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    Hourly Variability of Density at Radiosonde Heights

    Source: Journal of Applied Meteorology:;1964:;volume( 003 ):;issue: 002::page 175
    Author:
    Nee, Paul F.
    DOI: 10.1175/1520-0450(1964)003<0175:HVODAR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Estimates of the root mean square change in density at 1, 7, 12, 18, and 25 km are presented for lags of one through 24 hours. The lag variability at all of the heights considered increased with an increase in time. The relative magnitudes of these lag variabilities, expressed as a per cent of the observed mean at each level, show that for a given lag, the variability decreases from 1 to 7 km, increases from 7 to 12 km, and then decreases again from 12 to 25 km. The auto-correlation coefficient was derived from the lag variability and is also presented. The auto-correlation function decayed to zero at a lag of 22.6 hours at 7 km. Correlations greater than zero persisted for more than 24 hours at the other four levels. Observed diurnal variability was less than 1.2 per cent at all levels below 25 km.
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      Hourly Variability of Density at Radiosonde Heights

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    contributor authorNee, Paul F.
    date accessioned2017-06-09T16:35:47Z
    date available2017-06-09T16:35:47Z
    date copyright1964/04/01
    date issued1964
    identifier issn0021-8952
    identifier otherams-7063.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4212434
    description abstractEstimates of the root mean square change in density at 1, 7, 12, 18, and 25 km are presented for lags of one through 24 hours. The lag variability at all of the heights considered increased with an increase in time. The relative magnitudes of these lag variabilities, expressed as a per cent of the observed mean at each level, show that for a given lag, the variability decreases from 1 to 7 km, increases from 7 to 12 km, and then decreases again from 12 to 25 km. The auto-correlation coefficient was derived from the lag variability and is also presented. The auto-correlation function decayed to zero at a lag of 22.6 hours at 7 km. Correlations greater than zero persisted for more than 24 hours at the other four levels. Observed diurnal variability was less than 1.2 per cent at all levels below 25 km.
    publisherAmerican Meteorological Society
    titleHourly Variability of Density at Radiosonde Heights
    typeJournal Paper
    journal volume3
    journal issue2
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1964)003<0175:HVODAR>2.0.CO;2
    journal fristpage175
    journal lastpage178
    treeJournal of Applied Meteorology:;1964:;volume( 003 ):;issue: 002
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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