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J-GLOBAL ID:200902276161361760   Reference number:03A0811193

超音波反射強度から求めた砕波に伴う気泡連行特性

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Volume: 50  Issue:Page: 116-120  Publication year: Oct. 10, 2003 
JST Material Number: S0450A  ISSN: 0916-7897  Document type: Proceedings
Article type: 原著論文  Country of issue: Japan (JPN)  Language: JAPANESE (JA)
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Coastal engineering 
Reference (6):
  • 吉岡洋・芹沢重厚・高山知司 (1998): 超音波による海面境界層の観測 (風波砕波による気泡の取り込み), 海岸工学論文集, 第45巻, pp71-75
  • Hanson, J. L. and 0. M. Phillips (1999): Wind Sea Growth and Dissipation in the Open Ocean, Journal of Physical Oceangraphy, Vol.29, pp.1633-1648.
  • Leeuw, G. and L. H. Cohen (2000): Bubble size distributionson the North Atlantic and North Sea, Gas Transfer at Water Surfaces, Geophysical Monograph 127, pp.271-277.
  • Thorpe, S. A.(1992): On the clouds of bubbles formed by breaking wind waves in deep water, and their role in air-sea gas fransfer, Phil. Trans. R. Soc. London, A 304, pp.155- 210.
  • Toba Y. and H. Kawamura (1996): Wind-wave coupled downward-bursting boundary layer (DBBL) beneath the sea surface, J. Oceanography, Vol.52, pp.409-419.
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