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Frontogenesis is a meteorological process of tightening of horizontal temperature gradients to produce fronts. In the end, two types of fronts form: cold fronts and warm fronts. A cold front is a narrow line where temperature decreases rapidly. A warm front is a narrow line of warmer temperatures and essentially where much of the precipitation occurs.…
Elements of frontogenesis, Development of the frontogenetical circulation & 3-Dimensional equation
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horizontal temperature deformation cold front warm gradient shear fronts divergence wind vertical gradients line equation mid-latitude air along rossby geostrophic
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Frontogenesis | is a | meteorological process of tightening of horizontal temperature gradients to produce fronts | 0.90 | text |
| Frontogenesis | related to 3-Dimensional equation | The | 0.60 | section |
| Frontogenesis | related to Development of the frontogenetical circulation | During | 0.60 | section |
| Frontogenesis | related to Development of the frontogenetical circulation | To | 0.60 | section |
| Frontogenesis | related to Development of the frontogenetical circulation | Mass | 0.60 | section |
| Frontogenesis | related to Development of the frontogenetical circulation | Although | 0.60 | section |
| Frontogenesis | related to Development of the frontogenetical circulation | There | 0.60 | section |
| Frontogenesis | related to Elements of frontogenesis | The | 0.60 | section |
| Frontogenesis | related to Elements of frontogenesis | Rossby | 0.60 | section |
| Frontogenesis | related to References | Holton | 0.60 | section |
| Frontogenesis | related to References | An | 0.60 | section |
| Frontogenesis | related to References | Vol | 0.60 | section |
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