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Last edited by Plastikspork (talk | contribs) 2 months ago. (Update) |
trong Hải dương học vật lý, Tuần hoàn Langmuir bao gồm những dãy nước xoáy nông, chậm, có chiều ngược nhau trên bề mặt biển có gió thổi.Những vòng nước này được hình thành khi gió thổi đều đặn trên mặt đại dương. Irving Langmuir đã khám phá ra hiện tượng này khi đang quan sát những hàng tảo trên biển Sargasso vào năm 1927.[1]
Tham khảo
edit- Open University (2001), Ocean Circulation (ấn bản 2), Butterworth-Heinemann, ISBN 9780750652780
- ^ Open University (2001). Ocean Circulation (2nd ed.). Butterworth-Heinemann. ISBN 9780750652780.