BRIDGE FROST OCCURRENCE AND PREDICTION

Frost on bridges can present hazardous conditions to motorists, particularly if it occurs when adjacent roadways are clear of frost. Minimizing materials cost, vehicle corrosion, and negative environmental impacts calls for strategic use of frost-suppression chemicals. Accurate forecasts of bridge frost onset times, frost intensity, and frost disappearance (e.g., melting or sublimation) are needed to help roadway maintenance personnel decide when, where, and how much frost-suppression chemical to use. The authors have developed a finite-difference algorithm (BridgeT) that simulates vertical heat transfer in a bridge based on evolving meteorological conditions at its top and bottom as supplied by a weather forecast model. This algorithm simulates bridge deck surface temperature at 1-min intervals and calculates volume per unit area (i.e., depth) of frost deposited, melted, or sublimed. From this are produced forecasts of frost onset time, frost "depth," and duration of frost on the bridge. Evaluation of forecast methods for predicting frost on bridges and roadways is difficult because of a lack of observations of frost occurrences. Early morning observations of untreated bridges near Ames, Iowa, were made during two winter seasons to establish a database of bridge frost occurrences and non-occurrences. When frost was detected, observations were continued until the frost disappeared and thereby provided additional information on duration and timing of onset and demise of frost. Bridge frost predictions as well as predictions of air temperature, dew-point temperature, bridge-top surface temperature, and wind speed, are compared with observed and measured values to assess skill in forecasting bridge frost and associated conditions. Lack of agreement between forecasts of frost characteristics and visual observations on a particular (presumed chemical-free) bridge may arise from (1) inaccuracies in forecasts of meteorological variables by the weather forecast model at its model resolution, (2) spatial variability in meteorological conditions below resolution of the forecast model, (3) inaccuracies in simulation of heat transfer by BridgeT, or (4) an inability to detect frost visually.

Language

  • English

Media Info

  • Features: Figures; References; Tables;
  • Pagination: p. 391-398
  • Serial:

Subject/Index Terms

Filing Info

  • Accession Number: 00974859
  • Record Type: Publication
  • Report/Paper Numbers: E-C063,, SNOW04-005, SNOW04-039
  • Files: TRIS, TRB
  • Created Date: Jun 10 2004 12:00AM