Customer has credit limit on 01-0102010 as 1000 and we changed on 20-06-2010 as 2000 and on 30-10-2010 as 3000. The table KNKK is displaying only present credit limit as 3000.
Temperature inversion may occur during the passage of a cold front or result from the invasion of sea air by a cooler onshore breeze. Overnight radiative cooling of surface air often results in a nocturnal temperature inversion that is dissipated after sunrise by the warming of air near the ground.
Because air near the base of an inversion tends to be cool, fog is frequently present there. Inversions also affect diurnal variations in air temperature. The principal heating of air during the day is produced by its contact with a land surface that has been heated by the Sunâs radiation.