𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Measurements of cloud droplet size distributions in seeded warm cumulus clouds

✍ Scribed by R. K. Kapoor; S. K. Paul; A. S. Ramachandra Murty; K. Krishna; S. K. Sharma; Bh. V. Ramana Murty

Publisher
Springer
Year
1976
Tongue
English
Weight
622 KB
Volume
114
Category
Article
ISSN
0033-4533

No coin nor oath required. For personal study only.

πŸ“œ SIMILAR VOLUMES

Early evolution of the largest-sized dro
Early evolution of the largest-sized droplets in maritime cumulus clouds
✍ Jason H. Lowenstein; Alan M. Blyth; R. Paul Lawson πŸ“‚ Article πŸ“… 2010 πŸ› John Wiley and Sons 🌐 English βš– 209 KB

## Abstract Droplet size distributions (DSDs) measured within a distance of approximately 1 km above the base of shallow maritime cumulus clouds during the Rain in Cumulus over the Ocean (RICO) field campaign are compared with results of a condensation and stochastic coalescence model, run in the f

On the droplet distribution near the bas
On the droplet distribution near the base of cumulus clouds
✍ M. J. Manton; J. Warner πŸ“‚ Article πŸ“… 1982 πŸ› John Wiley and Sons 🌐 English βš– 770 KB

## Abstract Lateral entrainment in cumulus clouds is usually assumed to occur continuously as a cloud parcel rises. Computations of the droplet distribution using that assumption are compared with those in which entrainment occurs intermittently, and little difference is found. The width of the dro

The size of cloud droplets in layer-type
The size of cloud droplets in layer-type cloud
✍ A. C. Best πŸ“‚ Article πŸ“… 1951 πŸ› John Wiley and Sons 🌐 English βš– 432 KB

## Abstract The rate of growth of cloud droplets round a salt nucleus is examined and it is shown that, with nuclei of the size quoted in published measurements, the drop radius achieved in the period before the droplet is carried out of the cloud layer by turbulent diffusion is in reasonable accor

The evolution of droplet spectra and lar
The evolution of droplet spectra and large droplets by condensation in cumulus clouds
✍ B. J. Mason; P. R. Jonas πŸ“‚ Article πŸ“… 1974 πŸ› John Wiley and Sons 🌐 English βš– 759 KB

## Abstract The paper describes a relatively simple model of a non‐precipitating cumulus cloud that grows by the ascent of successive spherical thermals through the residues of their predecessors, mixing with the surroundings being determined by the relative velocity and the radius of the thermal.