BoucherBeginArseneaultEtAl2012

Référence

Boucher, E., Begin, Y., Arseneault, D., Ouarda, T.B.M.J. (2012) Long-Term and Large-Scale River-Ice Processes in Cold-Region Watersheds. (Scopus )

Résumé

This work focuses on large scale and long term ice jam dynamics. From a brief review of the literature and also by relying on personally collected data, three aspects are highlighted. First, we show that long ice jam chronologies increase the accuracy of ice jam frequency estimates at the local scale. Ice jam frequencies vary considerably through time and as a function of the time scale considered for the analysis. Second, we demonstrate that large scale river ice surveys enable characterization of the spatial variations of ice jamming activity within watersheds and help to identify sites where this activity is most frequent. Finally, we establish that large scale geomorphological descriptions coupled to spatio-temporally extensive ice jam data sets provide a unique insight into the various responses of river channels to ice dynamics. © 2012 John Wiley & Sons, Ltd.

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@BOOK { BoucherBeginArseneaultEtAl2012,
    TITLE = { Long-Term and Large-Scale River-Ice Processes in Cold-Region Watersheds },
    YEAR = { 2012 },
    AUTHOR = { Boucher, E. and Begin, Y. and Arseneault, D. and Ouarda, T.B.M.J. },
    PAGES = { 546-554 },
    NOTE = { cited By 1 },
    ABSTRACT = { This work focuses on large scale and long term ice jam dynamics. From a brief review of the literature and also by relying on personally collected data, three aspects are highlighted. First, we show that long ice jam chronologies increase the accuracy of ice jam frequency estimates at the local scale. Ice jam frequencies vary considerably through time and as a function of the time scale considered for the analysis. Second, we demonstrate that large scale river ice surveys enable characterization of the spatial variations of ice jamming activity within watersheds and help to identify sites where this activity is most frequent. Finally, we establish that large scale geomorphological descriptions coupled to spatio-temporally extensive ice jam data sets provide a unique insight into the various responses of river channels to ice dynamics. © 2012 John Wiley & Sons, Ltd. },
    AUTHOR_KEYWORDS = { Dendrochronology; Hydraulic geometry; Ice jams; Risk; Riverbank geomorphology },
    DOCUMENT_TYPE = { Book Chapter },
    DOI = { 10.1002/9781119952497.ch39 },
    JOURNAL = { Gravel-Bed Rivers: Processes, Tools, Environments },
    SOURCE = { Scopus },
    URL = { http://www.scopus.com/inward/record.url?eid=2-s2.0-84878655285&partnerID=40&md5=4d89eaf8e0bffdea6f4b2f190092334a },
}

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