LATENT REFERENCES / TAG2
Indian Ocean Dipole
Original title: ダイポールモード減少
This reference note belongs to Tag2 in Latent References, an archive curated by Keigo Yoshida. Its archive region is eme · Bricolage. The note preserves its source text and links so that readers can trace the material behind the 3D map.
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The Indian Ocean Dipole is an atmosphere-ocean phenomenon in which tropical Indian Ocean water temperatures fall in the east and rise in the west from early summer to late autumn. Including accompanying changes in wind and climate, it has been shown to strongly influence global climate like El Niño.
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ダイポールモード現象とは、インド洋熱帯域において初夏から晩秋にかけて東部で海水温が低くなり、西部で海水温が高くなる大気海洋現象の事を言う。それに伴って起こる風や気候の変化を含み、エルニーニョ現象と同様に世界の気候に大きな影響を与える事が明らかになった。
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Source updated 2024-10-04 · Snapshot 2026-10-08