1943
DOI: 10.1029/tr024i002p00452
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The relation of raindrop‐size to intensity

Abstract: Curiosity concerning the drop‐size composition of natural rain has arisen from attempts to measure erodibility and infiltration‐capacity by sprinkling small areas of land with artificial rain. The results have been found to be affected by the drop‐size and velocity of the artificial rains applied, and the applicability of such results to conditions of natural rainfall has been thrown in doubt.

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Cited by 789 publications
(397 citation statements)
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“…The flour method of Laws and Parsons (1943) as adapted by Kohl (1974) was used to obtain the independent droplet data set for comparison purposes. Measured droplet sizes ranged from 0.33 to 5.95 mm in 0.08-mm increments for the smallest droplets to a 1.01-mm increment at the upper end of the measurement range.…”
Section: Droplet Size Measurementsmentioning
confidence: 99%
“…The flour method of Laws and Parsons (1943) as adapted by Kohl (1974) was used to obtain the independent droplet data set for comparison purposes. Measured droplet sizes ranged from 0.33 to 5.95 mm in 0.08-mm increments for the smallest droplets to a 1.01-mm increment at the upper end of the measurement range.…”
Section: Droplet Size Measurementsmentioning
confidence: 99%
“…This attenuation depends on the dropsize of rain or snow. The most commonly used raindrop size distributions that have been proposed by Marshal and Palmer [22]. Rain or snow does not influence optical transmissions heavily, because they have the size of a few millimeters and are relatively large compared to laser wavelengths (1.5 microns) and thus cause minimal scattering of the laser energy.…”
Section: Atmospheric Losses and Weather Influencesmentioning
confidence: 99%
“…The modeling of the DSD varies from one climate to another. Drop size distribution modeling in temperate region; characterized by moderate rainfall is well suitable with models such as proposed by Marshall and Palmer [3], Laws and Parsons [4] and the negative exponential model of gamma [5].The modeling of DSD in the tropical region is most suitable with the globally accepted Ajayi and Olsen [6] lognormal model. In Durban, South Africa, a reasonable number of works have been carried out on rainfall attenuation and DSD [7][8][9][10][11][12] establishing the suitability of the lognormal and gamma models for DSD modeling in the region.…”
mentioning
confidence: 99%
“…The modeling of the DSD varies from one climate to another. Drop size distribution modeling in temperate region; characterized by moderate rainfall is well suitable with models such as proposed by Marshall and Palmer [3], Laws and Parsons [4] and the negative exponential model of gamma [5].…”
Section: Introductionmentioning
confidence: 99%