Airmar PB100 Technical Information Seite 54

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54
About the Air Temperature Sensor
The WeatherStation includes a built-in negative temperature coefficient thermistor
that measures the ambient air temperature. This NTC thermistor is located in a
thermally isolated region of the WeatherStation housing that is open to the
outside air.
About the Relative Humidity Sensor
The WeatherStation contains a capacitive cell humidity sensor that measures the
relative humidity of the air. Humidity refers to the amount of water vapor in the air.
Relative humidity is the percentage of saturation of the water vapor in the air. It is
the ratio of the moisture content of the air to the saturated moisture level at the
same temperature and pressure.
About Dew Point
Dew point is the temperature at which the water vapor in the air begins to
condense into a liquid. If the air were gradually cooled while maintaining constant
moisture content, the relative humidity would rise until it reaches 100%. The air
temperature at this point of saturation is called the dew point.
If the air is dry enough, it is possible to have a dew point that is below freezing.
The dew point is then sometimes referred to as the frost point.
The WeatherStation calculates dew point from the measured air temperature and
relative humidity sensor readings.
About Wind Chill Temperature
Wind Chill is a term that describes the heat loss on the human body resulting from
the combined effects of low temperature and wind. As wind speed increases, heat
is carried away from the body at a faster rate, causing a reduction in skin
temperature. Because the face is the part of the human body that is most likely to
be exposed, the wind chill index is adjusted for the average adult face.
The concept of wind chill does not apply to inanimate objects, such as a boat. The
only effect that wind chill has in this case is to shorten the time it takes the object
to cool to the actual air temperature––wind chill does not cause an object to cool
below that temperature. For example, fresh water freezes at 0°C (32°F)
regardless of what the wind chill is.
The WeatherStation calculates two values for wind chill temperature: one using
the apparent wind speed, and one using the true wind speed. The
apparent
wind
chill temperature is relevant to what an observer is currently experiencing on the
vessel. The
true
wind chill temperature indicates what the wind chill would be if the
vessel were not moving.
Wind chill temperature is only defined for temperatures at or below 10°C (50°F)
and wind speeds above 2.6 knots (3MPH).
By default, transmission of wind chill data is disabled by the WeatherStation.
When used with WeatherCaster, the wind chill data will be automatically enabled.
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