Ma Barry B, Nystuen Jeffrey A, Lien Ren-Chieh
University of Washington, Applied Physics Laboratory, 1013 NE 40th Street, Seattle, Washington 98105-6698, USA.
J Acoust Soc Am. 2005 Jun;117(6):3555-65. doi: 10.1121/1.1910283.
Wind and rain generated ambient sound from the ocean surface represents the background baseline of ocean noise. Understanding these ambient sounds under different conditions will facilitate other scientific studies. For example, measurement of the processes producing the sound, assessment of sonar performance, and helping to understand the influence of anthropogenic generated noise on marine mammals. About 90 buoy-months of ocean ambient sound data have been collected using Acoustic Rain Gauges in different open-ocean locations in the Tropical Pacific Ocean. Distinct ambient sound spectra for various rainfall rates and wind speeds are identified through a series of discrimination processes. Five divisions of the sound spectra associated with different sound generating mechanisms can be predicted using wind speed and rainfall rate as input variables. The ambient sound data collected from the Intertropical Convergence Zone are used to construct the prediction algorithms, and are tested on the data from the Western Pacific Warm Pool. This physically based semi-empirical model predicts the ambient sound spectra (0.5-50 kHz) at rainfall rates from 2-200 mm/h and wind speeds from 2 to 14 m/s.
海洋表面风雨产生的环境声音代表了海洋噪声的背景基线。了解不同条件下的这些环境声音将有助于其他科学研究。例如,测量产生声音的过程、评估声纳性能,以及有助于了解人为产生的噪声对海洋哺乳动物的影响。利用声学雨量计在热带太平洋不同公海区域收集了约90个浮标月的海洋环境声音数据。通过一系列判别过程,识别出了不同降雨率和风速下的独特环境声音频谱。以风速和降雨率作为输入变量,可以预测与不同声音产生机制相关的声音频谱的五个分区。从热带辐合带收集的环境声音数据用于构建预测算法,并在西太平洋暖池的数据上进行测试。这个基于物理的半经验模型预测了降雨率为2至200毫米/小时、风速为2至14米/秒时的环境声音频谱(0.5至50千赫)。