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    Statistics of Radar Echoes on Day 261 of GATE

    Source: Monthly Weather Review:;1978:;volume( 106 ):;issue: 007::page 983
    Author:
    Warner, C.
    ,
    Austin, G. L.
    DOI: 10.1175/1520-0493(1978)106<0983:SOREOD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Statistics of echoes observed on day 261 of GATE, using the radar aboard the Canadian ship Quadra, are described. This is a case in which detailed observations have been obtained from many sensors during the growth of a cloud cluster. Dividing the radar field of view into many ?bins,? it was found that rainfall rates and echo top heights were log-normally distributed UP to a certain limit, with a few additional high values. After identifying echo cores, bounded by a reflectivity threshold 24 dB above 1 mm6 m?3, their area were found to be distributed in a similar manner. Upper limits of log-normality before (and during) the growth of the cluster were about 5 (and 30) mm h?1 for rainfall rate, 7 (and 7) km for echo top height (at the 29 dB level of intensity) and 100 (and 400) km2 for area (within contours of intensity 24 dBZ). To echoes organized on a length scale of about 100 km for more, one attributes maximum rainfall rates reaching roughly 50 mm h?1, peak heights reaching 14 km, and maximum areas of elongated cores reaching 5000 km2.
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      Statistics of Radar Echoes on Day 261 of GATE

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4199879
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    • Monthly Weather Review

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    contributor authorWarner, C.
    contributor authorAustin, G. L.
    date accessioned2017-06-09T16:02:07Z
    date available2017-06-09T16:02:07Z
    date copyright1978/07/01
    date issued1978
    identifier issn0027-0644
    identifier otherams-59332.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4199879
    description abstractStatistics of echoes observed on day 261 of GATE, using the radar aboard the Canadian ship Quadra, are described. This is a case in which detailed observations have been obtained from many sensors during the growth of a cloud cluster. Dividing the radar field of view into many ?bins,? it was found that rainfall rates and echo top heights were log-normally distributed UP to a certain limit, with a few additional high values. After identifying echo cores, bounded by a reflectivity threshold 24 dB above 1 mm6 m?3, their area were found to be distributed in a similar manner. Upper limits of log-normality before (and during) the growth of the cluster were about 5 (and 30) mm h?1 for rainfall rate, 7 (and 7) km for echo top height (at the 29 dB level of intensity) and 100 (and 400) km2 for area (within contours of intensity 24 dBZ). To echoes organized on a length scale of about 100 km for more, one attributes maximum rainfall rates reaching roughly 50 mm h?1, peak heights reaching 14 km, and maximum areas of elongated cores reaching 5000 km2.
    publisherAmerican Meteorological Society
    titleStatistics of Radar Echoes on Day 261 of GATE
    typeJournal Paper
    journal volume106
    journal issue7
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1978)106<0983:SOREOD>2.0.CO;2
    journal fristpage983
    journal lastpage994
    treeMonthly Weather Review:;1978:;volume( 106 ):;issue: 007
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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