Averaged sound intensity in shallow water having a negative leap-layer and a constant depth[J]. 海洋湖沼学报(英文), 1986,4(4):333-342.
Yingwu, T., Jinquan, X. Averaged sound intensity in shallow water having a negative leap-layer and a constant depth., Chin. J. Ocean. Limnol. 4, 333–342 (1986). https://doi.org/10.1007/BF02845280
Averaged sound intensity in shallow water having a negative leap-layer and a constant depth[J]. 海洋湖沼学报(英文), 1986,4(4):333-342. DOI: 10.1007/BF02845280.
Yingwu, T., Jinquan, X. Averaged sound intensity in shallow water having a negative leap-layer and a constant depth., Chin. J. Ocean. Limnol. 4, 333–342 (1986). https://doi.org/10.1007/BF02845280DOI:
Averaged sound intensity in shallow water having a negative leap-layer and a constant depth
摘要
Abstract
The leap-layer is assumed to consist of two isovelocity water layers. The expressions of the law on the decay of the averaged sound intensity with range are derived when the source and receiver are laid in the same isovelocity water layer or in two different isovelocity water layers respectively. The results show that there is apparent depth constitution in the sound field in the leap-layer. The theoretical results agree quite well with the practical data.
关键词
Keywords
references
Brekhovskikh, L.M., 1957. Waves in Layered Media (Moscow, English transl: Academic Press Inc., New York, 1960), PP. 313.
Bucker, H. P. and Morris, H. E., 1965. Normal mode intensity calculations for a constant depth shallow water channel.J. Acoust. Soc. Am.,38(6):1010–1017.
Zhang Renhe, Xiao Jinquan, Gong Min, 1981. Analysis of individual modes in shallow water,Acta Acoustica 5(3):73–85.
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