How’s the weather outside today? Are you feeling a little warmer than you would like? Have you seen the weather forecast, and do you really know what all those numbers mean?
The simplest is temperature which is a measurement of the heat content of the air. The two popular scales are Celsius and Fahrenheit. Both have two defined points: the freezing point of fresh water at sea level is 0°C / 32°F, and the boiling point of fresh water at sea level is 100°C / 212°F. Note that the Fahrenheit scale, created in 1724 based on experiments carried out at that time by Polish physicist Danielle Gabriel Fahrenheit, is commonly used today in only four countries including Belize, Myanamar, Liberia and the United States, and only for non-scientific applications.
Another popular number shown on most weather predictions is either heat index or wind chill. If the apparent temperature, the “it-feels-like” number, is higher than the actual temperature, it is shown as heat index; if it is lower, it is shown as wind chill. The heat index is derived from temperature and relative humidity and indicates heat gained between the human body and the atmosphere. The wind chill is derived from temperature and wind speed and indicates heat lost between the human body and the atmosphere.
The human body removes heat by perspiring and letting drier air wick heat away. When the relative humidity is high enough that perspiration does not evaporate, then there is no cooling effect. The human body begins to absorb heat from the atmosphere and is in danger of suffering a heat related illness. As heat or relative humidity rises, the combination becomes more dangerous. The National Weather Service has published the heat index shown here:

The wind chill index is derived from temperature and wind speed, and indicates heat lost between the human body and the atmosphere. Wind chill formulas vary greatly worldwide, but since 2001, the U.S., Canada and the U.K. have agreed on a standardized formula that uses the following assumptions: the wind is striking a bare face on a person walking 3mph into a 3mph headwind at an actual temperature of 10°C / 50°F or lower. As the actual temperature falls or the wind speed rises, the wind chill falls and the danger of a cold related illness increases. The National Weather Service has published the wind chill index shown here:

When reading a weather report, humidity and relative humidity are two terms often used interchangeably. However, humidity, properly called absolute humidity and expressed in grams, is the amount of water vapor, by weight, in a cubic meter of air. This measurement is rarely used outside of scientific experiments. Another term is dew point temperature, a number that is considered by most meteorologists to be a better indicator of moisture in the air than relative humidity.
Relative humidity is the amount of water vapor in the air relative to the maximum amount of water vapor that air can hold at a given temperature. As the temperature rises but the water content remains the same, relative humidity drops because warmer air can hold more water vapor than cooler air. This means that if the air temperature is 80°F at noon and 84°F at 2:00 pm, but the water vapor content is constant, relative humidity will be lower at 2:00 pm even though the air is not any drier. And what we “feel” is the actual amount of moisture, i.e. the absolute humidity, in the air. So, while the relative humidity is dropping, it does not “feel” more comfortable.
The dew point temperature is also an indicator of how much water vapor is in the air, as well as how it “feels” to us. Dew point is calculated by the use of a hygrometer, a polished metal mirror that is cooled until water vapor in the air starts to condense on the surface. The temperature when condensation first starts is the dew point temperature.
When the outside air temperature cools down to where it is the same as the dew point, water condenses to form fog at surface levels, clouds at levels aloft, or a film of dew on surfaces. The larger the spread between temperature and dew point, the more comfortable we feel because as the temperature rises and the dew point remains constant or falls, the air becomes drier.
Humidity can make you feel uncomfortable whether you are in shade or sun, whether it is windy or calm, or whether you are acclimated to heat or not. As the dew point gets higher and closer to the actual temperature, we start to feel that humidity; we start to feel ‘sticky’. Remember, a person gets cool by perspiring, and no matter what the actual temperature, we can only get cool when perspiration can evaporate which only happens when air is not already saturated. A dew point greater than 65 is uncomfortable to most people. Dew point temperatures above 70 indicate unstable air conditions that may lead to severe weather.
All of this and more is included in the science of biometeorology; the study of weather and its effects on the human body. I will look at additional aspects of this science in later columns. To locate these numbers, take a look at your favorite weather website, or try one of the following:
| www.weather.com The Weather Channel Today, Hourly, 10-day Temp, clouds, wind speed & direction, chance of precip, heat index, windchill, humidity, UV index |
| www.accuweather.com Accuweather Hourly, Daily, Radar, Air Quality Temp, clouds, wind speed & direction, Humidity, UV, DP |
| www.wunderground.com Weather Underground Hourly, Daily, Historical Temp, clouds, wind speed & direction, chance of precip, heat index, windchill, humidity, DP, pressure |
| www.weather.gov National Weather Service / NOAA Current, Daily Forecast, History Temp, clouds, wind speed & direction, humidity, pressure, DP |
| www.weatherbug.com Weatherbug Current, Hourly, 10-day Temp, clouds, wind speed & direction, heat index, windchill, humidity, DP |
| https://www.wsdot.com/traffic/passes/snoqualmie/ Snoqualmie Current Weather My favorite ski area 🙂 |









































































