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TRIMIS

Local enhancement of granular snow from low stratus (industrial snow) (VSS1999/244)

Project

Local enhancement of granular snow from low stratus (industrial snow) (VSS1999/244)


Funding origin:
Switzerland
Switzerland
STRIA Roadmaps:
Transport infrastructure (INF)
Transport infrastructure
Transport mode:
Road
Road
Transport sectors:
Passenger transport
Passenger transport
Freight transport
Freight transport
Project website:
Duration:
Start date: 01/12/2002,
End date: 01/03/2005

Status: Finished
Funding details:

Overview

Background & policy context:

In freezing conditions precipitation from stagnant low stratus in the form of snow grains is enhanced near concentrated sources of moisture. The area affected by snow grains is typically 4 km square and the amount of precipitation is usually small but leads to slippery conditions on frosty road surfaces. Winter road maintenance is needed for the affected roads and sidewalks. Normally the use of salt is sufficient. In extreme cases mechanical snow removal is needed. The very local occurrence of snow covered roads in generally stable weather conditions without precipitations is often surprising for road users as well as for road maintenance services. Thus the phenomenon increases the risk of accidents. Locally enhanced precipitation of snow grains occurs most frequently in the cold morning hours. With low stratus persisting all day it can also occur after dusk.

Objectives:

The relevant meteorological processes shall be identified in case studies. Local sources of water vapor, atmospheric capacity for water vapor and amount of industrial snow shall be compared. Transport processes from the sources of water vapor to the affected road networks shall be investigated quantitatively. Methods for routine forecasts of industrial snowfall shall be defined and proposed.

Methodology:

The information gathering includes research in road inspectorates, power supplies, disposal systems, meteorological services and in the literature. The data is used for adaptation of the existing model convection on wintry night operation with local sources of heat, water vapor, gases and aerosols.

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