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    Evaluation by Monte Carlo Tests of Effects of Cloud Seeding on Growing Season Rainfall in North Dakota

    Source: Journal of Applied Meteorology:;1975:;volume( 014 ):;issue: 005::page 959
    Author:
    Dennis, A. S.
    ,
    Miller, J. R.
    ,
    Cain, D. E.
    ,
    Schwaller, R. L.
    DOI: 10.1175/1520-0450(1975)014<0959:EBMCTO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Rainfall data collected at 67 gages in a 2750 mi2 target area during a four-year randomized cloud seeding experiment in North Dakota have been stratified in a variety of ways and subjected to several kinds of statistical tests. Some stratifications related to cloud model predictions were possible for only the last two years when a rawinsonde station was operated as part of the project. Monte Carlo experiments simulating 500 reruns of the four-year experiment have been used to establish significance levels for the tests within each data stratification. The analysis provides significant evidence that seeding convective clouds on a determinate set of days leads to 1) an increase in the frequency of rainfall events at the individual target gages, 2) an increase in the average rainfall recorded per rainfall event, and 3) an increase in total rainfall on the target. The set of days to which this evidence applies is those days with dynamic seedability; that is, days for which a cloud model predicted an increase in cloud top height under the influence of silver iodide seeding. Rainfall observations on days when the cloud model predicted no increase in cloud height show no significant differences between seed and no-seed days. The possibility of bias has been checked by comparing the frequencies of wet and dry days and the averages of several meteorological variables for seed and no-seed days within each stratification, by cross-checking the stratifications, and by comparing rainfall on seed and no-seed days over an area of roughly 50,000 square miles surrounding the target area. There is no obvious bias to account for the significant differences between seed and no-seed days with dynamic seedability. It is tentatively concluded that dynamic effects, including rainfall increases, were produced by light to moderate silver iodide seeding from below cloud base. The potential rainfall increase resulting from seeding below selected clouds on days with dynamic seedability is estimated at one inch per growing season.
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      Evaluation by Monte Carlo Tests of Effects of Cloud Seeding on Growing Season Rainfall in North Dakota

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4232353
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    • Journal of Applied Meteorology

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    contributor authorDennis, A. S.
    contributor authorMiller, J. R.
    contributor authorCain, D. E.
    contributor authorSchwaller, R. L.
    date accessioned2017-06-09T17:38:17Z
    date available2017-06-09T17:38:17Z
    date copyright1975/08/01
    date issued1975
    identifier issn0021-8952
    identifier otherams-8922.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232353
    description abstractRainfall data collected at 67 gages in a 2750 mi2 target area during a four-year randomized cloud seeding experiment in North Dakota have been stratified in a variety of ways and subjected to several kinds of statistical tests. Some stratifications related to cloud model predictions were possible for only the last two years when a rawinsonde station was operated as part of the project. Monte Carlo experiments simulating 500 reruns of the four-year experiment have been used to establish significance levels for the tests within each data stratification. The analysis provides significant evidence that seeding convective clouds on a determinate set of days leads to 1) an increase in the frequency of rainfall events at the individual target gages, 2) an increase in the average rainfall recorded per rainfall event, and 3) an increase in total rainfall on the target. The set of days to which this evidence applies is those days with dynamic seedability; that is, days for which a cloud model predicted an increase in cloud top height under the influence of silver iodide seeding. Rainfall observations on days when the cloud model predicted no increase in cloud height show no significant differences between seed and no-seed days. The possibility of bias has been checked by comparing the frequencies of wet and dry days and the averages of several meteorological variables for seed and no-seed days within each stratification, by cross-checking the stratifications, and by comparing rainfall on seed and no-seed days over an area of roughly 50,000 square miles surrounding the target area. There is no obvious bias to account for the significant differences between seed and no-seed days with dynamic seedability. It is tentatively concluded that dynamic effects, including rainfall increases, were produced by light to moderate silver iodide seeding from below cloud base. The potential rainfall increase resulting from seeding below selected clouds on days with dynamic seedability is estimated at one inch per growing season.
    publisherAmerican Meteorological Society
    titleEvaluation by Monte Carlo Tests of Effects of Cloud Seeding on Growing Season Rainfall in North Dakota
    typeJournal Paper
    journal volume14
    journal issue5
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1975)014<0959:EBMCTO>2.0.CO;2
    journal fristpage959
    journal lastpage969
    treeJournal of Applied Meteorology:;1975:;volume( 014 ):;issue: 005
    contenttypeFulltext
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