The older of the models of extratropical cyclone development is known as the Norwegian cyclone model, developed during and shortly after World War I within the Bergen School of Meteorology. In this theory, cyclones develop as they move up and along a frontal boundary, eventually occluding and reaching a barotropically cold environment. It was developed completely from surface-based weather observations, including descriptions of clouds found near frontal boundaries. Developed from this model was the concept of the warm conveyor belt, which transports warm and moist air just ahead of the cold front above the surface warm front.
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| - Norwegian cyclone model (en)
- Modelo norueguês de ciclones (pt)
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| - The older of the models of extratropical cyclone development is known as the Norwegian cyclone model, developed during and shortly after World War I within the Bergen School of Meteorology. In this theory, cyclones develop as they move up and along a frontal boundary, eventually occluding and reaching a barotropically cold environment. It was developed completely from surface-based weather observations, including descriptions of clouds found near frontal boundaries. Developed from this model was the concept of the warm conveyor belt, which transports warm and moist air just ahead of the cold front above the surface warm front. (en)
- O modelo norueguês de ciclones é um dos mais antigos de previsão de ciclones extratropicais. O modelo norueguês de ciclones foi desenvolvido pela Escola de meteorologia de Bergen durante e pouco depois da Primeira Guerra Mundial. Nesta teoria, ciclones extratropicais se desenvolvem assim que se deslocam acima e ao longo de um limite frontal, ocludindo-se e alcançando um ambiente barotropicamente frio. O modelo foi desenvolvido completamente de observações meteorológicas de superfície, incluindo a descrição das nuvens perto do limite frontal. O conceito de esteira rolante quente, em meteorologia, que transporta calor e ar úmido logo a frente da frente fria acima da frente quente de superfície, foi desenvolvido a partir deste modelo de ciclones. (pt)
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| - A mature low pressure system (en)
- Dissipating stage of cyclone (en)
- Initial stage (en)
- Wave forms on front (en)
- Wave intensifies (en)
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| - Stages of development (en)
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| - Norwegian cyclone model 2 wave forms on front, 3D view.jpg (en)
- Cyclo 2.svg (en)
- Cyclo 3.svg (en)
- Cyclo 4.svg (en)
- Cyclo 5.svg (en)
- Cyclo1.png (en)
- Norwegian cyclone model 3 wave intensifies, 3D view.jpg (en)
- Norwegian cyclone model 5 dissipating stage of cyclone, 3D view.jpg (en)
- Norwegian cyclone model 1 initial stage, 3D view.jpg (en)
- Norwegian cyclone model 4 a mature low pressure system, 3D view.jpg (en)
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| - The older of the models of extratropical cyclone development is known as the Norwegian cyclone model, developed during and shortly after World War I within the Bergen School of Meteorology. In this theory, cyclones develop as they move up and along a frontal boundary, eventually occluding and reaching a barotropically cold environment. It was developed completely from surface-based weather observations, including descriptions of clouds found near frontal boundaries. Developed from this model was the concept of the warm conveyor belt, which transports warm and moist air just ahead of the cold front above the surface warm front. (en)
- O modelo norueguês de ciclones é um dos mais antigos de previsão de ciclones extratropicais. O modelo norueguês de ciclones foi desenvolvido pela Escola de meteorologia de Bergen durante e pouco depois da Primeira Guerra Mundial. Nesta teoria, ciclones extratropicais se desenvolvem assim que se deslocam acima e ao longo de um limite frontal, ocludindo-se e alcançando um ambiente barotropicamente frio. O modelo foi desenvolvido completamente de observações meteorológicas de superfície, incluindo a descrição das nuvens perto do limite frontal. O conceito de esteira rolante quente, em meteorologia, que transporta calor e ar úmido logo a frente da frente fria acima da frente quente de superfície, foi desenvolvido a partir deste modelo de ciclones. (pt)
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