Jose A. Constantine, Ph.D.

Affiliations: 
2008 Geological Sciences University of California, Santa Barbara, Santa Barbara, CA, United States 
Area:
Geology, Physical Geography
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"Jose Constantine"

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Thomas Dunne grad student 2008 UC Santa Barbara
 (Meander cutoff and the controls on the production and evolution of oxbow lakes.)
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Publications

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Qin Y, Alves TM, Constantine JA, et al. (2020) Effect of channel tributaries on the evolution of submarine channel confluences (Espírito Santo Basin, SE Brazil) Geological Society of America Bulletin. 132: 263-272
Ahmed J, Constantine JA, Dunne T. (2019) The role of sediment supply in the adjustment of channel sinuosity across the Amazon Basin Geology. 47: 807-810
Horton AJ, Lazarus ED, Hales TC, et al. (2018) Can Riparian Forest Buffers Increase Yields From Oil Palm Plantations? Earth's Future. 6: 1082-1096
Qin Y, Alves TM, Constantine J, et al. (2017) The Role of Mass Wasting In the Progressive Development Of Submarine Channels (Espírito Santo Basin, Se Brazil) Journal of Sedimentary Research. 87: 500-516
Horton AJ, Constantine JA, Hales TC, et al. (2017) Modification of river meandering by tropical deforestation Geology. 45: 511-514
Parker RN, Hales TC, Mudd SM, et al. (2016) Colluvium supply in humid regions limits the frequency of storm-triggered landslides. Scientific Reports. 6: 34438
Qin Y, Alves TM, Constantine J, et al. (2016) Quantitative seismic geomorphology of a submarine channel system in SE Brazil (Espírito Santo Basin): Scale comparison with other submarine channel systems Marine and Petroleum Geology. 78: 455-473
Thomas RJ, Constantine JA, Gough P, et al. (2015) Rapid Channel Widening Following Weir Removal due to Bed-Material Wave Dispersion on the River Monnow, Wales River Research and Applications. 31: 1017-1027
Constantine JA, Dunne T, Ahmed J, et al. (2014) Sediment supply as a driver of river meandering and floodplain evolution in the Amazon Basin Nature Geoscience. 7: 899-903
Lazarus ED, Constantine JA. (2013) Generic theory for channel sinuosity. Proceedings of the National Academy of Sciences of the United States of America. 110: 8447-52
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