TURBULENT-FLOW MICROSTRUCTURES OBSERVED BY SONAR

被引:10
作者
LHERMITTE, R [1 ]
LEMMIN, U [1 ]
机构
[1] ECOLE POLYTECH FED LAUSANNE,ECUBLENS,SWITZERLAND
关键词
D O I
10.1029/93GL00840
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
This note presents observations of sound wave backscattering in a turbulent water flow, conducted with a frequency scanning Doppler sonar working in a 0.5 to 5 MHz frequency band. The observed sound wave backscattering is attributed to temperature microstructures created by water turbulence. The backscattering intensity decreases systematically as a function of sonar frequency above 1 MHz and falls below detectability for sonar frequencies higher than a given value function of water turbulence intensity. This backscattering cutoff relates to the high wavenumber end, k(B), of the turbulent temperature spectrum. This k(B) estimate is found in excellent agreement with its theoretical calculation based on independent measurement of turbulence dissipation rate made using the Doppler observed velocity variance.
引用
收藏
页码:823 / 826
页数:4
相关论文
共 11 条
[1]  
Batchelor G K, 1957, S NAV HYDR NAT AC SC, P409
[3]   RST ANALYSIS OF MONOSTATIC AND BISTATIC ACOUSTIC ECHOES FROM AN ELASTIC SPHERE [J].
GAUNAURD, GC ;
UBERALL, H .
JOURNAL OF THE ACOUSTICAL SOCIETY OF AMERICA, 1983, 73 (01) :1-12
[4]   THE UNIVERSAL EQUILIBRIUM SPECTRA OF TURBULENT VELOCITY AND SCALAR FIELDS [J].
GIBSON, CH ;
SCHWARZ, WH .
JOURNAL OF FLUID MECHANICS, 1963, 16 (03) :365-+
[5]   ACOUSTIC SCATTERING FROM OCEAN MICROSTRUCTURE [J].
GOODMAN, L .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1990, 95 (C7) :11557-11573
[6]  
GRANT HL, 1961, J FLUID MECH, V12, P241
[7]  
LHERMITTE R, 1984, J ATMOSPHERIC OCEANI, V4, P293
[8]  
LHERMITTE R, 1990, GEOPHYS RES LETT, V10, P717
[9]  
Munk W. H., 1973, Boundary-Layer Meteorology, V4, P37, DOI 10.1007/BF02265224
[10]  
Tatarskii V., 1961, WAVE PROPAGATION TUR, P1