"Madden-Julian oscillation" meaning in English

See Madden-Julian oscillation in All languages combined, or Wiktionary

Proper name

Forms: the Madden-Julian oscillation [canonical]
Etymology: Discovered in 1971 by Roland Madden and Paul Julian of the American National Center for Atmospheric Research. Head templates: {{en-proper noun|def=1}} the Madden-Julian oscillation
  1. (meteorology) The largest element of the intraseasonal variability in the tropical atmosphere: a large-scale coupling between atmospheric circulation and tropical deep convection, manifesting itself most clearly as anomalous rainfall. Wikipedia link: Madden-Julian oscillation Categories (topical): Meteorology
    Sense id: en-Madden-Julian_oscillation-en-name-mfnwfUeL Categories (other): English entries with incorrect language header, Pages with 1 entry, Pages with entries Topics: climatology, meteorology, natural-sciences
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        "The largest element of the intraseasonal variability in the tropical atmosphere: a large-scale coupling between atmospheric circulation and tropical deep convection, manifesting itself most clearly as anomalous rainfall."
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      "links": [
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          "meteorology",
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          "intraseasonal"
        ],
        [
          "variability",
          "variability"
        ],
        [
          "tropical",
          "tropical"
        ],
        [
          "atmosphere",
          "atmosphere"
        ],
        [
          "coupling",
          "coupling"
        ],
        [
          "atmospheric",
          "atmospheric"
        ],
        [
          "circulation",
          "circulation"
        ],
        [
          "deep",
          "deep"
        ],
        [
          "convection",
          "convection"
        ],
        [
          "anomalous",
          "anomalous"
        ],
        [
          "rainfall",
          "rainfall"
        ]
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        "(meteorology) The largest element of the intraseasonal variability in the tropical atmosphere: a large-scale coupling between atmospheric circulation and tropical deep convection, manifesting itself most clearly as anomalous rainfall."
      ],
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        "climatology",
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          "deep",
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        ],
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          "convection",
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          "anomalous"
        ],
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        "(meteorology) The largest element of the intraseasonal variability in the tropical atmosphere: a large-scale coupling between atmospheric circulation and tropical deep convection, manifesting itself most clearly as anomalous rainfall."
      ],
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        "climatology",
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This page is a part of the kaikki.org machine-readable English dictionary. This dictionary is based on structured data extracted on 2024-11-06 from the enwiktionary dump dated 2024-10-02 using wiktextract (fbeafe8 and 7f03c9b). The data shown on this site has been post-processed and various details (e.g., extra categories) removed, some information disambiguated, and additional data merged from other sources. See the raw data download page for the unprocessed wiktextract data.

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