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    Characterizing the Atmospheric Conditions Leading to Large Error Growth in Volcanic Ash Cloud Forecasts

    Source: Journal of Applied Meteorology and Climatology:;2018:;volume 057:;issue 004::page 1011
    Author:
    Dacre, H. F.
    ,
    Harvey, N. J.
    DOI: 10.1175/JAMC-D-17-0298.1
    Publisher: American Meteorological Society
    Abstract: ABSTRACTVolcanic ash poses an ongoing risk to safety in the airspace worldwide. The accuracy with which volcanic ash dispersion can be forecast depends on the conditions of the atmosphere into which it is emitted. In this study, meteorological ensemble forecasts are used to drive a volcanic ash transport and dispersion model for the 2010 Eyjafjallajökull eruption in Iceland. From analysis of these simulations, the authors determine why the skill of deterministic-meteorological forecasts decreases with increasing ash residence time and identify the atmospheric conditions in which this drop in skill occurs most rapidly. Large forecast errors are more likely when ash particles encounter regions of large horizontal flow separation in the atmosphere. Nearby ash particle trajectories can rapidly diverge, leading to a reduction in the forecast accuracy of deterministic forecasts that do not represent variability in wind fields at the synoptic scale. The flow?separation diagnostic identifies where and why large ensemble spread may occur. This diagnostic can be used to alert forecasters to situations in which the ensemble mean is not representative of the individual ensemble?member volcanic ash distributions. Knowledge of potential ensemble outliers can be used to assess confidence in the forecast and to avoid potentially dangerous situations in which forecasts fail to predict harmful levels of volcanic ash.
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      Characterizing the Atmospheric Conditions Leading to Large Error Growth in Volcanic Ash Cloud Forecasts

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4261664
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    contributor authorDacre, H. F.
    contributor authorHarvey, N. J.
    date accessioned2019-09-19T10:06:47Z
    date available2019-09-19T10:06:47Z
    date copyright2/14/2018 12:00:00 AM
    date issued2018
    identifier otherjamc-d-17-0298.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4261664
    description abstractABSTRACTVolcanic ash poses an ongoing risk to safety in the airspace worldwide. The accuracy with which volcanic ash dispersion can be forecast depends on the conditions of the atmosphere into which it is emitted. In this study, meteorological ensemble forecasts are used to drive a volcanic ash transport and dispersion model for the 2010 Eyjafjallajökull eruption in Iceland. From analysis of these simulations, the authors determine why the skill of deterministic-meteorological forecasts decreases with increasing ash residence time and identify the atmospheric conditions in which this drop in skill occurs most rapidly. Large forecast errors are more likely when ash particles encounter regions of large horizontal flow separation in the atmosphere. Nearby ash particle trajectories can rapidly diverge, leading to a reduction in the forecast accuracy of deterministic forecasts that do not represent variability in wind fields at the synoptic scale. The flow?separation diagnostic identifies where and why large ensemble spread may occur. This diagnostic can be used to alert forecasters to situations in which the ensemble mean is not representative of the individual ensemble?member volcanic ash distributions. Knowledge of potential ensemble outliers can be used to assess confidence in the forecast and to avoid potentially dangerous situations in which forecasts fail to predict harmful levels of volcanic ash.
    publisherAmerican Meteorological Society
    titleCharacterizing the Atmospheric Conditions Leading to Large Error Growth in Volcanic Ash Cloud Forecasts
    typeJournal Paper
    journal volume57
    journal issue4
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/JAMC-D-17-0298.1
    journal fristpage1011
    journal lastpage1019
    treeJournal of Applied Meteorology and Climatology:;2018:;volume 057:;issue 004
    contenttypeFulltext
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