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I've been thinking about relative humidity and how it relates to temperature. I've been moving the hygrometer between warmer and cooler areas in the enclosure. The warmer areas have lower RH and the cooler areas have higher RH, and explanations for these observations are already well known.
But then, when we give out recommendations for RH in the enclosure of a certain animal, say a tegu, are we talking in the cool end or the warm end, because it makes a difference. So maybe RH is not the best measurement of humidity as it relates to living organisms.
Plant people already know this, but animal keepers are a bit behind, I suppose. People who run greenhouses often try to calculate a different measure of humidity, called the vapor pressure deficit (VPD). VPD is the difference between the vapor pressure at saturation (100% RH) and the actual vapor pressure at the same air temperature. Plant people use this measure because it is a better assessment of the drying capacity of an environment than relative humidity is.
If you have a warm location that is at 75% RH, the VPD will be higher than another location that is cooler but has the same 75% RH. The higher VPD number in the warmer location will reflect that the warmer location will have a greater capacity to suck moisture from the organism, even though the RH is the same.
Here's an example of a warm location and a cool location, where RH is constant and VPD is variable:
90 F, 75% RH - VPD = 12
60 F, 75% RH - VPD = 6
So even though the RH is measured at exactly the same value, the VPD is much greater at 90F than at 60F, meaning that warmer areas will suck more moisture out of your animal than cooler areas when RH is the same at both locations.
So VPD is a much better way to measure humidity as it relates to an animal. To have a constant VPD throughout an enclosure, you would have higher RH in warm areas and lower RH in cool areas.
Same example as above, except now VPD is constant and RH is variable:
90 F, VPD = 12 - 75% RH
60 F, VPD = 12 - <35% RH
This sounds great, but VPD is more difficult to calculate and there are no gauges. To calculate it you need to know the temperature, the saturation vapor pressure for that temperature, and the RH. If you know those things, the calculation is simple: saturation vapor pressure - (saturation vapor pressure x RH/100). It's the saturation vapor pressure that is more difficult to calculate.
This is mostly food for thought. I found it interesting and it cleared up some humidity-related questions that were roaming around in my head.
But then, when we give out recommendations for RH in the enclosure of a certain animal, say a tegu, are we talking in the cool end or the warm end, because it makes a difference. So maybe RH is not the best measurement of humidity as it relates to living organisms.
Plant people already know this, but animal keepers are a bit behind, I suppose. People who run greenhouses often try to calculate a different measure of humidity, called the vapor pressure deficit (VPD). VPD is the difference between the vapor pressure at saturation (100% RH) and the actual vapor pressure at the same air temperature. Plant people use this measure because it is a better assessment of the drying capacity of an environment than relative humidity is.
If you have a warm location that is at 75% RH, the VPD will be higher than another location that is cooler but has the same 75% RH. The higher VPD number in the warmer location will reflect that the warmer location will have a greater capacity to suck moisture from the organism, even though the RH is the same.
Here's an example of a warm location and a cool location, where RH is constant and VPD is variable:
90 F, 75% RH - VPD = 12
60 F, 75% RH - VPD = 6
So even though the RH is measured at exactly the same value, the VPD is much greater at 90F than at 60F, meaning that warmer areas will suck more moisture out of your animal than cooler areas when RH is the same at both locations.
So VPD is a much better way to measure humidity as it relates to an animal. To have a constant VPD throughout an enclosure, you would have higher RH in warm areas and lower RH in cool areas.
Same example as above, except now VPD is constant and RH is variable:
90 F, VPD = 12 - 75% RH
60 F, VPD = 12 - <35% RH
This sounds great, but VPD is more difficult to calculate and there are no gauges. To calculate it you need to know the temperature, the saturation vapor pressure for that temperature, and the RH. If you know those things, the calculation is simple: saturation vapor pressure - (saturation vapor pressure x RH/100). It's the saturation vapor pressure that is more difficult to calculate.
This is mostly food for thought. I found it interesting and it cleared up some humidity-related questions that were roaming around in my head.
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