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    EXPERIMENTS IN NUMERICAL OBJECTIVE FRONTAL ANALYSIS

    Source: Monthly Weather Review:;1965:;volume( 093 ):;issue: 009::page 547
    Author:
    RENARD, ROBERT J.
    ,
    CLARKE, LEO C.
    DOI: 10.1175/1520-0493(1965)093<0547:EINOFA>2.3.CO;2
    Publisher: American Meteorological Society
    Abstract: A major area of weather analysis still requiring manual subjective determination is that of locating fronts. The experiments reported on here concern an attempt to incorporate objective frontal analysis into the operational computer routines of the U.S. Navy Fleet Numerical Weather Facility, Monterey, Calif. The synoptically-important numerically-derived frontal zone is regarded as a hyperbaroclinic region whose boundaries may be defined as quasi first-order thermal and moisture discontinuities; the boundaries are located through use of suitably defined second derivatives of various potential temperature parameters. Application is made to 850-mb. and surface (or 1000-mb.) frontal analyses on a hemispheric basis. The analyses for 0000 and 1200 gmt January 1, 1965 are selected to exemplify results of the most promising of the experiments. Verification against hand-derived frontal analyses, difficulties with the existing scheme, and proposed modifications to the continuing program are discussed.
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      EXPERIMENTS IN NUMERICAL OBJECTIVE FRONTAL ANALYSIS

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4198006
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    contributor authorRENARD, ROBERT J.
    contributor authorCLARKE, LEO C.
    date accessioned2017-06-09T15:57:55Z
    date available2017-06-09T15:57:55Z
    date copyright1965/09/01
    date issued1965
    identifier issn0027-0644
    identifier otherams-57647.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198006
    description abstractA major area of weather analysis still requiring manual subjective determination is that of locating fronts. The experiments reported on here concern an attempt to incorporate objective frontal analysis into the operational computer routines of the U.S. Navy Fleet Numerical Weather Facility, Monterey, Calif. The synoptically-important numerically-derived frontal zone is regarded as a hyperbaroclinic region whose boundaries may be defined as quasi first-order thermal and moisture discontinuities; the boundaries are located through use of suitably defined second derivatives of various potential temperature parameters. Application is made to 850-mb. and surface (or 1000-mb.) frontal analyses on a hemispheric basis. The analyses for 0000 and 1200 gmt January 1, 1965 are selected to exemplify results of the most promising of the experiments. Verification against hand-derived frontal analyses, difficulties with the existing scheme, and proposed modifications to the continuing program are discussed.
    publisherAmerican Meteorological Society
    titleEXPERIMENTS IN NUMERICAL OBJECTIVE FRONTAL ANALYSIS
    typeJournal Paper
    journal volume93
    journal issue9
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1965)093<0547:EINOFA>2.3.CO;2
    journal fristpage547
    journal lastpage556
    treeMonthly Weather Review:;1965:;volume( 093 ):;issue: 009
    contenttypeFulltext
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