Mary, Mary, How does your dewpoint vary?

Today we are modifying the old nursery rhyme which inquires about Mary's garden  to consider typical fluctuations in dewpoint temperature.  Since the dewpoint depends on the total atmospheric pressure, and that changes from day-to-day, the dewpoint will change (for a given amount of moisture in the air) as the barometric pressure changes. We'll also look at how dewpoint might change with altitude.

Heat from Breath, part 2

In the last post we considered heat lost through breathing and determined that breathing air at 35 °F results in a heat loss of about 2 Watts for every liter/min of air flow.  Of course, this depends strongly on the temperature and relative humidity of the ambient air.  In this post, we’ll consider both the effect of the condition of the ambient air, and also how much of the heat is latent (due to moisture) and how much is sensible (due to temperature).

Heat from Breath

In an earlier post, we looked at how much water is lost through breathing.  Today, we’ll consider the amount of body heat lost through breathing.  Of course, depending on surroundings, air movement, and  how one is dressed, a lot of (or a little) heat might be lost through the skin, but we’re just considering the part that goes out with your breath.

Moisture and Altitude

Psychrometric charts are very useful for determining properties of moist air, but it is important to remember that each chart is prepared for a given atmospheric pressure.  Of course, it is easy to find charts created for specific elevations, but it is sometimes hard to visualize the variations in properties with elevation.  In this post, we’ll look at the effect of elevation on the moisture content of air.

Water from Air

We’ve talked in other posts about how water will condense out of air when it is cooled past the dewpoint temperature.  So I got to wondering how much it would cost to produce water that way.  In this post we’ll look at a very rough estimate of the minimum cost.

Potential for Evaporative Precoolers

In the last post we described a possible configuration for an evaporative precooler to lower total air conditioning operating costs at the expense of some additional capital costs (ducts, heat exchanger, evaporator) and perhaps a little additional maintenance costs on those items.   Of course, in order to make a decision on the payoff time, you have to know your climate conditions, your equipment costs, your operating costs, and the potential savings from the addition of the evaporative cooler.  In this post, we’ll provide a fuller description of the potential benefit you might be able to expect from an evaporative cooler for given inlet conditions.

An Evaporative Pre-cooler

We talked in an earlier post about evaporative cooling and how you can use it to cool off air by simply evaporating water.  Evaporative coolers work best in dry climates, and are much cheaper to operate than vapor compression systems since there is no electricity-hungry compressor.  Unfortunately, they result in a large increase in the relative humidity of the air which may render it unacceptable for some indoor air applications.  In this post we’ll talk about how evaporative coolers are used in combination with other air conditioning equipment to lower the overall cost of providing conditioned air.

Water Lost Through Breathing, Part 2

In the last post we talked about the water loss from breathing and used the assumptions of exhaled air being at 92 deg F and 90% relative humidity, and inhaled air close to freezing, to develop a constant to estimate the water loss per hour for any breathing rate. This time, we’ll look at the effect of temperature and relative humidity and elevation on that constant.

Water Lost Through Breathing

Have you ever wondered how much water you lose by breathing? Do you think that it is more or less than that lost through sweating? Most of the time when we breathe, we are exhaling moister air than we breathe in. There might be a few exceptions, but normally our bodies are losing a little bit of moisture with every breath. In this blog, we’ll try to quantify that moisture loss, at least in a ballpark way. 

Evaporative Cooling

Last post we talked about the psychrometric chart and the process that moist air follows on the chart when it is cooled until condensation begins.  You may be familiar with cooling systems that are variously termed “evaporative coolers”, “swamp coolers”, “desert coolers” and other names.  These systems work on something sort of like the inverse of the condensation process that we talked about last time.  Instead of cooling the moist air until liquid water condenses out, these systems evaporate liquid water into the air in order to cool it. 

Condensation from the Atmosphere

Have you ever noticed the beads of water that form on a cold beverage container in warm humid weather?  Or been annoyed by the fog that obscures your bathroom mirror when you are ready to shave or apply makeup?  Or seen white clouds billowing out of the tailpipe of a car on a cold day? These are all examples of water vapor in the air condensing into a liquid.  In the first two cases, the liquid condensation had formed on a cool surface, but condensation also occurs any time that you can see clouds, fog, or steam, as in the third case.  Water vapor is colorless and transparent, so when you can see a cloud, it is visible because of light reflecting off of tiny droplets of liquid.  In other words, condensation has already occurred by the time that you can see anything.