Výsledky vyhledávání - "Janet H. Curran"

Glacial conditioning of stream position and flooding in the braid plain of the Exit Glacier foreland, Alaska

Autor: Haley B. Williams, Janet H. Curran, Michael G. Loso

Publikováno v: Geomorphology. 293:272-288

Flow spilling out of an active braid plain often signals the onset of channel migration or avulsion to previously occupied areas. In a recently deglaciated environment, distinguishing between shifts in active braid plain location, considered reversib

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::9f8fa43555332878e38e58bf478557e9
https://doi.org/10.1016/j.geomorph.2017.06.004

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Estimating flood magnitude and frequency at gaged and ungaged sites on streams in Alaska and conterminous basins in Canada, based on data through water year 2012

Autor: Andrea G. Veilleux, Robert T. Ourso, Nancy A. Barth, Janet H. Curran

Publikováno v: Scientific Investigations Report.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::5fde860acf6812a2a340270119205603
https://doi.org/10.3133/sir20165024

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Large woody debris and flow resistance in step-pool channels, Cascade Range, Washington

Autor: Janet H. Curran, Ellen Wohl

Publikováno v: Geomorphology. 51:141-157

Total flow resistance, measured as Darcy–Weisbach f, in 20 step-pool channels with large woody debris (LWD) in Washington, ranged from 5 to 380 during summer low flows. Step risers in the study streams consist of either (1) large and relatively imm

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::a99d0ca2299c9b39e6a204cd12762f16
https://doi.org/10.1016/s0169-555x(02)00333-1

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Quaternary Geology and Geomorphology of the Lower Deschutes River Canyon, Oregon

Autor: Gordon E. Grant, Andrei M. Sarna-Wojcicki, Robin A. Beebee, Janet H. Curran, Jim E. O'Connor

Publikováno v: A Peculiar River

The morphology of the Deschutes River canyon downstream of the Pelton-Round Butte dam complex is the product of the regional geologic history, the composition of the geologic units that compose the valley walls, and Quaternary processes and events. G

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::43c90e68c96c4e8431914d2f2a25a29c
https://doi.org/10.1029/007ws07

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