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词汇 cyclogenesis
释义

Definition of cyclogenesis in English:

cyclogenesis

noun ˌsʌɪkləʊˈdʒɛnəsɪsˌsaɪkloʊˈdʒɛnəsəs
mass nounMeteorology
  • The development or strengthening of an area of low pressure in the atmosphere, resulting in the formation of a cyclone.

    cyclogenesis is common on the lee side of the mountains at the locations of the Alberta and Colorado storm track
    Example sentencesExamples
    • A cyclogenesis system is moving far north of the UK and is expected to pass over Ireland as it moves slowly eastwards towards Iceland.
    • The low developed off the coast of Japan, one of the areas of cyclogenesis that affects this area.
    • The atmospheric flow will also have an influence, as strong vertical wind shear can inhibit cyclogenesis.
    • Conditions are particularly suited to such cyclogenesis in winter off the east coasts of Asia and North America where horizontal temperature gradients are greatest.
    • The main energy (the Yukon energy bundle) is more northerly track, perhaps producing cyclogenesis well off the east coast of Long Island.

Origin

1920s: from cyclo- + genesis.

Definition of cyclogenesis in US English:

cyclogenesis

nounˌsaɪkloʊˈdʒɛnəsəsˌsīklōˈjenəsəs
Meteorology
  • The development or strengthening of an area of low pressure in the atmosphere, resulting in the formation of a cyclone.

    cyclogenesis is common on the lee side of the mountains at the locations of the Alberta and Colorado storm track
    Example sentencesExamples
    • The main energy (the Yukon energy bundle) is more northerly track, perhaps producing cyclogenesis well off the east coast of Long Island.
    • A cyclogenesis system is moving far north of the UK and is expected to pass over Ireland as it moves slowly eastwards towards Iceland.
    • The low developed off the coast of Japan, one of the areas of cyclogenesis that affects this area.
    • The atmospheric flow will also have an influence, as strong vertical wind shear can inhibit cyclogenesis.
    • Conditions are particularly suited to such cyclogenesis in winter off the east coasts of Asia and North America where horizontal temperature gradients are greatest.

Origin

1920s: from cyclo- + genesis.

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