The Weather Vane is prepared by Daniel Bezte, a teacher by profession with a BA (Hon.) in geography, specializing in climatology, from the University of Winnipeg. Daniel has taught university-level classes in climate and weather and currently operates a computerized weather station at his home near Birds Hill Park, on 10 acres he plans to develop into a vegetable and fruit hobby farm.
Contact him with your questions and comments at [email protected]
As we move into summer and with all this moisture around, I think it’s time to revisit one of my weather pet peeves: humidity. We are going to look at what exactly humidity is, how we measure it, and how it is reported and interpreted.
Humidity, by its simplest definition, is the amount of water vapour in the air. The warmer the air, the greater the distance between air molecules and therefore, the greater the holding capacity for water vapour. Conversely, when air is cooled, the distance between air molecules decreases, leaving less room for the air to hold water vapour. Because of this relationship, warm air has the capacity to hold much more water than cold air.
If we look only at the water-holding capacity of air at different temperatures and measure the amount of water by its mass (weight), we would find that for every 10 C increase in temperature, the holding capacity of the air for water nearly doubles. When humidity is measured this way it’s referred to as specific humidity. While this is a useful way to measure humidity, it’s not the way we usually hear it reported.
The most common way in which humidity is reported is relative humidity. Unfortunately, it’s probably one of the most misunderstood terms used in trying to describe the weather. Relative humidity is a ratio of the amount of water vapour in the air, compared to the maximum it could hold under those same conditions, and is expressed as a percentage. Taking one of the examples from above, if we had an air temperature of 10 C and had eight grams of water vapour per kg of air, our relative humidity would be 100 per cent, calculated as follows:
Actual amount of water vapour in the air (8 grams) the holding capacity of the air at the current temperature (air at 10 C has a holding capacity of about eight grams) X 100 = 100 per cent.
Now, if this same air was warmed up to a temperature of 30 C and the amount of water vapour in the air didn’t change, our relative humidity would be around 29 per cent [(8 grams 28 grams)] X 100).
This is where the misunderstanding begins to develop and it’s where my pet peeve lies. When the air temperature was 10 C and the relative humidity was 100 per cent, people would say it’s humid out, but once the temperature has warmed up to 30 C and the relative humidity dropped to 29 per cent, people would say that it is very dry out, but in reality, the amount of water vapour in the air has not changed; only the temperature has. This is particularly noticeable on humid summer days. In the morning we’ve had temperatures in the 16-18 C range with relative humidities in the 100 per cent range: it’s humid out. By afternoon, with temperatures in the mid-to upper 20s, the relative humidity has dropped down to around 50-60 per cent and people now say it’s dry out – but it’s not, it’s humid. The amount of water vapour in the air hasn’t changed.
A better way to measure humidity is by using the dew point temperature, which we simply refer to as the dew point.
This measurement is a fairly simple way of telling us exactly how much moisture is in the air no matter how the temperature changes during the day. The dew point is the temperature that we would have to cool the air down to in order for condensation (or dew) to begin forming – in other words, the temperature that the air would have to be to give us 100 per cent relative humidity.
In our previous example, the dew point first thing in the morning would have been around 18 C, since the air was at its holding capacity. By the afternoon, even though the air had warmed up, the dew point would still have been around 18 C since no additional water vapour was added or removed from the air. How does this relate to overall humidity?
If we have dew points that are less than 10 C, the atmosphere is considered to be fairly dry and dew points in the 10-15 C range are fairly comfortable. Once we get into the 15-20 C range, the atmosphere is becoming fairly humid. Dew points over 20 C are getting very humid, and it will start to feel very uncomfortable outside. If the dew point goes over 25 C, the atmosphere is heavy with moisture and conditions will be very uncomfortable and can even be dangerous. Going back to relative humidity once more, to pound home the difference between this and the dew point: if the dew point is 25 C, we know it is very humid out no matter what the temperature is, but if the temperature was, let’s say, 35 C, the relative humidity would only be about 55 per cent, and I could guarantee at least one person would be saying it’s not that humid out!
In Manitoba we rarely get dew points above 25 C, our record dew point being in the 28 C range around the Carman/Morden area (Carman did hit a record dew point of 30 C back in 2007), but we often have extended periods with dew points hovering in the low 20s. So remember, if it’s a hot summer day with dew points in the low 20s, even if the relative humidity is only 50 per cent, it is still humid out!