𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Organization of precipitation along cold fronts

✍ Scribed by Michael J. Brown; John D. Locatelli; Peter V. Hobbs


Publisher
John Wiley and Sons
Year
1998
Tongue
English
Weight
294 KB
Volume
124
Category
Article
ISSN
0035-9009

No coin nor oath required. For personal study only.


πŸ“œ SIMILAR VOLUMES


Precipitation growth at a cold front
✍ P. R. Jonas; R. C. Tabony πŸ“‚ Article πŸ“… 1973 πŸ› John Wiley and Sons 🌐 English βš– 541 KB

## Abstract A simple model of the growth of precipitation particles in cloud systems in which the air flow is known has been used to calculate the growth of hail pellets at a cold front. The calculated pellet sizes and densities, and surface rainfall rates, are consistent with observations. It is s

On the propagation of cold fronts
✍ M. J. Manton πŸ“‚ Article πŸ“… 2007 πŸ› John Wiley and Sons 🌐 English βš– 501 KB

## Abstract The assumption of steady two‐dimensional flow imposes constraints on the motion of a layer of cold air propagating through a body of warm air. Some general properties, such as the propagation speed of the front, can be deduced from consideration of the equations of motion away from the

Mesoscale structure of line convection a
✍ P. K. James; K. A. Browning πŸ“‚ Article πŸ“… 1979 πŸ› John Wiley and Sons 🌐 English βš– 708 KB

## Abstract In this paper we consider 15 cases of line convection at ana‐cold fronts which have been observed by radar. Although line convection can be a simple two‐dimensional feature, it is usually broken up into line elements having lengths from a few to many tens of kilometres separated by some

Precipitation fronts and the reflection
✍ Olivier Pauluis; Dargan M. W. Frierson; Andrew J. Majda πŸ“‚ Article πŸ“… 2008 πŸ› John Wiley and Sons 🌐 English βš– 508 KB

## Abstract This paper investigates the interactions between precipitation and the circulation in an idealized model for the tropical atmosphere where convection is represented by a quasi‐equilibrium closure. When studying large‐scale circulation in the Tropics, the governing equations can be furth