Research Services
RadTherm/RT Tour

WIND MODELING
Wind velocity and direction strongly influences the convective heat transfer. The RadTherm/RT wind algorithm calculates the convection coefficient based on wind direction/ speed and accounts for the heat transfer due to rain.  Convection is computed by calculating the direction of the wind relative to each element and the temperature difference between the air and the element.

Specific to modeling wind for the Montana State University project is the use of localized wind conditions. Data from widely spaced weather stations provides rough estimates for the surface wind at different road sections. 

Special data is NOT required and most models use weather files. Weather files are ASCII text files that contain the following information:

Variable Description
TIME TIME that the following weather conditions were observed. This is zone time in military style, where 2:30 P.M. is expressed as 1430 hours. Note that midnight should be expressed as 0000 hours and not 2400 hours.
AIRT AIR Temperature in C.
SOLAR SOLAR irradiance in W/m2 (total solar on horizontal).
WIND WIND speed in m/s.
HUMID HUMIDity in percent (0 - 100).
CLOUD CLOUD cover in tenths (0 = Clear, 10 = Total Overcast).
LWIR Long Wave InfraRed radiation in W/m2.
WINDIR WIND DIRection in from North to East in degrees (0-359).
RAINRATE RATE of RAINfall in mm/hr. (Optional)

 

 

 

 

 

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