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Katsuto Uehara Last modified date:2020.06.27



Graduate School


E-Mail
Homepage
https://kyushu-u.pure.elsevier.com/en/persons/katsuto-uehara
 Reseacher Profiling Tool Kyushu University Pure
Phone
092-583-7728
Fax
092-573-1996
Academic Degree
D. Sc.
Country of degree conferring institution (Overseas)
No
Field of Specialization
Physical Oceanography
Total Priod of education and research career in the foreign country
01years00months
Research
Research Interests
  • Depositional and removal processes of sea-bottom sediments in East and Southeast Asian continental shelves
    keyword : continental shelf, re-suspension, sediment transport, south china sea, east china sea
    2008.04~2025.03.
  • Coastal erosion along Asian megadeltas
    keyword : coastal erosion, climate change, human activity
    2008.07~2016.03.
  • Changes in oceanic environment since the Last Glacial Maximum on the NW European Shelf
    keyword : NW European Shelf, tides, climate change, numerical simulation
    2002.04.
  • Changes in oceanic environments in the East China Sea since the Last Glacial Maximum
    keyword : East China Sea, Changjiang, climate change, numerical simulation, continental shelf
    1999.04.
Academic Activities
Papers
1. Katsuto Uehara, Yoshiki Saito, Tidal amplitude decreases in response to estuarine shrinkage
Tokyo Bay during the Holocene, Estuarine, Coastal and Shelf Science, 10.1016/j.ecss.2019.05.007, 225, 2019.09, Tidal changes in Tokyo Bay during the last 10,000 years were investigated by combining a numerical model with newly compiled model bathymetries for the present day, the early 20th century, and every 1000 years from 4000 to 10,000 years ago. Over this time period, sea level has changed by more than 30 m, and the coastline has shifted 50–60 km. Tides during the early 20th century and 4000–9000 years ago were larger than those at present; from 9000 to 4000 years ago, the bay setting was mesotidal, in contrast to the modern microtidal setting. The maximum tidal level at the head of the bay was 72% higher 7000 years ago than at present, and M2 tidal currents at the bay mouth from 10,000 to 9000 years ago were three times stronger than those at present. When tides were compared at a fixed location, the greatest tidal enhancement was found to have occurred 9000 years ago. The weakening of tides over the last 9000 years can be explained by introducing the concept of estuarine shrinkage together with quarter-wavelength resonance theory. Tidal weakening occurred in two phases: during the first phase, 9000–7000 years ago, it was due to the rise in sea level (type 2 shrinkage), and during the second phase, a decrease in the length of the bay was responsible (type 1 shrinkage). These findings can be applied to the assessment of both past tidal changes and potential future tidal changes in other elongated estuaries with lengths of several tens of kilometers..
2. Uehara, K., Sojisuporn, P., Saito, Y., Jarupongsakul, T., Erosion and accretion processes in a muddy dissipative coast, the Chao Phraya River delta, Thailand, Earth Surface Processes and Landforms, 10.1002/esp.2012, 35, 14, 1701-1711, doi:10.1002/esp.2012, 2010.04.
3. Uehara, K., Scourse, J.D., Horsburgh, K.J., Lambeck, K., Purcell, A.P., Tidal evolution of the northwest European shelf seas from the Last Glacial Maximum to the present, Journal of Geophysical Research--Oceans, 10.1029/2006JC003531, 111, C9, Vol. 111, C09025, doi:10.1029/2006JC003531, 15pp., 2006.09.
4. Uehara, K., Saito, Y., Late Quaternary evolution of the Yellow/East China Sea tidal regime and its impacts on sediments dispersal and seafloor morphology, Sedimentary Geology, 10.1016/S0037-0738(03)00234-3, 162, 1-2, 25-38, Volume 162, issue 1-2, p. 25-38, 2003.11.