## Abstract Experimental data relating to drop size distribution in rain are examined and it is shown that in many cases the size distribution is in accordance with the following formulae 1 โ __F__ = exp [โ(x/a)^n^] __a__ = A I^p^ __W = C I^r^__ where __F__ = fraction of liquid water in the air com
Modification of the size distribution of falling raindrops by coalescence
โ Scribed by B. J. Mason; R. Ramanadham
- Publisher
- John Wiley and Sons
- Year
- 1954
- Tongue
- English
- Weight
- 456 KB
- Volume
- 80
- Category
- Article
- ISSN
- 0035-9009
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โฆ Synopsis
Abstract
The manner in which the size distribution of raindrops is modified during their fall by mutual coalescence, accretion with cloud droplets, and by evaporation below cloud base is investigated. It is shown that if a constant flux of raindrops having an exponetial size distribution occurs at the level of origin (just below the melting level in a layerโcloud) to give a steadyโstate, this initial distribution will undergo considerable modification after a fall of 1 km, the smaller drops being seriously depleted and the larger ones increased. All three processes will cause a shift in the dropโsize spectrum towards larger diameters and produce an increase in the intensity of the radar echo at lower levels of the kind which is sometimes observed. Because of this modification of the dropโsize spectrum during fall and because of the rather rapid fluctuations which are frequently observed in the distribution at the ground, it is not often possible to correlate the latter with the intensity of the radar echo located higher up.
๐ SIMILAR VOLUMES
## Abstract The photoelectric raindropโsize spectrometer has made possible the resolution of dropโsize spectra in natural rains to 1โmin intervals of time. Characteristics of the dropโsize spectra thus obtained and their timeโsequences are discussed. Various factors affecting the development of rai
This paper presents a model that simulates the size distribution and erosivity of raindrops and throughfall drops. It utilizes existing models of rainfall drop size distribution and fall velocity and combines them with newly collated evidence of throughfall drop size distributions. A sensitivity ana