海洋混合层结构对表面声道中声传播特性的影响分析

张旭; 张永刚; 张健雪; 董楠

海洋混合层结构对表面声道中声传播特性的影响分析

1.
中国人民解放军91550部队, 辽宁大连 116023
2.
海军大连舰艇学院科研部, 辽宁大连 116018
3.
中国海洋大学海洋环境学院, 山东青岛 266003

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出版历程
- 收稿日期: 2010-04-15
- 修回日期: 2011-04-05

The effect of ocean mixed-layer structure on acoustic propagation in a surface duct environment

1.
Unit 91550 of PLA, Dalian 116023, China
2.
Department of Scientific Research, Dalian Naval Academy, Dalian 116018, China
3.
Institute of Marine Environment, Ocean University of China, Qingdao 266003, China

摘要

摘要: 利用WOA05气候态数据集和北黄海调查数据,应用BELLHOP高斯束射线模型分析了我国近海及西太平洋典型海区的混合层结构对表面声道中声传播特性的影响,结果表明:我国近海的混合层结构有显著的区域性和季节性变化;深海中主要表现为混合层深度变化,这种变化直接影响表面声道的空间分布,声波在混合层中的表面声道中传播与在混合层外的影区中传播产生的能量场差异较大;浅海中混合层深度与声速梯度的空间变化都很明显,声速梯度的增大和混合层的加深都能使更多声线以反转的形式传播,使表面声道声场增强。两组海上实验数据表明,在真实海洋中混合层可在短时间内出现生消变化或在局部海域出现非均匀分布。在浅海温跃层环境下,海-气边界特定的物理过程能够使混合层发生间歇性的变化,当表面声道出现时近表层声场明显增强。
- 混合层 /
- 声速剖面 /
- 表面声道 /
- 声传播 /
- BELLHOP模型
Abstract: Based on WOA05 climatological database and the measured hydrologic data in the northern Huanghai Sea, the effect of typical mixed-layer structures on the acoustic propagation in a surface duct environment in adjacent sea areas of China is discussed using the BELLHOP Gaussian beam model. The mixed-layer structures show distinct variations between different areas and seasons. In the deep sea, the mixed-layer depth is a main variable factor, which defines the vertical space of the surface duct. A obvious difference of acoustic energe level appears when the propagation occurs in a surface channel inside the mixed-layer compared with that in a shadow zone outside the mixed-layer. In the shallow water, the mixed-layer depth and the sound speed grads are both streaky. More reversal rays are involved when the sound speed grads enhancing or the mixed-layer depth deepening, which make the energe level in the surface duct increased. Two groups of measured data show that the mixed-layer depth may yield or fade suddenly with time and distribute asymmetrically with range. Under a thermocline enviroment in the shallow water, the acoustic energy level near the surface can be evidently raising when the surface duct comes into being in condition of some specific oceanographic phenomena in the air-sea boundary layer.
- mixed-layer /
- sound speed profile /
- surface duct channel /
- acoustic propagation /
- BELLHOP model

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参考文献(24)

URICK R J. Principles of Underwater Sound [M]. New York: McGraw-Hill, 1983: 79-162.

SCHULKIN M. Surface coupled losses in surface sound channels[J]. J Acoust Soc Am, 1968, 44: 1152-1154.

PEDERSEN M A, GORDON D F. Normal-mode theory applied to short range propagation in an underwater acoustic surface duct[J]. J Acoust Soc Am, 1965, 37: 105-118.

BAKER W F. New formular for calculating acoustic propagation loss in a surface duct[J]. J Acoust Soc Am, 1975, 57: 1198-1200.

HALL M. Surface-duct propagation: an evaluation of models of the effects of surface roughness[J]. J Acoust Soc Am, 1980, 67: 803-811.

ROBINSON A R, LEE D. Oceanography and Acoustics: Prediction and Propagation Models[M]. New York: American Institute of Physics, 1994: 50-79.

LUKAS R, LINDSTROM E. The mixed layer of the western equatorial Pacific Ocean[J]. J Geophys Res, 1991, 96(Suppl.): 3343-3358.

MONTEREY G I, LEVITUS S. Seasonal variability of mixed layer depth for the world ocean, NOAA NESDIS ATLAS 14[R]. Washington: U.S. Gov. Printing Office, 1997.

SUGA T, MOTOKI K, AOKI Y, et al. The North Pacific climatology of winter mixed layer and mode waters[J]. J Phys Oceanogr, 2004, 18: 89-106.

刘丽萍, 黄大吉, 章本照. 渤黄东海混合层化演变规律的研究进展[J]. 海洋科学进展, 2002, 20(3):84-89.

施平, 杜岩, 王东晓, 等. 南海混合层年循环特征[J]. 热带海洋学报, 2001, 20(1): 10-17.

芦静, 乔方利, 魏泽勋, 等. 夏季海洋上混合层深度分布研究——Argo资料与Levitus资料的比较[J]. 海洋科学进展, 2008, 26(2): 145-155.

张仁和. 浅海表面声道中的简正波声场[J]. 物理学报, 1975, 24: 200-209.

SPRINTALL J, TOMCZAK M. Evidence of the barrier layer in the surface layer of the tropics[J]. J Geophys Res, 1992, 97: 7305-7316.

王东晓, 杜岩, 施平. 南海上层海洋物理学气候图集[M]. 北京: 气象出版社, 2002.

LOCARNINI R A, MISHONOV A V, ANTONOV J I, et al. World Ocean Atlas 2005, Volume 1: Temperature, NOAA Atlas NESDIS 61 . In: LEVITUS S Ed. Washington: U.S. Government Printing Office, 2006: 1-38.

ANTONOV J I, LOCARNINI R A, Boyer T B, et al. World Ocean Atlas 2005, Volume 2: Salinity, NOAA Atlas NESDIS 62[R]//LEVITUS S Ed. Washington: U.S. Government Printing Office, 2006: 1-38.

王东晓, 杜岩, 施平. 冬季南海温跃层通风的证据[J]. 科学通报, 2001, 46(9): 758-762.

PORTER M B, BUCHER H P. Gaussian beam tracing for computing ocean acoustic fields[J]. J Acoust Soc Am, 1987, 82: 1349-1359.

JENSEN F B, KUPERMAN W A, PORTER M B, et al. Computational Ocean Acoustics[M]. New York: American Institute of Physics Press, 1994.

BUCKER H P. A simple 3-D Gaussian beam sound propagation model for shallow water[J]. J Acoust Soc Am, 1994, 95: 2437-2440.

WEINBERG H, KEENAN R E. Gaussian ray bundles for modeling high-frequency propagation loss under shallow-water conditions[J]. J Acoust Soc Am, 1996, 100: 1421-1996.

许东禹, 陈祁彦. 中国近海地质[M]. 北京:地质出版社, 1997.

HAMILTON E L. Geoacoustic modeling of the sea floor[J]. J Acoust Soc Am, 1980, 68: 1313-1340.

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文章访问数: 1644
HTML全文浏览量: 10
PDF下载量: 2484
被引次数: 0

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