vertical temperature and humidity profile within the forest canopy. Analysis of the precipitation interception characteristics of the canopy indicated that the mean direct throughfall proportion was 0.36, and the mean saturation storage was 3.3 mm. Evaporation from small storms insufficient to saturate the canopy comprised 19% of the net interception loss, and canopy drying and evaporation during rainfall accounted for 47% and 33% of the net loss, respectively. Results of the measurement program were used to modify the Simultaneous Heat and Water (SHAW) model for forested systems. Changes to the model include improved representation of interception dynamics, stomatal conductance, and within-canopy energy transfer processes. The model effectively simulated canopy air and vapor density profiles, snowcover processes, throughfall, soil water content profiles, shallow soil temperatures, and transpiration fluxes for both a calibration period and for an uncalibrated year. Soil warming at bare locations was delayed until most of the snowcover ablated due to the large heat sink associated with the residual snow patches. During the summer, simulated evapotranspiration decreased from a maximum monthly mean of 2.17 mm day����� in July to 1.34 mm day����� in September, as a result of declining soil moisture and net radiation. Our results indicate that a relatively simple parameterization of the SHAW model for the vegetation canopy can accurately simulate seasonal hydrologic fluxes in this environment. Application and validation of the model in other forest systems will establish similarities and differences in the interactions of vegetation and hydrology, and assess the sensitivity of other systems to natural and anthropogenic perturbations. / Graduation date: 2002

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Old-growth stands are important for management, conservation, wildlife, recreation, and maintaining biological diversity in forested landscapes. However, we are lacking the information needed to adequately identify and characterize old-growth stands. This is especially true for high elevation, interior forests. The characterization of stand structure and regeneration pattern will help in the development of site-specific guidelines for identifying old growth stands and restoring some of the old-growth characteristics in managed stands. This pamphlet presents a synopsis of a study investigating stand structure and regeneration of old-growth stands in the Moist Cold Engelmann Spruce - Subalpine Fir (ESSFmc) Subzone near Smithers, B.C. The three stands selected for the study were located on zonal sites, each in different watersheds, and the stands were established after fire. The criteria used for selection were: i) absence of lodgepole pine, ii) presence of advanced regeneration, and iii) abundant snags and coarse woody debris. These stands were presumed to represent the old-growth stage of stand development or the final (climax) stage of secondary succession.

The species richness, abundance and composition of saproxylic Coleoptera was compared between 'old-growth' and mature-managed hemlock-hardwood forests in southeastern Ontario, Canada. Beetles were sampled weekly from 29 April until 3 October 2003 using large-area flight-intercept traps (FITs) and trunk-window traps (TTs). Analyses were conducted using the Fisher's alpha and Simpson's diversity indices, rarefaction, indicator species analysis and cluster analysis. A total of 11,888 fungivorous Coleoptera was collected from 11 families and 73 species (excluding Nitidulidae). Nitidulidae were analysed separately with traps yielding 2,129 sap beetles comprising 30 species. The species richness and abundance of fungivorous Coleoptera did not differ significantly between the two forest types. Conversely, the species abundance of nitidulid beetles was higher in managed forests and the species richness higher in 'old-growth' forests. Several species were strongly associated with either managed or 'old-growth' forest types. Certain species such as Anisotoma inops (Leiodidae) and Glischrochilus sanguinolentus (Nitidulidae) were much more frequently caught in TTs than in FITs.

I examined saproxylic beetle responses in two silvicultural systems of the eastern mixedwood boreal forest of Quebec. I first investigated habitat-use and aspen-host use of saproxylic and bark and wood-boring beetles in remnant forest patches (cut-bock separators and small patches) left after harvest, theorized to resemble natural post-fire residual trees and snags. A second study focused on effects of partial cutting, a method that may serve to imitate natural succession dynamics. / Remnant forest patches had the highest saproxylic and bark and woodboring beetle species richness and relative abundance. Although non-significant, higher larval densities were also collected from remnant forest patches. In the second study, partial cut patches had an intermediate saproxylic beetle assemblage compared to uncut forest and clearcuts. / This research has brought new information on the effects of alternative harvesting practices on saproxylic beetles, supporting the hypothesis that biodiversity is best preserved based on forest management that is diversified and based on natural disturbance dynamics.