Hostname: page-component-cd9895bd7-lnqnp Total loading time: 0 Render date: 2024-12-29T11:55:59.629Z Has data issue: false hasContentIssue false

Temperature differences in the air layer close to a road surface

Published online by Cambridge University Press:  23 January 2002

Jörgen Bogren
Affiliation:
Laboratory of Climatology, Physical Geography, Department of Earth Sciences, University of Göteborg, Box 460, SE 405 30 Göteborg, Sweden
Torbjörn Gustavsson
Affiliation:
Laboratory of Climatology, Physical Geography, Department of Earth Sciences, University of Göteborg, Box 460, SE 405 30 Göteborg, Sweden
Maria Karlsson
Affiliation:
Laboratory of Climatology, Physical Geography, Department of Earth Sciences, University of Göteborg, Box 460, SE 405 30 Göteborg, Sweden
Get access

Abstract

In this study, profiles of temperature and humidity (<250 cm above the road and 5 m into the surroundings) have been used to examine the development of temperature differences in the air layer close to the road. Temperature, humidity and wind profiles were measured, together with net radiation and observations of road surface state, at a test site at Road 45, Surte, Sweden. Measured temperature differences were compared with present weather, preceding weather, surface status, wind direction and other parameters thought to be important for the development of temperature differences. The results showed that large temperature differences (1-3 °C between 250 cm and 10 cm above the road) occurred when there was a high risk of slipperiness caused by hoarfrost, snow or ice on the road. The temperature differences between different levels were associated with the exchange of humidity and temperature between the air layer and the road surface. The 10 cm level reflected the surface processes well. Higher levels were influenced by the surroundings because of turbulence and advection. This study emphasises the need for measurements to be taken at a height and place that reflects the processes at the road surface.

Type
Research Article
Copyright
© 2001 Royal Meteorological Society

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)