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.
Dew Point Temperature and Frost Point Temperature. The temperature at which the change of state occurs as the air is cooled is called the dew point temperature when the change of state occurs at a temperature above freezing or the frost point temperature when the change of state occurs at a temperature below freezing.hether dew or frost will form is determined by two factors: 1  If the amount of moisture in the air causes the condensation temperature to be above or below freezing and. 2  If the temperature will cool to the condensation temperature.