I'll have a crack at it - at least my understanding of it - apologies if either too simple or too technical!
Water, like pretty much everything else (including metals) has a 'vapour pressure' (in the case of water its related to the absolute humidity) where molecules are knocked off the surface (evaporating). If hot, the molecules are banging about and more get knocked off and the humidity rises - taking away some of the heat and cooling it. This is true even when its ice.
At some point the rate at which they boil off is equal to the rate at which they recondense and the air is saturated at that temperature - an equilibrium. If the temperature rises to the point where the vapour pressure is the same as the air pressure, it boils. This is why at altitude, with a low pressure, water boils at a lower temperature.
Conversely, because low temperature air cannot support as much vapour as warm air, if there is a cold surface more molecules condense than boil off and so you get those drips of water on the perfectly chilled glass of amber nectar you're about to savour... sorry, off the subject a bit
That's the Dew Point - any surface colder starts to get condensation - or if cold enough, frost. It also starts to warm - its gaining additional energy - and the amount of water in the air goes down - the overall humidity drops.
The Relative Humidity is the current vapour pressure compared to the maximum at the current temperature as a percentage.
The bottom line is that in a sealed box, surfaces below the dew point mean lower relative humidity. If you use 'forced' humidifying techniques the excess moisture will tend to condense on to them, which also warms them - Paul, that is probably why you are seeing it cutting in more often, and why I was asking if Oddley had tried the fan approach - hopefully raising the element above the Dew Point for the overall temperature.
I have done some Dew Point calcs (in Excel) for the area of interest they are:
Relative Humidity
Temp 60% 65% 70% 75% 80%
8 0.7 1.8 2.9 3.8 4.8
9 1.7 2.8 3.8 4.8 5.7
10 2.6 3.7 4.8 5.8 6.7
11 3.5 4.7 5.7 6.7 7.7
12 4.5 5.6 6.7 7.7 8.7
13 5.4 6.6 7.7 8.7 9.6
14 6.4 7.5 8.6 9.6 10.6
Afraid it doesn't seem to format properly - email me if anyone wants a copy of the spreadsheet.
Now, if someone could just explain why the water with salt in would be colder than the water on its own...
Before the Roman came to Rye or out to Severn strode, the rolling English Drunkard made the rolling English road... G.K.Chesterton