Moisture Differential
Atmospheric moisture metrics define the temperature drop required for water vapor to condense on chilled surfaces. Calculating dew point depression indicates the difference between ambient air temperature and the temperature at which moisture forms on paperboard packaging surfaces during cold chain transport. High humidity environments cause rapid moisture absorption into exposed paperboard fibers when surface temperatures fall below the dew point.
Scope ends when ambient air temperatures equal the dew point temperature, resulting in immediate surface condensation.
Thermal Condensation
Cold storage packaging transitions from refrigerated warehouses to ambient loading docks generate steep thermal gradients across paperboard corrugated cases. When ambient air temperature exceeds packaging surface temperature, small dew point depression values cause water condensation on structural containerboard. Moisture absorption reduces corrugated compression strength and causes box stacking failure in damp distribution environments.
Barrier coatings and hydrophobic sizing agents delay water liquid penetration during brief dew point condensation events. Refrigerated transport protocols maintain low relative humidity to widen dew point depression values and prevent moisture accumulation.
Humidity Control
Warehouse climate management relies on active dehumidification to protect paperboard structural integrity during seasonal weather changes. Saturated paperboard corrugated containers lose up to sixty percent of their stacking strength under severe condensation conditions.