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.
Inversions frequently develop during evenings and nights and can occur at the surface or aloft in the atmosphere. During the daylight hours, surface inversions normally weaken or disappear when the sun warms the ground. In addition, wind speed and rain contribute to how quickly inversion will break up.