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Gao, Peng, Josefson, Maria (2012) Event-based suspended sediment dynamics in a central New York watershed. Geomorphology, 139. 425-437 doi:10.1016/j.geomorph.2011.11.007

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Reference TypeJournal (article/letter/editorial)
TitleEvent-based suspended sediment dynamics in a central New York watershed
JournalGeomorphology
AuthorsGao, PengAuthor
Josefson, MariaAuthor
Year2012 (February)Volume139
PublisherElsevier BV
DOIdoi:10.1016/j.geomorph.2011.11.007Search in ResearchGate
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Mindat Ref. ID946006Long-form Identifiermindat:1:5:946006:9
GUID0
Full ReferenceGao, Peng, Josefson, Maria (2012) Event-based suspended sediment dynamics in a central New York watershed. Geomorphology, 139. 425-437 doi:10.1016/j.geomorph.2011.11.007
Plain TextGao, Peng, Josefson, Maria (2012) Event-based suspended sediment dynamics in a central New York watershed. Geomorphology, 139. 425-437 doi:10.1016/j.geomorph.2011.11.007
In(2012) Geomorphology Vol. 139. Elsevier BV

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Gao, Peng, Puckett, James (2012) A new approach for linking event-based upland sediment sources to downstream suspended sediment transport. Earth Surface Processes and Landforms, 37 (2) 169-179 doi:10.1002/esp.2229
Tian, Peng, Feng, Jiahao, Zhao, Guangju, Gao, Peng, Sun, Wenyi, Hörmann, Georg, Mu, Xingmin (2022) Rainfall, runoff, and suspended sediment dynamics at the flood event scale in a Loess Plateau watershed, China. Hydrological Processes, 36 (2) doi:10.1002/hyp.14486
Mao, Luca, Carrillo, Ricardo (2017) Temporal dynamics of suspended sediment transport in a glacierized Andean basin. Geomorphology, 287. 116-125 doi:10.1016/j.geomorph.2016.02.003
Gao, Peng, Cooper, James R., Wainwright, John (2019) Toward understanding complexity of sediment dynamics in geomorphic systems. Geomorphology, 330. 129-132 doi:10.1016/j.geomorph.2019.01.018
De Freitas, Cathrine-Rose, Grenfell, Suzanne (2024) Event-scale suspended sediment fluxes in a dryland environment valley-bottom wetland: Implications for downstream sediment and phosphorous fluxes. Geomorphology, 452. 109101 doi:10.1016/j.geomorph.2024.109101
 
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