WIND CHILL INDEX
CITY Wednesday 12.12.2018. Thursday 13.12.2018. Friday 14.12.2018. Saturday 15.12.2018.
Bihać        
B.Luka        
Bugojno        
Livno        
Mostar        
Sarajevo        
Trebinje        
Tuzla        
Zenica        
MOUNTAINS
Babin Do        
Bjelašnica        
Jahorina        
Kozara        
Vlasić        

   no risk     moderate risk     great risk     very high risk 

Wind chill

A surface loses heat through conduction, convection, and radiation. The rate of convection depends on both the difference in temperature between the surface and the fluid surrounding it and the velocity of that fluid with respect to the surface. As convection from a warm surface heats the air around it, an insulating boundary layer of warm air forms against the surface. Moving air disrupts this boundary layer, or epiclimate, allowing for cooler air to replace the warm air against the surface. The faster the wind speed, the more readily the surface cools.

The attempt to maintain a given surface temperature in an environment of faster heat loss results in both the perception of lower temperatures and an actual greater heat loss. In other words, the air 'feels' colder than it is because of the chilling effect of the wind on the skin.

Source: Wikipedia - https://en.wikipedia.org/wiki/Wind_chill

 biometeorologY
  • Biometeorological Forecast
  • Wind Chill Index
  • CITY Wednesday 12.12.2018.
    Bihać  
    B.Luka  
    Bugojno  
    Livno  
    Mostar  
    Sarajevo  
    Trebinje  
    Tuzla  
    Zenica  
    MOUNTAINS
    Babin Do  
    Bjelašnica  
    Jahorina  
    Kozara  
    Vlasić  
  • Humidex Index
  • UV index