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Salt nuclei, wind and daily rainfall in Hawaii

Abstract

The discovery of large sea-salt particulates at cloud levels led to the hypothesis that these particles act as nuclei on which raindrops initially form within clouds and to the suggestion that the amount of rainfall on an oceanic island might be a function of the number of the salt particles in the air. Exploratory observations of rain and airborne salt in Hawaii, which were intended to test this suggestion, are presented and discussed. These observations do not prove that greater numbers of salt nuclei are related to greater amounts of rain. They do, however, indicate that such a relationship may exist, and that additional field studies should be made which utilize the pertinent results of the present study.
Publication Date:
Jan 01, 1955
Product Type:
Journal Article
Reference Number:
EDB-84-085934
Resource Relation:
Journal Name: Tellus; (Sweden); Journal Volume: 7
Subject:
54 ENVIRONMENTAL SCIENCES; AIR POLLUTION; AIR-WATER INTERACTIONS; CONDENSATION NUCLEI; SALTS; ENVIRONMENTAL TRANSPORT; ACID RAIN; DAILY VARIATIONS; FEDERAL REGION IV; HAWAII; PARTICULATES; WIND; ATMOSPHERIC PRECIPITATIONS; FEDERAL REGION IX; MASS TRANSFER; NORTH AMERICA; PARTICLES; POLLUTION; RAIN; USA; VARIATIONS; 500200* - Environment, Atmospheric- Chemicals Monitoring & Transport- (-1989)
OSTI ID:
6918466
Country of Origin:
Sweden
Language:
English
Other Identifying Numbers:
Journal ID: CODEN: TELLA
Submitting Site:
HEDB
Size:
Pages: 291-300
Announcement Date:
Aug 01, 1983

Citation Formats

Woodcock, A H, and Mordy, W A. Salt nuclei, wind and daily rainfall in Hawaii. Sweden: N. p., 1955. Web. doi:10.1111/j.2153-3490.1955.tb01165.x.
Woodcock, A H, & Mordy, W A. Salt nuclei, wind and daily rainfall in Hawaii. Sweden. https://doi.org/10.1111/j.2153-3490.1955.tb01165.x
Woodcock, A H, and Mordy, W A. 1955. "Salt nuclei, wind and daily rainfall in Hawaii." Sweden. https://doi.org/10.1111/j.2153-3490.1955.tb01165.x.
@misc{etde_6918466,
title = {Salt nuclei, wind and daily rainfall in Hawaii}
author = {Woodcock, A H, and Mordy, W A}
abstractNote = {The discovery of large sea-salt particulates at cloud levels led to the hypothesis that these particles act as nuclei on which raindrops initially form within clouds and to the suggestion that the amount of rainfall on an oceanic island might be a function of the number of the salt particles in the air. Exploratory observations of rain and airborne salt in Hawaii, which were intended to test this suggestion, are presented and discussed. These observations do not prove that greater numbers of salt nuclei are related to greater amounts of rain. They do, however, indicate that such a relationship may exist, and that additional field studies should be made which utilize the pertinent results of the present study.}
doi = {10.1111/j.2153-3490.1955.tb01165.x}
journal = []
volume = {7}
journal type = {AC}
place = {Sweden}
year = {1955}
month = {Jan}
}