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    Near-Surface Current Mapping by Shipboard Marine X-Band Radar: A Validation

    Source: Journal of Atmospheric and Oceanic Technology:;2018:;volume 035:;issue 005::page 1077
    Author:
    Lund, Björn
    ,
    Haus, Brian K.
    ,
    Horstmann, Jochen
    ,
    Graber, Hans C.
    ,
    Carrasco, Ruben
    ,
    Laxague, Nathan J. M.
    ,
    Novelli, Guillaume
    ,
    Guigand, Cédric M.
    ,
    Özgökmen, Tamay M.
    DOI: 10.1175/JTECH-D-17-0154.1
    Publisher: American Meteorological Society
    Abstract: AbstractThe Lagrangian Submesoscale Experiment (LASER) involved the deployment of ~1000 biodegradable GPS-tracked Consortium for Advanced Research on Transport of Hydrocarbon in the Environment (CARTHE) drifters to measure submesoscale upper-ocean currents and their potential impact on oil spills. The experiment was conducted from January to February 2016 in the Gulf of Mexico (GoM) near the mouth of the Mississippi River, an area characterized by strong submesoscale currents. A Helmholtz-Zentrum Geesthacht (HZG) marine X-band radar (MR) on board the R/V F. G. Walton Smith was used to locate fronts and eddies by their sea surface roughness signatures. The MR data were further processed to yield near-surface current maps at ~500-m resolution up to a maximum range of ~3 km. This study employs the drifter measurements to perform the first comprehensive validation of MR near-surface current maps. For a total of 4130 MR?drifter pairs, the root-mean-square error for the current speed is 4 cm and that for the current direction is 12°. The MR samples currents at a greater effective depth than the CARTHE drifters (1?5 m vs ~0.4 m). The mean MR?drifter differences are consistent with a wave- and wind-driven vertical current profile that weakens with increasing depth and rotates clockwise from the wind direction (by 0.7% of the wind speed and 15°). The technique presented here has great potential in observational oceanography, as it allows research vessels to map the horizontal flow structure, complementing the vertical profiles measured by ADCP.
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      Near-Surface Current Mapping by Shipboard Marine X-Band Radar: A Validation

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4261073
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    contributor authorLund, Björn
    contributor authorHaus, Brian K.
    contributor authorHorstmann, Jochen
    contributor authorGraber, Hans C.
    contributor authorCarrasco, Ruben
    contributor authorLaxague, Nathan J. M.
    contributor authorNovelli, Guillaume
    contributor authorGuigand, Cédric M.
    contributor authorÖzgökmen, Tamay M.
    date accessioned2019-09-19T10:03:35Z
    date available2019-09-19T10:03:35Z
    date copyright3/5/2018 12:00:00 AM
    date issued2018
    identifier otherjtech-d-17-0154.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4261073
    description abstractAbstractThe Lagrangian Submesoscale Experiment (LASER) involved the deployment of ~1000 biodegradable GPS-tracked Consortium for Advanced Research on Transport of Hydrocarbon in the Environment (CARTHE) drifters to measure submesoscale upper-ocean currents and their potential impact on oil spills. The experiment was conducted from January to February 2016 in the Gulf of Mexico (GoM) near the mouth of the Mississippi River, an area characterized by strong submesoscale currents. A Helmholtz-Zentrum Geesthacht (HZG) marine X-band radar (MR) on board the R/V F. G. Walton Smith was used to locate fronts and eddies by their sea surface roughness signatures. The MR data were further processed to yield near-surface current maps at ~500-m resolution up to a maximum range of ~3 km. This study employs the drifter measurements to perform the first comprehensive validation of MR near-surface current maps. For a total of 4130 MR?drifter pairs, the root-mean-square error for the current speed is 4 cm and that for the current direction is 12°. The MR samples currents at a greater effective depth than the CARTHE drifters (1?5 m vs ~0.4 m). The mean MR?drifter differences are consistent with a wave- and wind-driven vertical current profile that weakens with increasing depth and rotates clockwise from the wind direction (by 0.7% of the wind speed and 15°). The technique presented here has great potential in observational oceanography, as it allows research vessels to map the horizontal flow structure, complementing the vertical profiles measured by ADCP.
    publisherAmerican Meteorological Society
    titleNear-Surface Current Mapping by Shipboard Marine X-Band Radar: A Validation
    typeJournal Paper
    journal volume35
    journal issue5
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/JTECH-D-17-0154.1
    journal fristpage1077
    journal lastpage1090
    treeJournal of Atmospheric and Oceanic Technology:;2018:;volume 035:;issue 005
    contenttypeFulltext
    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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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian