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    Comparison of 10-m Wind Forecasts from a Regional Area Model and QuikSCAT Scatterometer Wind Observations over the Mediterranean Sea

    Source: Monthly Weather Review:;2007:;volume( 135 ):;issue: 005::page 1945
    Author:
    Accadia, Christophe
    ,
    Zecchetto, Stefano
    ,
    Lavagnini, Alfredo
    ,
    Speranza, Antonio
    DOI: 10.1175/MWR3370.1
    Publisher: American Meteorological Society
    Abstract: Surface wind forecasts from a limited-area model [the Quadrics Bologna Limited-Area Model (QBOLAM)] covering the entire Mediterranean area at 0.1° grid spacing are verified against Quick Scatterometer (QuikSCAT) wind observations. Only forecasts within the first 24 h in coincidence with satellite overpasses are used. Two years of data, from 1 October 2000 to 31 October 2002, have been considered, allowing for an adequate statistical assessment under different wind conditions. This has been carried out by analyzing the fields of the mean wind vectors, wind speed bias, correlation, difference standard deviation, steadiness, gustiness, and mean wind direction difference, in order to investigate spatial variability. Statistics have been computed on a seasonal basis. A comparison of satellite and forecast winds with measurements from three buoys was also performed. Some critical areas of the Mediterranean Sea where wind forecast quality is lower than average have been identified. Such areas correspond to semienclosed basins surrounded by important orography and to small regions at the lee side of the main islands. In open-sea regions the model underestimates wind strength from about 0.5 m s?1 in spring and summer to 1.0 m s?1 in winter, as evidenced by the existing biases against scatterometer data. Also, a wind direction bias (scatterometer minus model) generally between 5° and 15° exists. A survey of the identified and likely sources of forecast error is performed, indicating that orography representation plays an important role. Numerical damping is identified as a likely factor reducing forecast wind strength. The need for a correction scheme is envisaged to provide more accurate forcing for numerical sea state forecasting models, wind energy evaluation, and latent and/or sensible heat exchanges.
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      Comparison of 10-m Wind Forecasts from a Regional Area Model and QuikSCAT Scatterometer Wind Observations over the Mediterranean Sea

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4229416
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    • Monthly Weather Review

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    contributor authorAccadia, Christophe
    contributor authorZecchetto, Stefano
    contributor authorLavagnini, Alfredo
    contributor authorSperanza, Antonio
    date accessioned2017-06-09T17:28:27Z
    date available2017-06-09T17:28:27Z
    date copyright2007/05/01
    date issued2007
    identifier issn0027-0644
    identifier otherams-85916.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4229416
    description abstractSurface wind forecasts from a limited-area model [the Quadrics Bologna Limited-Area Model (QBOLAM)] covering the entire Mediterranean area at 0.1° grid spacing are verified against Quick Scatterometer (QuikSCAT) wind observations. Only forecasts within the first 24 h in coincidence with satellite overpasses are used. Two years of data, from 1 October 2000 to 31 October 2002, have been considered, allowing for an adequate statistical assessment under different wind conditions. This has been carried out by analyzing the fields of the mean wind vectors, wind speed bias, correlation, difference standard deviation, steadiness, gustiness, and mean wind direction difference, in order to investigate spatial variability. Statistics have been computed on a seasonal basis. A comparison of satellite and forecast winds with measurements from three buoys was also performed. Some critical areas of the Mediterranean Sea where wind forecast quality is lower than average have been identified. Such areas correspond to semienclosed basins surrounded by important orography and to small regions at the lee side of the main islands. In open-sea regions the model underestimates wind strength from about 0.5 m s?1 in spring and summer to 1.0 m s?1 in winter, as evidenced by the existing biases against scatterometer data. Also, a wind direction bias (scatterometer minus model) generally between 5° and 15° exists. A survey of the identified and likely sources of forecast error is performed, indicating that orography representation plays an important role. Numerical damping is identified as a likely factor reducing forecast wind strength. The need for a correction scheme is envisaged to provide more accurate forcing for numerical sea state forecasting models, wind energy evaluation, and latent and/or sensible heat exchanges.
    publisherAmerican Meteorological Society
    titleComparison of 10-m Wind Forecasts from a Regional Area Model and QuikSCAT Scatterometer Wind Observations over the Mediterranean Sea
    typeJournal Paper
    journal volume135
    journal issue5
    journal titleMonthly Weather Review
    identifier doi10.1175/MWR3370.1
    journal fristpage1945
    journal lastpage1960
    treeMonthly Weather Review:;2007:;volume( 135 ):;issue: 005
    contenttypeFulltext
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