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Woodcock, A. H.; Mordy, W. A. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
The discovery of large sea-salt particles 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
  • The results below are discovered through our pilot algorithms. Let us know how we are doing!

    • (C) Fig. 3 . Pseudo-adiabatic chart of Honolulu radiosonde record ( I sooZ, 26 February 1952) illustrating derivation of the cloud-base-to-inversion distances and thc instability areas shown on table I , coluinns 5 and 13. The circled X marks a tempcrature and prrssure observed on the same day from aircraft over the windward sea.
    • Telluc \'I1 (1933). 3 ANON,1950: Physical basis for the production of rain in Hawaii (A statement by members of the forecast staff, U.S. Weather Bureau, Honolulu, Hawaii).
    • BOWENE,. G., 1950: The formation of rain by coalescence. Ausfr. J . Sci. Res., A, 3, 193-213.
    • HALSTEADM,. H., and LEOPOLDL,. B., 1948: Monthly median rainfall maps. Meteorology Dept., Pineapple Research Institute and Experiment Station, Hawaiian Sugar Planters Association, Honolulu, Hawaii, Report No. 2.
    • KEITH,C. H., and ARONSA,. B., 1954: The growth of sea-salt particles by condensation of atmospheric water vapor. Joirr. Met., 11, 173-184.
    • LANGMUI RIR,VING1,948: The production of rain by chain reaction in cumulus clouds at temperatures above freezing. J . Meteor., 5 , 175-192.
    • LEOPOLDL, UNAB., 1948: Diurnal weather patterns on Oahu and Lanai, Hawaii. Pacific Science, 2, 81-95.
    • LUDLAMF., H., 1951: The production of showers by the coalescence of cloud droplets. Qirart. /. r. mefeor. Soc., 77, 402-417, MALKUSJ O,ANNESTARRa,nd SCORERR,. S., 1955: The erosion of cumulus towers. J . ttiefeor., 12. 43-57.
    • 1951: The northeast trade of the Pacific Ocean.
    • Quart. J . r. meteor. SOL.,7 7 , 598-626.
    • RIEHL,HERBERT1,947: Diurnal variation of cloudiness over the subtropical Atlantic Ocean. Birll. 24mer. .Wcf.
    • SOC.2,8, 37-40.
    • SOLOT,SAMUELB., 1950: Further studies in Hawaiian precipitation. Research paper No. 32, Weather Bureau, U.S. Department of Commerce, Washington, D.C.
    • STIDD,C. K., 1954 a: Objective Hawaiian rainfall cstimates from mean 700 m b charts. T o be published.
    • - 1954 b: Personal communication.
    • WOODCOCKA,. H., and GIFFORD,MARYM., 1949: Sampling atmospheric sea-salt nuclei over the ocean.
    • J . Marine Res., 8 , 177-197.
    • WOODCOCAK.H,., 1952: Atmospheric salt particles and raindrops. J . Meteor., 9, ZOO---ZIZ.
    • - 1953: Salt nuclei in marine air as a function of altitude and wind force. J . Meteor., 10, 362-371.
    • YEH, T. C., WALLBNC,. C., and CARSONJ,. E., 1951: A study of rainfall over Oahu. Meteorological Mono.
    • graphs, Vol. I , No. 3, 34---46, Amer. Met. Soc., Boston 8, Massachusetts.
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  • No similar publications.

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