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Field-aligned irregularity

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General referenceInterpretive dossier study · Crown Archives visual atlas
Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionOct 1, 2023
Entity authorityQ5446968
Source-derived summary

A field-aligned irregularity (FAI) is an anisotropic (different values when measured in different directions) perturbation of plasma density associated with magnetic fields. FAIs are often thought of in the context of the Earth's ionosphere where several natural processes generate FAIs in the E-region and F-region.

They occur at 50 and 140 MHz, where electrons associated with the event become vertically aligned with Earth's magnetic field. FAI may occur for several hours after it starts. Optimum times for observance appear to be between 8 PM and midnight.

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The public source identifies “Field-aligned irregularity” as open-knowledge reference entry. This brief keeps that definition visible, then builds a research path around Field-aligned, irregularity and Open-knowledge.

Editorial reviewA practical starting point whose main value is the path it opens into stronger specialist and primary sources. The current 86-word lead offers orientation but no explicit four-digit date, so chronology should not be assumed. The selected authority fields contribute no independent date. Its value is orientation rather than verdict, with Field-aligned, irregularity and Open-knowledge providing the first useful test.
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This entry incorporates text from Field-aligned irregularity” on English Wikipedia. Contributors are listed in the page history. Text is available under the Creative Commons Attribution-ShareAlike 4.0 License. Selected authority identifiers and statements are retrieved from Wikidata under CC0; their references and qualifiers remain part of the verification path.