Fog is a natural phenomenon and is formed when water vapours in the air
near the surface begin to condense into liquid water. Fog occurs over
Punjab (Pakistan), during winter months of November, December and
January. The aim of this study was to investigate the dense fog events
and also to find the reasons of this prolonged fog. This
prolonged/unusual fog affects the air and road traffic badly. Many
accidents take place because of poor visibility and many people lose
their lives. Using 30-year (1976-2005) real meteorological data of
10-weather stations, four dense fog years were investigated. Daily,
ten-days and monthly temperature and moisture data of these four years
showed significant changes during the fog events. It is observed that
day time temperature decreases and night time temperature increases
during fog events but the mean temperature remains below 15.5 degrees
Celsius, mean relative humidity examined more than 80% for the north
Punjab and more than 70% for the south Punjab and throughout the fog
period, daily saturatain vapour pressure deficit found below 1hpa and
with these conditions, dense fog events could be predicted precisely for
next 24-48 hours