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.
Temperature inversion stops atmospheric convection (which is normally present) from happening in the affected area and can lead to the air becoming stiller and murky from the collection of dust and pollutants that are no longer able to be lifted from the surface. 1  This can become a problem in cities where many pollutants exist.