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airborne geomagnetic - translation to russian
нефтегазовая промышленность
аэромагниторазведка
общая лексика
геомагнитный полюс
.jpg?width=200)
![A [[Brazilian Air Force]] [[Embraer R-99]]](https://commons.wikimedia.org/wiki/Special:FilePath/Aeronaves Ágata 7 - FAB - EMB145 Erieye.jpg?width=200 "A [[Brazilian Air Force]] [[Embraer R-99]]")
![The [[KJ-2000]] is based on the [[Beriev A-50]] aircraft.](https://commons.wikimedia.org/wiki/Special:FilePath/Airborne early warning and control aircraft A-50U (Red 41).jpg?width=200 "The [[KJ-2000]] is based on the [[Beriev A-50]] aircraft.")
![E-767]] of the [[Japan Air Self Defense Force]]](https://commons.wikimedia.org/wiki/Special:FilePath/Boeing E-767 (light).jpg?width=200 "E-767]] of the [[Japan Air Self Defense Force]]")
![[[Lockheed EC-121]]M one of the first AEW aircraft](https://commons.wikimedia.org/wiki/Special:FilePath/Lockheed EC-121M with F-4B (cropped).jpg?width=200 "[[Lockheed EC-121]]M one of the first AEW aircraft")
![An AEW [[Westland Sea King]] helicopter of the [[Royal Navy]]](https://commons.wikimedia.org/wiki/Special:FilePath/Royal Navy AEW Seaking Helicopter from 849 Naval Air Squadron MOD (cropped).jpg?width=200 "An AEW [[Westland Sea King]] helicopter of the [[Royal Navy]]")
![A Boeing 737 AEW&C of the [[Turkish Air Force]]](https://commons.wikimedia.org/wiki/Special:FilePath/Turkish Air Force Boeing 737-700 KvW.jpg?width=200 "A Boeing 737 AEW&C of the [[Turkish Air Force]]")
.jpg?width=200 "Wellington Ic \"Air Controlled Interception\" showing rotating radar antenna")
Wikipedia
A geomagnetic excursion, like a geomagnetic reversal, is a significant change in the Earth's magnetic field. Unlike reversals, an excursion is not a "permanent" re-orientation of the large-scale field, but rather represents a dramatic, typically a (geologically) short-lived change in field intensity, with a variation in pole orientation of up to 45° from the previous position.
Excursion events typically only last a few thousand to a few tens of thousands of years, and often involve declines in field strength to between 0 and 20% of normal. Unlike full reversals, excursions are generally not recorded around the entire globe. This is certainly due in part to them not registering well in the sedimentary record, but it also seems likely that excursions may not typically extend through the entire global geomagnetic field. There are significant exceptions, however.
