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	<journal>
		<journal_title>Natural Hazards and Earth System Science</journal_title>
		<journal_url>www.nat-hazards-earth-syst-sci.net</journal_url>
		<issn>1561-8633</issn>
		<eissn>1684-9981</eissn>
		<volume_number>8</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/nhess-8-685-2008</doi>
	<article_url>http://www.nat-hazards-earth-syst-sci.net/8/685/2008/</article_url>
	<abstract_html>http://www.nat-hazards-earth-syst-sci.net/8/685/2008/nhess-8-685-2008.html</abstract_html>
	<fulltext_pdf>http://www.nat-hazards-earth-syst-sci.net/8/685/2008/nhess-8-685-2008.pdf</fulltext_pdf>
	<start_page>685</start_page>
	<end_page>705</end_page>
	<publication_date>2008-07-16</publication_date>
	<article_title content_type="html">Regional evaluation of three day snow depth for avalanche hazard mapping in Switzerland</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>D. Bocchiola</name>
			<email>daniele.bocchiola@polimi.it</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>E. Bianchi Janetti</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>E. Gorni</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>C. Marty</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>B. Sovilla</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Dept. of Hydraulic, Environmental, Surveying and Road Structures Engineering, Politecnico di Milano, L. Da Vinci Square 32, 20133 Milano, Italy</affiliation>
		<affiliation numeration="2" content_type="html">WSL, Swiss Federal Institute for Snow and Avalanche Research SLF, Flüelastr. 11, 7260 Davos Dorf, Switzerland</affiliation>
	</affiliations>
	<abstract content_type="html">The distribution of the maximum annual three day snow fall depth &lt;i&gt;H&lt;sub&gt;72&lt;/sub&gt;&lt;/i&gt;,
used for avalanche hazard mapping according to the Swiss procedure (&lt;i&gt;Sp&lt;/i&gt;), is
investigated for a network of 124 stations in the Alpine part of
Switzerland, using a data set dating back to 1931. Stationarity in time is
investigated, showing in practice no significant trend for the considered
period. Building on previous studies about climatology of Switzerland and
using an iterative approach based on statistical tests for regional
homogeneity and scaling of &lt;i&gt;H&lt;sub&gt;72&lt;/sub&gt;&lt;/i&gt; with altitude, seven homogenous
regions are identified. A regional approach based on the index value is then
developed to estimate the &lt;i&gt;T&lt;/i&gt;-years return period quantiles of &lt;i&gt;H&lt;sub&gt;72&lt;/sub&gt;&lt;/i&gt; at each
single site &lt;i&gt;i&lt;/i&gt;, &lt;i&gt;H&lt;sub&gt;72i&lt;/sub&gt;(T)&lt;/i&gt;. The index value is the single site sample average
&amp;mu;&lt;sub&gt;&lt;i&gt;H&lt;sub&gt;72i&lt;/sub&gt;&lt;/i&gt;&lt;/sub&gt;. The dimensionless values of &lt;i&gt;H&lt;sup&gt;*&lt;/sup&gt;&lt;sub&gt;72i&lt;/sub&gt;=H&lt;sub&gt;72i&lt;/sub&gt; / &amp;mu;&lt;sub&gt;H&lt;sub&gt;72i&lt;/sub&gt;&lt;/sub&gt;&lt;/i&gt; are
grouped in one sample for each region and their frequency of occurrence is
accommodated by a General Extreme Value, GEV, probability distribution,
including Gumbel. The proposed distributions, valid in each site of the
homogeneous regions, can be used to assess the &lt;i&gt;T&lt;/i&gt;-years return period
quantiles of &lt;i&gt;H&lt;sup&gt;*&lt;/sup&gt;&lt;sub&gt;72i&lt;/sub&gt;&lt;/i&gt;. It is shown that the value of
&lt;i&gt;H&lt;sub&gt;72i&lt;/sub&gt;(T)&lt;/i&gt; estimated with the regional approach is more accurate than that
calculated by single site distribution fitting, particularly for high return
periods. A sampling strategy based on accuracy is also suggested to estimate
the single site index value, i.e. the sample average &amp;mu;&lt;sub&gt;&lt;i&gt;H&lt;sub&gt;72i&lt;/sub&gt;&lt;/i&gt;&lt;/sub&gt;, critical for the
evaluation of the distribution of &lt;i&gt;H&lt;sub&gt;72i&lt;/sub&gt;&lt;/i&gt;. The proposed regional approach
is valuable because it gives more accurate snow depth input to dynamics
models than the present procedure based on single site analysis, so
decreasing uncertainty in hazard mapping procedure.</abstract>
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