How Do Some Waves Get SO Big?

published 4 months ago by Neptune Studios

Enjoy 10% off MOVA Globes with code MINUTEEARTH. Shop now on All over the world, giant wave breaks appear because of underwater geology that supercharges their wave energy. LEARN MORE ************** To learn more about this topic, start your googling with these keywords: Amplitude - The distance between the crest and trough of a wave. Bathymetry - The measurement of depth of water in oceans, seas, or lakes. Nazaré Canyon - An undersea canyon just off the coast of Nazaré, Portugal, in the eastern North Atlantic Ocean. It is the largest submarine canyon in Europe, reaching depths of about 5,000 meters (16,000 ft) deep and a length of about 230 kilometers (140 mi). Plunging Breaker - Occurs when there are rapid depth changes. The crest of the wave becomes very steep, and the rear of the wave violently plunges over the front. Reef Break - A location where waves break over a reef, often amplifying them. Spilling Breaker - Occurs when the seafloor slopes gradually. As the wave becomes unstable, energy is dissipated by water spilling over the crest of the wave. Swell - a slow, regular movement of the sea in rolling waves that do not break. Wave period - The time between waves. SUPPORT MINUTEEARTH ************************** If you like what we do, you can help us!: - Become our patron: - Share this video with your friends and family - Leave us a comment (we read them!) CREDITS ********* Cameron Duke | Script Writer Kate Yoshida | Narrator David Goldenberg | Director Arcadi Garcia i Rius | Illustration, Video Editing, and Animation Nathaniel Schroeder | Music MinuteEarth is produced by Neptune Studios LLC OUR STAFF ************ Sarah Berman • Arcadi Garcia Rius David Goldenberg • Julián Gustavo Gómez Melissa Hayes • Alex Reich • Henry Reich Peter Reich • Ever Salazar • Kate Yoshida OUR LINKS ************ Youtube | TikTok | minuteearth Twitter | Instagram | Facebook | Website | Apple Podcasts| REFERENCES ************** Babanin, A. V., Rogers, W. E., de Camargo, R., Doble, M., Durrant, T., Filchuk, K., Ewans, K., Hemer, M., Janssen, T., Kelly-Gerreyn, B., Machutchon, K., McComb, P., Qiao, F., Schulz, E., Skvortsov, A., Thomson, J., Vichi, M., Violante-Carvalho, N., Wang, D., & Waseda, T. (2019). Waves and Swells in High Wind and Extreme Fetches, Measurements in the Southern Ocean. Frontiers in Marine Science, 6. Retrieved from: Editor At (2013, November 5). The canyon that makes waves. Surfertoday; | The Ultimate Surfing News Website. Retrieved from: Griffiths, L. S., & Porter, R. (2012). Focusing of surface waves by variable bathymetry. Applied Ocean Research, 34, 150–163. Retrieved from: Inman, D. (2021). Living with Coastal Change - Coastal Basics - Wave Refraction Model - Jaws, Hawaii. Retrieved from: Keating, S. (2020, January 6). The story of a wave: from wind-blown ripples to breaking on the beach. The Conversation. Retrieved from: Pedro Proença Cunha, & Margarida, M. (2015, February). The Nazaré coast, the submarine canyon and the giant waves - a synthesis. ResearchGate; Universidade de Coimbra. Retrieved from: Pinet, P. R. (2009). Invitation to oceanography (5th ed.). Jones & Bartlett Learning. The generation and propagation of ocean waves and swell. I. Wave periods and velocities | Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences. (2017). Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences. Retrieved from: Warner, S. (2020). What makes the world’s biggest surfable waves? The Conversation. Retrieved from: Warner, S. (2021). Department of Environmental Studies, Brandeis University. Personal Communication. Homepage:

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