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- https://geo.libretexts.org/Courses/Coalinga_College/Introduction_to_Earth_Science_(C-ID%3A_GEOL_121)/03%3A_The_Hydrosphere/3.11%3A_Waves_at_SeaConstructive interference occurs when the two waves are completely in phase; the crest of one wave lines up exactly with the crest of the other wave, as do the troughs of the two waves. Waves in the S...Constructive interference occurs when the two waves are completely in phase; the crest of one wave lines up exactly with the crest of the other wave, as do the troughs of the two waves. Waves in the Southern Ocean are generally fairly large (the red areas in Figure \(\PageIndex{2}\)) because of the strong winds and the lack of landmasses, which provide the winds with a very long fetch, allowing them to blow unimpeded over the ocean for very long distances.
- https://geo.libretexts.org/Courses/Diablo_Valley_College/OCEAN-101%3A_Fundamentals_of_Oceanography_(Keddy)/12%3A_Waves/12.01%3A_Waves/12.1.02%3A_Waves_at_SeaConstructive interference occurs when the two waves are completely in phase; the crest of one wave lines up exactly with the crest of the other wave, as do the troughs of the two waves. Waves in the S...Constructive interference occurs when the two waves are completely in phase; the crest of one wave lines up exactly with the crest of the other wave, as do the troughs of the two waves. Waves in the Southern Ocean are generally fairly large (the red areas in Figure \(\PageIndex{2}\)) because of the strong winds and the lack of landmasses, which provide the winds with a very long fetch, allowing them to blow unimpeded over the ocean for very long distances.
- https://geo.libretexts.org/Courses/Sierra_College/Introduction_to_Oceanography_(Sierra_College_Edition)/10%3A_Waves/10.02%3A_Waves_at_SeaConstructive interference occurs when the two waves are completely in phase; the crest of one wave lines up exactly with the crest of the other wave, as do the troughs of the two waves. Waves in the S...Constructive interference occurs when the two waves are completely in phase; the crest of one wave lines up exactly with the crest of the other wave, as do the troughs of the two waves. Waves in the Southern Ocean are generally fairly large (the red areas in Figure \(\PageIndex{2}\)) because of the strong winds and the lack of landmasses, which provide the winds with a very long fetch, allowing them to blow unimpeded over the ocean for very long distances.
- https://geo.libretexts.org/Bookshelves/Oceanography/Introduction_to_Oceanography_(Webb)/10%3A_Waves/10.02%3A_Waves_at_SeaConstructive interference occurs when the two waves are completely in phase; the crest of one wave lines up exactly with the crest of the other wave, as do the troughs of the two waves. Waves in the S...Constructive interference occurs when the two waves are completely in phase; the crest of one wave lines up exactly with the crest of the other wave, as do the troughs of the two waves. Waves in the Southern Ocean are generally fairly large (the red areas in Figure \(\PageIndex{2}\)) because of the strong winds and the lack of landmasses, which provide the winds with a very long fetch, allowing them to blow unimpeded over the ocean for very long distances.
