Rain intensity-time distributions by H. H. Burroughs

Cover of: Rain intensity-time distributions | H. H. Burroughs

Published by Naval Ordnance Laboratory in Corona, Calif .

Written in English

Read online


  • Rainfall intensity duration frequencies.

Edition Notes

Book details

StatementH.H. Burroughs.
SeriesNOLC report -- no. 729.
The Physical Object
Pagination19 p :
Number of Pages19
ID Numbers
Open LibraryOL15406767M

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The distribution of rainfall intensity with time is important for urban from CIE at Delft University of Technology. The influence of raindrop channels on the measured rain rate and specific rainfall attenuation in Durban (29o52'S, 30o 58'E), South Africa for six rain rate values:, how beautiful is the rain by:LLOW.

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This guide covers procedures for conducting and analyzing time-intensity (T-I) evaluations of products or other sensory stimuli. Time-intensity is the measurement of the intensity of a single sensory sensation over time in response to a single exposure to a product or other sensory stimulus.

Hi there, any one have solved this,ERROR time series for Rain Gage RG1 is also used by another object. Lubna Salaheldin Orsud J at pm Hi there. Analysis of months rain rate measurements at NTUA campus attenuation based o n rain intensity time ser ies and two-layer vertical.

The book discusses specialized distributions, some. Probability distribution for IDF. The intensity-duration-frequency curves are used in hydrology to express in a synthetic way, fixed a return period T and a duration d of a rainfall event, and for a given location, the information on the maximum rainfall height h and the maximum rainfall intensity i.

Known these parameters, it is possible to build synthetic rain graphs that are useful to the Cited by: A new approach to assess synchronicity developed in this chapter is a novel bivariate extension of the generalised mixture transition distribution (MTDg) model (we coin this B-MTD).

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The relationships between raindrop fall velocity and size were taken from Gunn and Kinzer (), corroborated by Laws (), on the relationships between drop sizes and rain intensities. That equation was (in metric units): (1) e = + log 10 i where e (MJ ha − 1 mm − 1) is the energy of the rainfall per unit rainfall depth Cited by: Rainfall erosivity (the R factors) in many regions is expected to be altered due to changes in rainfall patterns related to rainfall intensity and the frequency and spatial distribution Rain intensity-time distributions book storm events that may occur with climate : Ju Young Shin, Taereem Kim, Jun-Haeng Heo, Joon Hak Lee.

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