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    Comparisons of Results from a Three-Dimensional Cloud Model with Statistics of Radar Echoes on Day 261 of GATE

    Source: Monthly Weather Review:;1981:;volume( 109 ):;issue: 007::page 1495
    Author:
    Turpeinen, Olli
    ,
    Yau, Man Kong
    DOI: 10.1175/1520-0493(1981)109<1495:CORFAT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: An analysis of 5 min resolution Quadra data on day 261 of GATE, (0953?1451 GMT) is made to yield statistics of maximum area, echo top, lifetime and maximum reflectivity factor in medium-sized convective cells. The results, obtained by tracking 140 echoes throughout their lifetime, indicate that the maximum area is log-normally distributed, 90% of the echoes being smaller than 40 km2 and existing less than 60 min. The modes of the maximum echo top and maximum reflectivity factor distributions are around 2.5 km and 30 dBZ, respectively. Further stratification of the data according to minimum edge to edge separation (d) reveals that merging cells (d = 0) have an average lifetime three times longer and a maximum area five times larger than isolated ones (d > 7 km). For a fixed maximum area, however, echo parameters generally decrease with decreasing d. A fully three-dimensional cloud model including precipitation processes is used to simulate the development of an isolated and two adjacent cells. Comparison of modeled and observed echo parameters indicates a fair degree of realism in the simulations. The computed maximum reflectivity factor, however, is considerably higher than that of the observations because of the unrealistic drop-size distribution assumed in the model. Results of two cloud simulations suggest that the alignment of the clouds in relation to the wind-shear vector is an important factor in addition to d in determining the intensity of cloud development. The upshear cell of the parallel clouds, even with a small d value, behaves similarly to an isolated one. The suppression experienced by adjacent cells is attributed to the reduced low-level moisture convergence.
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      Comparisons of Results from a Three-Dimensional Cloud Model with Statistics of Radar Echoes on Day 261 of GATE

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4200530
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    contributor authorTurpeinen, Olli
    contributor authorYau, Man Kong
    date accessioned2017-06-09T16:03:30Z
    date available2017-06-09T16:03:30Z
    date copyright1981/07/01
    date issued1981
    identifier issn0027-0644
    identifier otherams-59919.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4200530
    description abstractAn analysis of 5 min resolution Quadra data on day 261 of GATE, (0953?1451 GMT) is made to yield statistics of maximum area, echo top, lifetime and maximum reflectivity factor in medium-sized convective cells. The results, obtained by tracking 140 echoes throughout their lifetime, indicate that the maximum area is log-normally distributed, 90% of the echoes being smaller than 40 km2 and existing less than 60 min. The modes of the maximum echo top and maximum reflectivity factor distributions are around 2.5 km and 30 dBZ, respectively. Further stratification of the data according to minimum edge to edge separation (d) reveals that merging cells (d = 0) have an average lifetime three times longer and a maximum area five times larger than isolated ones (d > 7 km). For a fixed maximum area, however, echo parameters generally decrease with decreasing d. A fully three-dimensional cloud model including precipitation processes is used to simulate the development of an isolated and two adjacent cells. Comparison of modeled and observed echo parameters indicates a fair degree of realism in the simulations. The computed maximum reflectivity factor, however, is considerably higher than that of the observations because of the unrealistic drop-size distribution assumed in the model. Results of two cloud simulations suggest that the alignment of the clouds in relation to the wind-shear vector is an important factor in addition to d in determining the intensity of cloud development. The upshear cell of the parallel clouds, even with a small d value, behaves similarly to an isolated one. The suppression experienced by adjacent cells is attributed to the reduced low-level moisture convergence.
    publisherAmerican Meteorological Society
    titleComparisons of Results from a Three-Dimensional Cloud Model with Statistics of Radar Echoes on Day 261 of GATE
    typeJournal Paper
    journal volume109
    journal issue7
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1981)109<1495:CORFAT>2.0.CO;2
    journal fristpage1495
    journal lastpage1511
    treeMonthly Weather Review:;1981:;volume( 109 ):;issue: 007
    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
    yabeshDSpacePersian