Mapping avalanche risk using GIS and dendrochronological techniques

Giovanni Comunello 1, Marco Ciolli 1, Paolo Cherubini 2


cherubini@wsl.ch
1: Dipartimento di Ingegneria Civile e Ambientale Università degli studi di Trento, Italy
2: Swiss Federal Research Institute WSL, Birmensdorf, Switzerland

 


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In this work we present a method for the evaluation of avalanche risk (Comunello, 2000). The study site (Tòf Larch) is an avalanche track located in Val di Pejo, in Trentino (Italy).

GIS and dendrochronological techniques provide useful information. We compared field observations with the geographical model. At the study site it was difficult to obtain complete information regarding the avalanche track, because of the lack of significant historical records.In order to obtain more data, we analyzed the spatial distribution of tree vegetation and made a dendrochronological preliminary study of the larch trees (Larix decidua Mill.) growing within the avalanche path.

With the aid of a numerical model elaborated by means of the GIS G.R.A.S.S. (Geographical Resources Analysis Support System) forest areas exposed to the avalanche hazard were mapped. We individuated two different kinds of risk:

  • morphological risk, based on topographical features that lead to the detachment of snowpack, i.e. slope, aspect and presence of morphological discontinuities;
  • potential risk, as a function of two parameters of the stand structure, i.e. number of stems per ha and canopy density (Salm, 1978; Meyer-Grass, 1985).

Using these models, the protective function of the forest may be assessed and evaluated, analysing the so called ‘global risk areas’, where the risk parameters are simultaneously presented.

We compared the results of the GIS study with field observations. The presence of clear-cut trimlines (Burrows and Burrows, 1986) suggested the occurrence of past avalanche events. A dendrochronological study was carried out in order to reconstruct and map the spatial extent of past avalanches. Three sampling zones were selected along the main trimline and within the track. The occurrence of dendroecological indicators and the observation of various kind of damage on trees indicated the more active avalanche path, in agreement with the topographical output produced by the GIS.

This multidisciplinary approach revealed to be useful. The comparative analysis was effective to deduce information about the past occurrence of avalanches, especially where historical records and direct observations of phenomena are uncomplete.

References
Burrows, C.J., Burrows, V.L., 1976, Procedures for the study of snow avalanche chronology using growth layers of wood plants. Institute of Arctic and Alpine Research, University of Colorado, INSTAAR Occasional Paper No. 23.
Meyer-Grass, M., 1985, Valanghe che si staccano in bosco: soprassuoli più esposti, provvedimenti. Istituto Federale per lo studio della Neve e delle Valanghe, Davos, CH.
Salm, B., 1978, Snow forces on forest plants, IUFRO, Proceedings International Seminar Mountain Forest and Avalanches, Davos: pp. 157-181.
Comunello, G., 2000, Impiego di tecniche GIS e di dendrocronologia applicata per lo studio delle zone potenzialmente esposte al rischio di valanghe. Tesi di laurea, Università degli studi di Trento, Corso di Laurea in Ingegneria per l’Ambiente e il Territorio.

Keywords: avalanche risk, GIS, Val di Pejo, Trentino, Italy

Poster abstract 201 (http://www.wsl.ch/forest/dendro2001/abstracts/abs201.ehtml)
Conference "Tree Rings and People", September 22-26 2001, Davos, Switzerland (http://www.wsl.ch/forest/dendro2001/)


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