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Avalanche Forecasting with GIS
R. Bolognesi1, M. Denuelle2, L. Dexter2

1 Swiss Federal Institute for Snow and Avalanche Research, Davos, Switzerland

2 Department of Geography, Northern Arizona University, Flagstaff, Arizona
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Key words : Local Avalanche Forecasting, Geographic Infor-

mation System

INTRODUCTION

Avalanches depend on snowpack stability as well as ter-
rain conditions. Thus, these two kinds of information
are required to perform punctual predictions. However,
if the site is very large, including many gullies and
slopes, it may be difficult to define the starting zone.
Therefore, a detailed topographic analysis of the site is
useful. This analysis can be done by a Geographic Infor-
mation System (GIS).
This paper presents an idea : using a GIS to determine
and describe the starting zone(s) of a large avalanche site
in order to provide computed inputs to a local avalanche
forecasting model.
This model is the NxLog system, which was designed
at the Swiss Federal Institute for Snow and AvalancheRe-
search (Bolognesi, 1994). NxLog is an expert system run-
ning symbolic calculations as well as nearest neighbor
procedure. The aim of this system is to provide every day
the probability of avalanche occurrence for each starting
zone of a defined area (a ski resort for example). Is it pos-
sible and profitable to make the GIS and NxLog work to-
gether ? This is the question we want to answer.
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GISIMPLEMENTATION

The source of information used for the topographic analy-
sis
ofthe avalanche sites istheDigital ElevationModel
(DEM).Such DEMs are useful forany terrain analysis or
representation. The data included in the DEMs iseleva-
tion, and geographical coordinates. Using a GIS software,
this data can be derived into slope angle and slope aspect.
Withslopeaspect,slopeangle,andelevation,atopo-
graphic representation and analysis of any avalanche site
can be done in greater precision.The minimum size unit
of terrain of such data is 30x30 meters cell which isthe
standard format of a DEM in the USA.The GIS software
used to derive the data in slope aspect,slope angel,and
elevation isthe GRID module of ArcInfoT M .The GIS im-
plementation can be divided into two steps.
The first step is to create the three layers (slope aspect,
slope angle, and elevation) from the DEMs. After creating
those layers with GRID,we divide each layerinto inter-
vals
ofcriticalimportance foravalancherelease.These
intervalswaschosenaccordingtoexperts'opinion
(K.Birkeland, R.Bolognesi, L.Dexter, A.Gleason, D.Hogan).
The slope aspect layer is broken down into 8 intervals
of 45degrees each representing North,North East,East,
SouthEast,South,SouthWest,West,NorthWest.The
slopeanglelayerisdividedinto9intervals.Theeleva-
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