Abstract

The service life of exposed wooden structures depends on many endogenous and exogenous factors with moisture being key for fungal degradation. Climate parameters are therefore important input variables for modelling fungal decay in wood. In recent years, different approaches aimed at modelling climate-induced dosage on the material climate (i.e., exposure models) and the effect of the latter on fungal decay (i.e., decay models). Based on maps of Europe, North America or Australia, the decay hazard can be assigned to zones and used for estimating the relative decay potential of an arbitrary location. However, especially in topographically divergent regions, the climate-induced decay hazard can vary strongly within a small area. Within this study, decay hazards were quantified and mapped for a mountainous region where topography-induced differences in local climate and corresponding exposure dosage can be expected. The area under investigation was Switzerland. In addition to the Scheffer Climate Index (SCI), two exposure models were combined with two decay models and used to quantify the relative moisture- and temperature-induced exposure dose at 75 different weather stations in Switzerland and adjacent regions. The exposure was expressed as relative dosage with Uppsala (Sweden) as a reference location. Relative dose values were calculated for locations between weather stations using an ‘inverse distance weighted (IDW)’ interpolation and displayed in maps for the entire country. A more detailed analysis was undertaken for the Lötschental area, which is the largest valley on the northern side of the Rhône valley in the canton of Valais. The relative dose differed strongly within small areas and altitude was well correlated with the average annual temperature and the resulting relative dose. It became evident that small-scale mapping with high resolution is needed to fully reflect the impact of topography and other local conditions on the moisture- and temperature-induced decay risk in wooden components.

Highlights

  • The service life of exposed wooden structures depends on many endogenous and exogenous factors, with moisture being key for fungal degradation

  • It became evident that small-scale mapping with high resolution is needed to fully reflect the impact of topography and other local conditions on the moisture- and temperature-induced decay risk in wooden components

  • In contrast to annual precipitation and annual average temperature, the annual average relative humidity (RH) showed a clear gradient from North to South with an overall range between 62%

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Summary

Introduction

The service life of exposed wooden structures depends on many endogenous and exogenous factors, with moisture being key for fungal degradation. Climate parameters are important input variables for modelling fungal decay in wood and decay hazard mapping can help to estimate exposure-related dosage in a quantitative manner [1]. Pioneering work on decay hazard mapping was carried out by Theodore Scheffer in the early 1970s. Scheffer [2] suggested a climate index to correlate climatic data with the site-specific potential for biological decay. The hazard potential of different climates in the USA was estimated by empirically determined decay intensity from field tests. Forests 2020, 11, 510 at four different locations. In this early attempt the focus was on the parameters ‘temperature’ and ‘distribution of rainfall’, which Scheffer described as follows: Sche f f er Climate Index (SCI ) =

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