High-resolution radar measurements of snow avalanches

Two snow avalanches that occurred in the winter 2010–2011 at Vallée de la Sionne, Switzerland, are studied using a new phased array FMCW radar system with unprecedented spatial resolution. The 5.3 GHz radar penetrates through the powder cloud and reflects off the underlying denser core. Data are rec...

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Bibliographic Details
Published inGeophysical research letters Vol. 40; no. 4; pp. 727 - 731
Main Authors Vriend, N. M., McElwaine, J. N., Sovilla, B., Keylock, C. J., Ash, M., Brennan, P. V.
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 28.02.2013
American Geophysical Union
John Wiley & Sons, Inc
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Summary:Two snow avalanches that occurred in the winter 2010–2011 at Vallée de la Sionne, Switzerland, are studied using a new phased array FMCW radar system with unprecedented spatial resolution. The 5.3 GHz radar penetrates through the powder cloud and reflects off the underlying denser core. Data are recorded at 50 Hz and have a range resolution better than 1 m over the entire avalanche track. We are able to demonstrate good agreement between the radar results and existing measurement systems that record at particular points on the avalanche track. The radar data reveal a wealth of structure in the avalanche and allow the tracking of individual fronts and surges down the slope for the first time. Key Points Validation between our radar results and existing point measurement systems High‐resolution radar allows tracking of fronts and surges from start to finish Velocity linked with topography may be used to measure rheology of snow
Bibliography:istex:F64006A48025540F1DD1BEB05FEC0F5DFFBBE6F4
ark:/67375/WNG-JFBLCNF5-S
ArticleID:GRL50134
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0094-8276
1944-8007
DOI:10.1002/grl.50134