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    Simulation of Extreme New Zealand Precipitation Events. Part I: Sensitivity to Orography and Resolution

    Source: Monthly Weather Review:;1995:;volume( 123 ):;issue: 003::page 737
    Author:
    Katzfey, Jack J.
    DOI: 10.1175/1520-0493(1995)123<0737:SOENZP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The extreme precipitation events with peak observed rainfall of greater than 700 mm over the South Island of New Zealand were simulated using the DAR hydrostatic mesoscale model nested within the ECMWF analyses. The ECMWF analyses for two of the events showed a low-level jet with mixing ratios greater than 12 g kg?1 crossing the South Island of New Zealand during the heavy precipitation near a cold front. The third case, which had smaller mixing ratios, occurred as a low-level jet and crossed the South Island while a low redeveloped downstream. Three different orographies were used with the 30-km horizontal resolution model runs, with progressively increased terrain heights. The highest orography was created by artificially inserting the effective barrier of the Southern Alps to northwesterly flow in the model grid. Orography had a strong influence on the amount of precipitation: the peak precipitation was related to orographic slope while the area-averaged precipitation was related to the maximum orographic elevation. The model successfully simulated nearly half the peak observed precipitation and over half the area-averaged precipitation (determined by hydrological means) in two of the cases and much less in the third case. Refining the horizontal resolution from 30 to 15 km also increased the peak precipitation amounts. However, the area-averaged precipitation in the 15-km runs was not significantly larger than in the 30-km runs, suggesting more concentrated precipitation over a smaller area. All simulations, except the artificial barrier orography case, produced a mountain wave consistent with linear theory, in spite of the nonsteady flow, irregular orography, and the large amount of diabatic heating present. The amplitude of the mountain wave increased with mountain height and resolution. The absence of a mountain wave in the run with the artificial barrier orography indicates unrealistic flow for that configuration.
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      Simulation of Extreme New Zealand Precipitation Events. Part I: Sensitivity to Orography and Resolution

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4203449
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    • Monthly Weather Review

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    contributor authorKatzfey, Jack J.
    date accessioned2017-06-09T16:10:20Z
    date available2017-06-09T16:10:20Z
    date copyright1995/03/01
    date issued1995
    identifier issn0027-0644
    identifier otherams-62545.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4203449
    description abstractThe extreme precipitation events with peak observed rainfall of greater than 700 mm over the South Island of New Zealand were simulated using the DAR hydrostatic mesoscale model nested within the ECMWF analyses. The ECMWF analyses for two of the events showed a low-level jet with mixing ratios greater than 12 g kg?1 crossing the South Island of New Zealand during the heavy precipitation near a cold front. The third case, which had smaller mixing ratios, occurred as a low-level jet and crossed the South Island while a low redeveloped downstream. Three different orographies were used with the 30-km horizontal resolution model runs, with progressively increased terrain heights. The highest orography was created by artificially inserting the effective barrier of the Southern Alps to northwesterly flow in the model grid. Orography had a strong influence on the amount of precipitation: the peak precipitation was related to orographic slope while the area-averaged precipitation was related to the maximum orographic elevation. The model successfully simulated nearly half the peak observed precipitation and over half the area-averaged precipitation (determined by hydrological means) in two of the cases and much less in the third case. Refining the horizontal resolution from 30 to 15 km also increased the peak precipitation amounts. However, the area-averaged precipitation in the 15-km runs was not significantly larger than in the 30-km runs, suggesting more concentrated precipitation over a smaller area. All simulations, except the artificial barrier orography case, produced a mountain wave consistent with linear theory, in spite of the nonsteady flow, irregular orography, and the large amount of diabatic heating present. The amplitude of the mountain wave increased with mountain height and resolution. The absence of a mountain wave in the run with the artificial barrier orography indicates unrealistic flow for that configuration.
    publisherAmerican Meteorological Society
    titleSimulation of Extreme New Zealand Precipitation Events. Part I: Sensitivity to Orography and Resolution
    typeJournal Paper
    journal volume123
    journal issue3
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1995)123<0737:SOENZP>2.0.CO;2
    journal fristpage737
    journal lastpage754
    treeMonthly Weather Review:;1995:;volume( 123 ):;issue: 003
    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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