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    Numerical Weather Prediction in New Zealand

    Source: Monthly Weather Review:;1977:;volume( 105 ):;issue: 007::page 817
    Author:
    Trenberth, Kevin E.
    ,
    Neale, Alex A.
    DOI: 10.1175/1520-0493(1977)105<0817:NWPINZ>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The main problem in weather forecasting over New Zealand and the Southern Oceans is the lack of sufficient data for good analyses, especially at upper levels. Numerical weather prediction also suffers from this problem, but it can to some degree be alleviated by producing several prognoses from reasonable alternative analyses to alert the forecaster to the sensitivity of the situation to data-blank areas. This procedure allows forecasters to assess the degree of confidence that can be placed in a forecast since unresolvable problems in the initial analyses cause uncertainty in predicting the exact timing and areas that will be affected by short-wave disturbances. It also gives them greater flexibility when later information becomes available and clearly invalidates one of the forecasts. The performance of a five-layer quasi-geostrophic model developed for this purpose in New Zealand is described and illustrated with one case study of an unusual summer situation in the Australia?New Zealand region where a decaying tropical cyclone is absorbed into the frontal system of an extratropical cyclone undergoing explosive cyclogenesis.
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      Numerical Weather Prediction in New Zealand

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4199661
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    contributor authorTrenberth, Kevin E.
    contributor authorNeale, Alex A.
    date accessioned2017-06-09T16:01:39Z
    date available2017-06-09T16:01:39Z
    date copyright1977/07/01
    date issued1977
    identifier issn0027-0644
    identifier otherams-59136.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4199661
    description abstractThe main problem in weather forecasting over New Zealand and the Southern Oceans is the lack of sufficient data for good analyses, especially at upper levels. Numerical weather prediction also suffers from this problem, but it can to some degree be alleviated by producing several prognoses from reasonable alternative analyses to alert the forecaster to the sensitivity of the situation to data-blank areas. This procedure allows forecasters to assess the degree of confidence that can be placed in a forecast since unresolvable problems in the initial analyses cause uncertainty in predicting the exact timing and areas that will be affected by short-wave disturbances. It also gives them greater flexibility when later information becomes available and clearly invalidates one of the forecasts. The performance of a five-layer quasi-geostrophic model developed for this purpose in New Zealand is described and illustrated with one case study of an unusual summer situation in the Australia?New Zealand region where a decaying tropical cyclone is absorbed into the frontal system of an extratropical cyclone undergoing explosive cyclogenesis.
    publisherAmerican Meteorological Society
    titleNumerical Weather Prediction in New Zealand
    typeJournal Paper
    journal volume105
    journal issue7
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1977)105<0817:NWPINZ>2.0.CO;2
    journal fristpage817
    journal lastpage825
    treeMonthly Weather Review:;1977:;volume( 105 ):;issue: 007
    contenttypeFulltext
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