Clothing insulation is the thermal insulation provided by clothing.
Even if the main role of clothing is to protect from the cold, protective clothing also exists to protect from heat, such as for metallurgical workers or firemen. As regards thermal comfort, only the first case is considered.
Thermophysiological comfort is the capacity of the clothing material that makes the balance of moisture and heat between the body and the environment. It is a property of textile materials that creates ease by maintaining moisture and thermal levels in a human's resting and active states. The selection of textile material significantly affects the comfort of the wearer. Different textile fiber holds individual properties that suit in different environments. Natural fibers are breathable and absorb moisture, while synthetic fibers are hydrophobic; they repel moisture and do not allow air to pass. Different environments demand a diverse selection of clothing materials. Hence the appropriate choice is important. The major determinants that influence Thermophysiological comfort are the permeable construction, heat, and moisture transfer rate.
There are three kinds of heat transfer: conduction (exchange of heat through contact), convection (movement of fluids), and radiation.
Air has a low thermal conductivity but is very mobile. There are thus two elements that are important in protecting from the cold:
Another important factor is humidity. Water is a better conductor of heat than air, thus if clothes are damp â because of sweat, rain, or immersion â water replaces some or all of the air between the fibres of the clothing, causing thermal loss through conduction and/or evaporation.
Thermal insulation is thus optimal with three layers of clothing:
The layers of trapped air between the skin and the exterior surface play a major insulating role. If the clothing is squeezed tight (as by the straps of a backpack), insulation will be poorer in those places. Insulation is improved when convection in the air layers is minimised.
Clothing insulation may be expressed in clo units. The clo has the same dimensions as the R value (square metre kelvins per watt or m<sup>2</sup>â K/W) used to describe insulation used in residential and commercial constructionâÂÂthus, the higher the value, the better the insulation performance.
There are a number of ways to determine clothing insulation provided by clothes, but the most accurate according to ASHRAE Fundamentals are measurements on heated manikins and on active subjects. Equations may then be used to calculate the thermal insulation. Because clothing insulation cannot be measured for most routine engineering applications, tables of measured values for various clothing ensembles can be used. According to ASHRAE-55 2010 standard, there are three methods for estimating clothing insulation using the tables provided.
Another unit that is used is the "tog":
The name comes from the word "togs", British slang for clothes.
Icl is intrinsic clo, which is the clo of the garment * the percent of body surface area covered by that garment. Thus, you can add up the intrinsic clo of all the garments and get the total clo of your body.
The above applies more to clothing worn indoors. It references the ASHRAE handbook which is used to design HVAC systems for indoor spaces. Outdoors the temperature range is much larger, and the exertion level range can be much higher so clothing is different.
When it's cold, if the skin temperature gets below 30 C (86 F) the human will be uncomfortable. The goal of clothing insulation is to keep the skin temperature at that temperature or above. Comfort
The skin temperature can be determined using the differential form of Fouriers Law (Thermal conduction).
where (including the SI units)
Doing a little algebra we can reformulate.
where
and
where
substituting k and T and reordering
The heat flux (q) of the human body is (Metabolic equivalent of task)
where MET is the exertion level.
Now we can figure out if we'll be warm. We know the temperature of the skin when we're just barely warm (30 C = 86 F). If the ambient temperature is greater than (skin temperature - T), then we'll be warm.
This is overly simplistic but it's too complicated to do more than this. Different parts of the body have different heat flux, skin temperature, and insulation. We can just average over the entire body and we'll be close. Wind, radiant heat loss, and humidity also affect this. We can still make some reasonable conclusions.
R value of different insulations
Now, we can look at a number of cases. First, consider the lightest insulation from that table, fleece, at different exertion levels. Calculate the minimum comfort temperature using the formula above:
For example, wearing fleece, when sleeping (MET = 0.8), the minimum temperature where you'll be comfortable is 72 F (22 C). You would have to wear this all over your body.
You can see that at high exertion levels, even light insulation is warm down to very cold temperatures. The result for this cold is inaccurate - the assumptions about equal coverage over the entire body, wind, radiant heat loss, and humidity are too great, but it gives a general idea.
There is a useful strategy that comes from this. If you're cold, increase your exertion level.
Next, consider a number of different insulations at a low exertion level:
For example, wearing fleece, standing around (MET = 1.5), the minimum temperature where you'll be comfortable is 59 F (15 C).
Again, the results for the coldest cases are inaccurate - the assumptions about equal coverage over the entire body, wind, radiant heat loss, and humidity are too great, but it gives a general idea. If you had the heavy insulation over your entire body, you could survive very cold temperatures. It's important to have insulation over your head. Conventional wisdom is "if you want to keep warm, put a hat on".