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The National Ocean Sciences Bowl (NOSB) is a national high-school science competition currently hosted by the Center for Ocean Leadership, a University Corporation for Atmospheric Research Community Program beginning 10/3/2022.
This is a coupled ocean/atmosphere wave that circles the Southern Ocean about every eight years. Since it is a wave-2 phenomenon (there are two peaks and two troughs in a latitude circle) at each fixed point in space a signal with a period of four years is seen. The wave moves eastward in the direction of the Antarctic Circumpolar Current.
The series aired on PBS (Public Broadcasting Service) and was created by the Bank Street College of Education in 1984 [3] to teach middle-schoolers about science and mathematics in an interesting and interactive way, where every lesson related to real world applications. Its budget was 3.65 million dollars.
In physical oceanography and fluid mechanics, the Miles-Phillips mechanism describes the generation of wind waves from a flat sea surface by two distinct mechanisms. Wind blowing over the surface generates tiny wavelets. These wavelets develop over time and become ocean surface waves by absorbing the energy transferred from the wind.
When you spend time on the ocean, it’s safe to assume the animals that call the sea home will stay in the water. This wasn’t the case for an Australian kite surfer.
Breaking swell waves at Hermosa Beach, California. A swell, also sometimes referred to as ground swell, in the context of an ocean, sea or lake, is a series of mechanical waves that propagate along the interface between water and air under the predominating influence of gravity, and thus are often referred to as surface gravity waves.
Ocean Waves, known in Japan as I Can Hear the Sea (Japanese: 海がきこえる, Hepburn: Umi ga Kikoeru), is a 1993 Japanese anime coming-of-age romantic drama television film directed by Tomomi Mochizuki and written by Keiko Niwa (credited as Kaoru Nakamura) based on the 1990–1992 novel of the same name by Saeko Himuro.
When waves travel into areas of shallow water, they begin to be affected by the ocean bottom. [1] The free orbital motion of the water is disrupted, and water particles in orbital motion no longer return to their original position. As the water becomes shallower, the swell becomes higher and steeper, ultimately assuming the familiar sharp ...
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related to: educational activities for high schoolers about ocean waveseducation.com has been visited by 100K+ users in the past month