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Kestrel, 4250 racing weather, Tracker 21 glossary – Kestrel 4250 (Racing) User Manual

Page 11

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Kestrel

®

4250 Racing Weather

®

Tracker

21

GLOSSARY

The below definitions have been greatly simplified in order to keep this section brief. We strongly

recommend that anyone who wishes to make use of these measurements refer to one of the many

excellent weather references available for a more in-depth definition. On the internet, visit www.usatoday.

com or www.noaa.gov. Or, locate the USA Today publication, The Weather Book. Please note that any words

in a definition printed in italics are themselves defined in this glossary.
Altimeter Setting

An aviation term for the local barometric pressure. Same as reference pressure.
Altitude

The distance above sea level. The Kestrel Meter calculates altitude based on the measured station pressure

and the input barometric pressure — or “reference pressure”.
Air Density

The mass of air per unit volume. It is a function of temperature, humidity, and pressure.
Barometric Pressure

The air pressure of your location reduced to sea level. Pressure will change as weather systems move into

your location. Falling pressure indicates the arrival of a low pressure system and expected precipitation or

storm conditions. Steady or rising pressure indicates clear weather. A correct altitude must be input for the

Kestrel Meter to display barometric pressure correctly.
Density Altitude

The altitude at which you would be, given the current air density. Often used by individuals who tune

high performance internal combustion engines, such as race car engines. Also of interest pilots in order to

determine how an aircraft will perform.

Dewpoint

The temperature to which air must be cooled in order for condensation to occur. The difference between

dewpoint and temperature is referred to as the “temperature/dew point spread”. A low dewpoint spread

indicates high relative humidity, while a large dewpoint spread indicates dry conditions.
Heat Index

A practical measure of how hot the current combination of relative humidity and temperature feels to a

human body. Higher relative humidity makes it seem hotter because the body’s ability to cool itself by

evaporating perspiration is reduced.
Moisture Content (Water Grains)

The ratio between the actual mass of water vapor present in moist air — to the mass of the dry air.
Reference Pressure

The local barometric pressure. Input to the altitude screen to provide correct altitude readings. Also known

as the altimeter setting.
Relative Air Density

A proportion of measured air density to standard air density. Standard air density uses standard (fixed)

values for temperature, humidity and pressure.
Relative Humidity

The amount of water vapor actually in the air divided by the maximum amount of water vapor the air could

hold at that temperature, expressed as a percentage.
Station Pressure

The air pressure of your location, NOT reduced to the sea level equivalent.