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17 Barometrische / Atmosferische
Druk
Atmosferische druk is de druk op een willekeurige plaats op
aarde, veroorzaakt door het gewicht van de luchtkolom er-
boven. Een atmosferische druk verwijst naar de gemiddelde
druk en neemt geleidelijk af naarmate de hoogte toeneemt.
Meteorologen gebruiken barometers om de luchtdruk te me-
ten. Aangezien de variatie in luchtdruk sterk beïnvloed
wordt door het weer, is het mogelijk om het weer te voor-
spellen door de drukveranderingen te meten.
1. Druk op de BARO-knop om te schakelen tussen de
weergave van de barometerdruk in inHg of in hPa.
2. Druk 3 seconden op de BARO knop om te wisselen
tussen absolute en relatieve atmosferische druk.
ABSOLUTE: de absolute atmosferische druk van uw lo-
catie.
RELATIEF: de relatieve atmosferische druk op basis
van de zeespiegel.
Relatieve atmosferische drukwaarde instellen
3. Haal de atmosferische drukgegevens van de zeespie-
gel (het is ook de relatieve atmosferische drukgege-
vens van uw thuisgebied) via de lokale weerdienst, in-
ternet en andere kanalen.
4. Houd de BARO-toets ca. 3 seconden ingedrukt tot
"abs" of "rel" knippert.
5. Druk op de toets CH/UP of 12/24/DOWN-toets om over
te schakelen naar de "rel"-modus.
107


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