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pro vyhledávání: '"Tinh, Than Xuan"'
Autor:
Dolojan, Nilo Lemuel J., Moriguchi, Shuji, Hashimoto, Masakazu, Tinh, Nguyen Xuan, Tanaka, Hitoshi, Terada, Kenjiro
Publikováno v:
In Engineering Geology 20 September 2023 323
Publikováno v:
In Continental Shelf Research 1 December 2021 231
Publikováno v:
Journal of Water and Climate Change; March 2024, Vol. 15 Issue: 3 p1262-1281, 20p
Autor:
Tanaka, Hitoshi, Tinh, Nguyen Xuan
Publikováno v:
In Procedia IUTAM 2017 25:10-17
Akademický článek
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Autor:
VIET NGUYEN TRUNG, Nhat Quang Dinh, Tinh Nguyen Xuan, Sy Tam Ho, Nguyễn Quang Đức Anh, Hitoshi Tanaka
Publikováno v:
Journal of Marine Science and Engineering; Volume 11; Issue 3; Pages: 611
Coastal erosion and accretion along the Quang Nam coast in Vietnam have been increasing in recent years, causing negative impacts on the inhabitants and local ecology. The Cua Lo estuary in Nui Thanh district has a complex hydrodynamic regime owing t
Publikováno v:
Intelligent Systems and Networks ISBN: 9789811933936
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e1571065b532246c36f742bd7875dfc9
https://doi.org/10.1007/978-981-19-3394-3_22
https://doi.org/10.1007/978-981-19-3394-3_22
Publikováno v:
Intelligent Systems and Networks ISBN: 9789811933936
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f11b9be589e148b0ddbadd40c0c0a48d
https://doi.org/10.1007/978-981-19-3394-3_23
https://doi.org/10.1007/978-981-19-3394-3_23
Publikováno v:
MATEC Web of Conferences, Vol 161, p 02013 (2018)
Multi-motor drive systems are nonlinear, multi-input multi-output (MIMO) and strong-coupling complicated system, including the effect of friction and elastic, backlash. They have been widely used in many modern industries. The control law for this di
Externí odkaz:
https://doaj.org/article/3cc46269ac064313b3deca20cf47cc4d
Publikováno v:
Journal of Marine Science and Engineering; Volume 10; Issue 10; Pages: 1433
According to recent investigations on bottom boundary layer development under tsunami, a wave boundary can be observed even at the water depth of 10 m, rather than a steady flow type boundary layer. Moreover, it has been surprisingly reported that th