Validation of an application for forecasting blowing snow
被引:59
作者:
Guyomarc'h, G
论文数: 0引用数: 0
h-index: 0
机构:
Meteo France, Ctr Natl Rech Meteorol, Ctr Etud Neige, F-38406 St Martin Dheres, FranceMeteo France, Ctr Natl Rech Meteorol, Ctr Etud Neige, F-38406 St Martin Dheres, France
Guyomarc'h, G
[1
]
Merindol, L
论文数: 0引用数: 0
h-index: 0
机构:
Meteo France, Ctr Natl Rech Meteorol, Ctr Etud Neige, F-38406 St Martin Dheres, FranceMeteo France, Ctr Natl Rech Meteorol, Ctr Etud Neige, F-38406 St Martin Dheres, France
Merindol, L
[1
]
机构:
[1] Meteo France, Ctr Natl Rech Meteorol, Ctr Etud Neige, F-38406 St Martin Dheres, France
来源:
ANNALS OF GLACIOLOGY, VOL 26, 1998
|
1998年
/
26卷
关键词:
D O I:
10.3189/1998AoG26-1-138-143
中图分类号:
P3 [地球物理学];
P59 [地球化学];
学科分类号:
0708 ;
070902 ;
摘要:
Wind effects on snow distribution and increasing avalanche hazard are well known. Forecasting such phenomena is based on empirical rules and experience. For two years, the CEN has tested a new analysis program for forecasting blowing-snow events at an Alpine site. The aim is to improve avalanche-forecasting tools so as to increase the accuracy of avalanche-hazard forecasts. Our understanding of blowing-snow mechanisms began with observations and field measurements at a high altitude site during periods of strong wind. Using an empirical approach, snow-grain morphology, cohesion between snow particles and grain-size have been combined to define a function for the calculation of a "driftability index" By comparing this index with the wind thresholds observed in field, a snowdrifting index has been defined. Snow profiles calculated by SAFRAN (estimation of relevant meteorological parameters for snow models) and Crocus (snowpack-evolution model) were analysed using an application called PROTEON. Forecasts of wind velocity and snow profiles have been used to discriminate between periods with or without snow transport. For the subsequent 24 hours and for each snow layer, the value of this snowdrifting index is calculated and displayed on a graph. Validation consists of a comparison of forecasted blowing -snow periods with the field observations and measurements at a pass situated at 2700 m a.s.l. Meteorological and snow-parameter data are available at this site.