| Автор | Kays, Marvin |
| Автор | Craig, Richard A. |
| Дата выпуска | 1966 |
| dc.description | In a recent paper [Kays and Craig, 1965], we evaluated temperature advection V·∇T from the equation (1)V⋅∇T=−(ƒT/g)V2∂θ/∂zwhere V is the velocity, T the temperature, ƒ the Coriolis parameter, g the gravity field strength, V the wind speed, and θ the wind direction. Small‐scale structure, which is present in the wind field in the upper stratosphere, was eliminated by smoothing V<sup>2</sup> and θ separately. Alternatively, one can compute temperature advection from the equation (2)V⋅∇T=−(ƒT/g)(u ∂u/∂z−v ∂u/∂z)where u is the wind component toward the east and υ the wind component toward the north. In this case, u and υ can be smoothed separately. |
| Формат | application.pdf |
| Копирайт | Copyright 1966 by the American Geophysical Union. |
| Тема | MARINE GEOLOGY AND GEOPHYSICS |
| Тема | Meteorology: Convection, turbulence, and diffusion |
| Название | The order of magnitude of large‐scale vertical motions in the upper stratosphere, 2 |
| Тип | article |
| DOI | 10.1029/JZ071i008p02171 |
| Electronic ISSN | 2156-2202 |
| Print ISSN | 0148-0227 |
| Журнал | Journal of Geophysical Research |
| Том | 71 |
| Первая страница | 2171 |
| Последняя страница | 2171 |
| Выпуск | 8 |
| Библиографическая ссылка | Kays, M., Richard A.Craig, On the order of magnitude of large‐scale vertical motions in the upper stratosphere, J. Geophys. Res., 7018, 4453–4461, 1965. |
