On formation and intensification of tropical cyclones by deep cumulus convection.
It is well established that the main energy source for the development of tropical cyclones is the release of latent heat of condensation. Broadly speaking, latent heat can be released through two entirely different mechanisms, namely (i) by mean vertical motion, and (ii) by small scale, deep cumulu...
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 1964 |
| País: | México |
| Institución: | UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO |
| Repositorio: | Geofísica Internacional |
| Idioma: | español |
| OAI Identifier: | oai:revistagi.geofisica.unam.mx:article/1672 |
| Acceso en línea: | http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1672 |
| Access Level: | acceso abierto |
| Palabra clave: | Ciclones tropicales Formación Convección profunda de cumulus Modelos dinámicos Dynamical models Tropical cyclones Formation Deep cumulus convection |
| Sumario: | It is well established that the main energy source for the development of tropical cyclones is the release of latent heat of condensation. Broadly speaking, latent heat can be released through two entirely different mechanisms, namely (i) by mean vertical motion, and (ii) by small scale, deep cumulus convection. |
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