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- W1428794893 abstract "Atmospheric fronts may be defined as sloping zones of pronounced transition in the thermal and wind fields. Consequently, they are characterized by a combination of relatively large horizontal temperature gradients, static stability, absolute vorticity (horizontal wind shear), and vertical wind shear. When depicted on quasi-horizontal surfaces, fronts appear as long, narrow features in which the along-front scale is typically an order of magnitude greater than the cross-front scale (1000–2000 km compared with 100–200 km). Therefore, according to the scale definitions of Orlanski (1975), the along-front dimension is meso-α (200–2000 km), and the cross-front dimension is meso-β (20–200 km). The scale of the middle-latitude baroclinic waves in which fronts are embedded ranges from meso-α to macro-β or synoptic (2000–10,000 km). Fronts are shallow phenomena, with depths typically 1–2 km. Because of this geometrical configuration, horizontal variations in the cross-front direction greatly exceed those in the along-front direction." @default.
- W1428794893 created "2016-06-24" @default.
- W1428794893 creator A5007138155 @default.
- W1428794893 date "1986-01-01" @default.
- W1428794893 modified "2023-10-02" @default.
- W1428794893 title "Atmospheric Fronts: An Observational Perspective" @default.
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- W1428794893 doi "https://doi.org/10.1007/978-1-935704-20-1_10" @default.
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