A critical point that is often ignored!
I keep harping on about the lack of dynamic modelling in "standard" interstitial condensation risk models, but I do so because it's important. Once water vapour has condensed in a region inside the structure that can be prone to damage induced by organisms that thrive on damp, then it takes a LOT of heat energy to cause that water to undergo a phase change back to vapour and be able to escape from the structure.
In effect, you can have a sort of "one-way valve", where vapour enters under a certain combination of short duration conditions and condenses inside the structure. Insufficient heat energy ever reaches the area where the water vapour has condensed, so it stay there, and build up every time a dynamic condition exists that allows more vapour to condense. Some of these dynamic conditions can be of short duration - for example a cold, still, wet, night, followed by a hot and sunny windless morning, where the air immediately around the external structure and in any cavity could easily reach high water vapour concentration levels, and some parts of the internal structure may well be just below the local dew point for a time. The fact they get above the local dew point later in the day may not be enough, as there may still not be enough heat energy available to convert the condensate back to vapour.