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    Impact of Assimilating Ocean Velocity Observations Inferred from Lagrangian Drifter Data Using the NCOM-4DVAR

    Source: Monthly Weather Review:;2013:;volume( 142 ):;issue: 004::page 1509
    Author:
    Carrier, Matthew J.
    ,
    Ngodock, Hans
    ,
    Smith, Scott
    ,
    Jacobs, Gregg
    ,
    Muscarella, Philip
    ,
    Ozgokmen, Tamay
    ,
    Haus, Brian
    ,
    Lipphardt, Bruce
    DOI: 10.1175/MWR-D-13-00236.1
    Publisher: American Meteorological Society
    Abstract: ulerian velocity fields are derived from 300 drifters released in the Gulf of Mexico by The Consortium for Advanced Research on Transport of Hydrocarbon in the Environment (CARTHE) during the summer 2012 Grand Lagrangian Deployment (GLAD) experiment. These data are directly assimilated into the Navy Coastal Ocean Model (NCOM) four-dimensional variational data assimilation (4DVAR) analysis system in a series of experiments to investigate their impact on the model circulation. The NCOM-4DVAR is a newly developed tool for data analysis, formulated for weak-constraint data assimilation based on the indirect representer method. The assimilation experiments take advantage of this velocity data along with other available data sources from in situ and satellite measurements of surface and subsurface temperature and salinity. Three different experiments are done: (i) A nonassimilative NCOM free run, (ii) an assimilative NCOM run that utilizes temperature and salinity observations, and (iii) an assimilative NCOM run that uses temperature and salinity observations as well as the GLAD velocity observations. The resulting analyses and subsequent forecasts are compared to assimilated and future GLAD velocity and temperature/salinity observations to determine the performance of each experiment and the impact of the GLAD data on the analysis and the forecast. It is shown that the NCOM-4DVAR is able to fit the observations not only in the analysis step, but also in the subsequent forecast. It is also found that the GLAD velocity data greatly improves the characterization of the circulation, with the forecast showing a better fit to future GLAD observations than those experiments without the velocity data included.
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      Impact of Assimilating Ocean Velocity Observations Inferred from Lagrangian Drifter Data Using the NCOM-4DVAR

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4230281
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    • Monthly Weather Review

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    contributor authorCarrier, Matthew J.
    contributor authorNgodock, Hans
    contributor authorSmith, Scott
    contributor authorJacobs, Gregg
    contributor authorMuscarella, Philip
    contributor authorOzgokmen, Tamay
    contributor authorHaus, Brian
    contributor authorLipphardt, Bruce
    date accessioned2017-06-09T17:31:28Z
    date available2017-06-09T17:31:28Z
    date copyright2014/04/01
    date issued2013
    identifier issn0027-0644
    identifier otherams-86695.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4230281
    description abstractulerian velocity fields are derived from 300 drifters released in the Gulf of Mexico by The Consortium for Advanced Research on Transport of Hydrocarbon in the Environment (CARTHE) during the summer 2012 Grand Lagrangian Deployment (GLAD) experiment. These data are directly assimilated into the Navy Coastal Ocean Model (NCOM) four-dimensional variational data assimilation (4DVAR) analysis system in a series of experiments to investigate their impact on the model circulation. The NCOM-4DVAR is a newly developed tool for data analysis, formulated for weak-constraint data assimilation based on the indirect representer method. The assimilation experiments take advantage of this velocity data along with other available data sources from in situ and satellite measurements of surface and subsurface temperature and salinity. Three different experiments are done: (i) A nonassimilative NCOM free run, (ii) an assimilative NCOM run that utilizes temperature and salinity observations, and (iii) an assimilative NCOM run that uses temperature and salinity observations as well as the GLAD velocity observations. The resulting analyses and subsequent forecasts are compared to assimilated and future GLAD velocity and temperature/salinity observations to determine the performance of each experiment and the impact of the GLAD data on the analysis and the forecast. It is shown that the NCOM-4DVAR is able to fit the observations not only in the analysis step, but also in the subsequent forecast. It is also found that the GLAD velocity data greatly improves the characterization of the circulation, with the forecast showing a better fit to future GLAD observations than those experiments without the velocity data included.
    publisherAmerican Meteorological Society
    titleImpact of Assimilating Ocean Velocity Observations Inferred from Lagrangian Drifter Data Using the NCOM-4DVAR
    typeJournal Paper
    journal volume142
    journal issue4
    journal titleMonthly Weather Review
    identifier doi10.1175/MWR-D-13-00236.1
    journal fristpage1509
    journal lastpage1524
    treeMonthly Weather Review:;2013:;volume( 142 ):;issue: 004
    contenttypeFulltext
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