The dew point is the minimum temperature to which a gas (usually air) can be cooled before water in the gas (usually air) condenses. As the temperature is cooled, the water carrying capacity of the gas decreases (relative humidity - the amount of water in a gas divided by the maximum amount it can carry - increases). Eventually the amount of water vapor in the gas reaches the maximum amount the gas can hold (relative humidity = 100%). Any further reduction in temperature causes the water vapor to condense. The dew point is mostly a function of the water vapor concentration and the temperature. The history of a gas doesn't seem to me as though it would matter to the dewpoint, unless the history affects the water content. As an example, suppose that nitrogen gas has x% of water content, which would impart a certain dew point y. If liquification of the nitrogen followed by de-liquification causes the water content to be different, then the dew point of the nitrogen will also be different for the previously liquidifed nitrogen. I guess one could envision a scenario where liquification of nitrogen causes its water content to rise lower slightly. In which case the de-liquified nitrogen would then have a lower dew point because it has a higher lower water content. Whether this is generally true of previously liquified nitrogen, I have no idea.