YaBeSH Engineering and Technology Library

    • Journals
    • PaperQuest
    • YSE Standards
    • YaBeSH
    • Login
    View Item 
    •   YE&T Library
    • AMS
    • Journal of Applied Meteorology
    • View Item
    •   YE&T Library
    • AMS
    • Journal of Applied Meteorology
    • View Item
    • All Fields
    • Source Title
    • Year
    • Publisher
    • Title
    • Subject
    • Author
    • DOI
    • ISBN
    Advanced Search
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Archive

    An Observationally Based Conceptual Model of Warm Oceanic Convective Rain in the Tropics

    Source: Journal of Applied Meteorology:;2000:;volume( 039 ):;issue: 012::page 2165
    Author:
    Atlas, David
    ,
    Ulbrich, Carlton W.
    DOI: 10.1175/1520-0450(2001)040<2165:AOBCMO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Distinctively different Z?R relations for initial convective and transition rain at the surface were found during the Tropical Ocean and Global Atmosphere Coupled Ocean?Atmosphere Response Experiment. Initial convective rain (of 20?30-min duration) is marked by nearly constant median volume diameter of Do ≈ 2 mm and narrow drop size spectra, while R rises to >50 mm h?1. The constant form of the drop spectra independent of rain rate indicates an equilibrium distribution that accounts for the near linearity between Z and R. The form of the distribution differs from those previously reported, however. In contrast, the airborne raindrop measurements at 3 km in climatologically similar conditions show size spectra closely resembling the equilibrium collision?coalescence?breakup spectra of Hu and Srivastava and others at R > 20 mm h?1. The center of the plateau (of near-constant size) of these spectra repeatedly occurs at a drop size of 1 ± 0.1 mm whose fall speed equals the updraft speed. This suggests a mechanism in which the updraft decreases the rate of fall of the drops relative to the surface, thus extending the residence time for collisions and reducing the depth of fall required for equilibrium to be reached. At the same time the updraft separates the large fast-falling drops from the smaller ones. The large ones fall within the convergent core of the convective cell to form the narrow equilibrium drop spectra observed at the surface, while the small ones rise into the divergent air above the updraft maximum and fall out elsewhere if they survive. Also, the updrafts in warm tropical convective clouds that produce R > 20 mm h?1 are commonly 4?5 m s?1, the speeds necessary to support the 0.5?1.5-mm-diameter range of drop sizes at which the collision rate is maximized. The warm convective clouds of the western tropical Pacific Ocean appear to be well tuned to this process. The implications for radar measurements of rainfall are also treated.
    • Download: (402.8Kb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Statistics

      An Observationally Based Conceptual Model of Warm Oceanic Convective Rain in the Tropics

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4148507
    Collections
    • Journal of Applied Meteorology

    Show full item record

    contributor authorAtlas, David
    contributor authorUlbrich, Carlton W.
    date accessioned2017-06-09T14:08:11Z
    date available2017-06-09T14:08:11Z
    date copyright2000/12/01
    date issued2000
    identifier issn0894-8763
    identifier otherams-13095.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148507
    description abstractDistinctively different Z?R relations for initial convective and transition rain at the surface were found during the Tropical Ocean and Global Atmosphere Coupled Ocean?Atmosphere Response Experiment. Initial convective rain (of 20?30-min duration) is marked by nearly constant median volume diameter of Do ≈ 2 mm and narrow drop size spectra, while R rises to >50 mm h?1. The constant form of the drop spectra independent of rain rate indicates an equilibrium distribution that accounts for the near linearity between Z and R. The form of the distribution differs from those previously reported, however. In contrast, the airborne raindrop measurements at 3 km in climatologically similar conditions show size spectra closely resembling the equilibrium collision?coalescence?breakup spectra of Hu and Srivastava and others at R > 20 mm h?1. The center of the plateau (of near-constant size) of these spectra repeatedly occurs at a drop size of 1 ± 0.1 mm whose fall speed equals the updraft speed. This suggests a mechanism in which the updraft decreases the rate of fall of the drops relative to the surface, thus extending the residence time for collisions and reducing the depth of fall required for equilibrium to be reached. At the same time the updraft separates the large fast-falling drops from the smaller ones. The large ones fall within the convergent core of the convective cell to form the narrow equilibrium drop spectra observed at the surface, while the small ones rise into the divergent air above the updraft maximum and fall out elsewhere if they survive. Also, the updrafts in warm tropical convective clouds that produce R > 20 mm h?1 are commonly 4?5 m s?1, the speeds necessary to support the 0.5?1.5-mm-diameter range of drop sizes at which the collision rate is maximized. The warm convective clouds of the western tropical Pacific Ocean appear to be well tuned to this process. The implications for radar measurements of rainfall are also treated.
    publisherAmerican Meteorological Society
    titleAn Observationally Based Conceptual Model of Warm Oceanic Convective Rain in the Tropics
    typeJournal Paper
    journal volume39
    journal issue12
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(2001)040<2165:AOBCMO>2.0.CO;2
    journal fristpage2165
    journal lastpage2181
    treeJournal of Applied Meteorology:;2000:;volume( 039 ):;issue: 012
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian