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Mechanism 2: crossing waves

Research output: Contribution in Book/Report/Proceedings - With ISBN/ISSN › Chapter (peer-reviewed) › peer-review

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Mechanism 2: crossing waves. / Ilic, Suzana; Luxmoore, James; Mori, Nobuhito.
Science and Engineering of Freak Waves. ed. / Nobuhito Mori; Takuji Waseda; Amin Chabchoub. 1st. ed. Elsevier, 2023. p. 77-97.

Research output: Contribution in Book/Report/Proceedings - With ISBN/ISSN › Chapter (peer-reviewed) › peer-review

Harvard

Ilic, S, Luxmoore, J & Mori, N 2023, Mechanism 2: crossing waves. in N Mori, T Waseda & A Chabchoub (eds), Science and Engineering of Freak Waves. 1st edn, Elsevier, pp. 77-97. <https://shop.elsevier.com/books/science-and-engineering-of-freak-waves/mori/978-0-323-91736-0>

APA

Ilic, S., Luxmoore, J., & Mori, N. (2023). Mechanism 2: crossing waves. In N. Mori, T. Waseda, & A. Chabchoub (Eds.), Science and Engineering of Freak Waves (1st ed., pp. 77-97). Elsevier. https://shop.elsevier.com/books/science-and-engineering-of-freak-waves/mori/978-0-323-91736-0

Vancouver

Ilic S, Luxmoore J, Mori N. Mechanism 2: crossing waves. In Mori N, Waseda T, Chabchoub A, editors, Science and Engineering of Freak Waves. 1st ed. Elsevier. 2023. p. 77-97

Author

Ilic, Suzana ; Luxmoore, James ; Mori, Nobuhito. / Mechanism 2: crossing waves. Science and Engineering of Freak Waves. editor / Nobuhito Mori ; Takuji Waseda ; Amin Chabchoub. 1st. ed. Elsevier, 2023. pp. 77-97

Bibtex

@inbook{0b29cf146dae4c1f8e116d56dc6358e4,
title = "Mechanism 2: crossing waves",
abstract = "Bimodal and crossing seas can generate extreme and freak wave events (see e.g. Tamura et al., 2009). Sea states comprised of swell and wind waves resulting in two distinctive frequency peaks are a common feature in oceans. If they travel along different directions, two distinctive directional peaks can be detected. These are referred to here as bimodal or crossing seas. This bimodal state can also be caused by rapidly turning wind, which will result in two sea states with similar frequency distributions and different directions. This chapter summarises the mechanisms responsible for formation of rogues waves in crossing seas, laboratory measurements, numerical simulations of crossing wave fields and nonlinear wave statistics.",
keywords = "crossing sea, angle, directionality, long-crested wave, short-crested wave",
author = "Suzana Ilic and James Luxmoore and Nobuhito Mori",
year = "2023",
month = oct,
day = "27",
language = "English",
isbn = "9780323917360",
pages = "77--97",
editor = "Mori, {Nobuhito } and Takuji Waseda and Amin Chabchoub",
booktitle = "Science and Engineering of Freak Waves",
publisher = "Elsevier",
edition = "1st",

}

RIS

TY - CHAP

T1 - Mechanism 2: crossing waves

AU - Ilic, Suzana

AU - Luxmoore, James

AU - Mori, Nobuhito

PY - 2023/10/27

Y1 - 2023/10/27

N2 - Bimodal and crossing seas can generate extreme and freak wave events (see e.g. Tamura et al., 2009). Sea states comprised of swell and wind waves resulting in two distinctive frequency peaks are a common feature in oceans. If they travel along different directions, two distinctive directional peaks can be detected. These are referred to here as bimodal or crossing seas. This bimodal state can also be caused by rapidly turning wind, which will result in two sea states with similar frequency distributions and different directions. This chapter summarises the mechanisms responsible for formation of rogues waves in crossing seas, laboratory measurements, numerical simulations of crossing wave fields and nonlinear wave statistics.

AB - Bimodal and crossing seas can generate extreme and freak wave events (see e.g. Tamura et al., 2009). Sea states comprised of swell and wind waves resulting in two distinctive frequency peaks are a common feature in oceans. If they travel along different directions, two distinctive directional peaks can be detected. These are referred to here as bimodal or crossing seas. This bimodal state can also be caused by rapidly turning wind, which will result in two sea states with similar frequency distributions and different directions. This chapter summarises the mechanisms responsible for formation of rogues waves in crossing seas, laboratory measurements, numerical simulations of crossing wave fields and nonlinear wave statistics.

KW - crossing sea, angle, directionality, long-crested wave, short-crested wave

M3 - Chapter (peer-reviewed)

SN - 9780323917360

SP - 77

EP - 97

BT - Science and Engineering of Freak Waves

A2 - Mori, Nobuhito

A2 - Waseda, Takuji

A2 - Chabchoub, Amin

PB - Elsevier

ER -