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    ADCP Measurements of Gravity Currents in the Chicago River, Illinois

    Source: Journal of Hydraulic Engineering:;2007:;Volume ( 133 ):;issue: 012
    Author:
    Carlos M. García
    ,
    Kevin Oberg
    ,
    Marcelo H. García
    DOI: 10.1061/(ASCE)0733-9429(2007)133:12(1356)
    Publisher: American Society of Civil Engineers
    Abstract: A unique set of observations of stratified flow phenomena in the Chicago River was made using an upward-looking acoustic Doppler current profiler (ADCP) during the period November 20, 2003 to February 1, 2004. Water density differences between the Chicago River and its North Branch (NB) seem to be responsible for the development of gravity currents. With the objective of characterizing the occurrence, frequency, and evolution of such currents, the ADCP was configured to continuously collect high-resolution water velocity and echo intensity profiles in the Chicago River at Columbus Drive. During the observation period, 28 gravity current events were identified, lasting a total of 77% of the time. Sixteen of these events were generated by underflows from the NB and 12 of these events were generated by overflows from the NB. On average, the duration of the underflow and overflow events was 52.3 and
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      ADCP Measurements of Gravity Currents in the Chicago River, Illinois

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    http://yetl.yabesh.ir/yetl1/handle/yetl/26241
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    contributor authorCarlos M. García
    contributor authorKevin Oberg
    contributor authorMarcelo H. García
    date accessioned2017-05-08T20:45:42Z
    date available2017-05-08T20:45:42Z
    date copyrightDecember 2007
    date issued2007
    identifier other%28asce%290733-9429%282007%29133%3A12%281356%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/26241
    description abstractA unique set of observations of stratified flow phenomena in the Chicago River was made using an upward-looking acoustic Doppler current profiler (ADCP) during the period November 20, 2003 to February 1, 2004. Water density differences between the Chicago River and its North Branch (NB) seem to be responsible for the development of gravity currents. With the objective of characterizing the occurrence, frequency, and evolution of such currents, the ADCP was configured to continuously collect high-resolution water velocity and echo intensity profiles in the Chicago River at Columbus Drive. During the observation period, 28 gravity current events were identified, lasting a total of 77% of the time. Sixteen of these events were generated by underflows from the NB and 12 of these events were generated by overflows from the NB. On average, the duration of the underflow and overflow events was 52.3 and
    publisherAmerican Society of Civil Engineers
    titleADCP Measurements of Gravity Currents in the Chicago River, Illinois
    typeJournal Paper
    journal volume133
    journal issue12
    journal titleJournal of Hydraulic Engineering
    identifier doi10.1061/(ASCE)0733-9429(2007)133:12(1356)
    treeJournal of Hydraulic Engineering:;2007:;Volume ( 133 ):;issue: 012
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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