"substorm current wedge" meaning in All languages combined

See substorm current wedge on Wiktionary

Noun [English]

Forms: substorm current wedges [plural]
Head templates: {{en-noun}} substorm current wedge (plural substorm current wedges)
  1. A sudden disruption of an azimuthally confined section of enhanced current across a magnetotail and its diversion to the auroral ionosphere via field-aligned currents.
    Sense id: en-substorm_current_wedge-en-noun-RfMxCSxK Categories (other): English entries with incorrect language header, Pages with 1 entry, Pages with entries

Inflected forms

Alternative forms

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      "examples": [
        {
          "ref": "2000, Shin-ichi Ohtani, Ryoichi Fujii, Michael Hesse, Magnetospheric Current Systems, page 199:",
          "text": "In particular, the relative contributions of ionospheric Pedersen and Hall currents to field-aligned currents are evaluated in hoping to shed some new light on the ionospheric closure of the substorm current wedge.",
          "type": "quote"
        },
        {
          "ref": "2015, Yongliang Zhang, Larry J. Paxton, Auroral Dynamics and Space Weather, page 106:",
          "text": "These are all signatures of substorm current wedge formation, indicating that current wedge formation is more of a response to the current system and accompanying dipolarization of postonset plasmasheet flow bursts than to the process leading to substorm auroral onset. If this is the case, then, while substorm current wedge formation is critical to substorm expansion phase development, it may not be a critical aspect of the substorm onset process.",
          "type": "quote"
        },
        {
          "ref": "2022, Wolfgang Baumjohann, Rudolf A Treumann, Basic Space Plasma Physics, page 117:",
          "text": "The substorm current wedge diverts part of the neutral sheet current along magnetic field lines through the ionosphere.",
          "type": "quote"
        }
      ],
      "glosses": [
        "A sudden disruption of an azimuthally confined section of enhanced current across a magnetotail and its diversion to the auroral ionosphere via field-aligned currents."
      ],
      "id": "en-substorm_current_wedge-en-noun-RfMxCSxK",
      "links": [
        [
          "disruption",
          "disruption"
        ],
        [
          "azimuthally",
          "azimuthally"
        ],
        [
          "magnetotail",
          "magnetotail"
        ],
        [
          "auroral",
          "auroral"
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          "ionosphere",
          "ionosphere"
        ],
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          "current",
          "current"
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        },
        {
          "ref": "2015, Yongliang Zhang, Larry J. Paxton, Auroral Dynamics and Space Weather, page 106:",
          "text": "These are all signatures of substorm current wedge formation, indicating that current wedge formation is more of a response to the current system and accompanying dipolarization of postonset plasmasheet flow bursts than to the process leading to substorm auroral onset. If this is the case, then, while substorm current wedge formation is critical to substorm expansion phase development, it may not be a critical aspect of the substorm onset process.",
          "type": "quote"
        },
        {
          "ref": "2022, Wolfgang Baumjohann, Rudolf A Treumann, Basic Space Plasma Physics, page 117:",
          "text": "The substorm current wedge diverts part of the neutral sheet current along magnetic field lines through the ionosphere.",
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        }
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        "A sudden disruption of an azimuthally confined section of enhanced current across a magnetotail and its diversion to the auroral ionosphere via field-aligned currents."
      ],
      "links": [
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          "disruption",
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          "azimuthally",
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          "magnetotail",
          "magnetotail"
        ],
        [
          "auroral",
          "auroral"
        ],
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          "ionosphere",
          "ionosphere"
        ],
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        ]
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  "word": "substorm current wedge"
}

Download raw JSONL data for substorm current wedge meaning in All languages combined (2.0kB)


This page is a part of the kaikki.org machine-readable All languages combined 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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