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Diurnal Variability of Ambient Noise in Shallow Tropical Waters, South Western Bay of Bengal

机译:孟加拉西南湾浅热带水域环境噪声的日变化

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摘要

Ambient noise recorded at shallow southwestern Bay of Bengal during September 2010 has been analyzed for spectral characteristics in the band 0.1-5.0 kHz. The noise level (NL) exhibits diurnal periodicity in the band 0.5-2.0 kHz, during most of the day. The in situ wind data at the site correlates well with the NL, which also shows a diurnal cycle. Wavelet analysis further carried out establishes of the diurnal periodicity in wind/NL pattern during fair weather conditions under the influence of local wind effects. Wavelet coherence shows wind and noise to be in phase or wind leading noise. Diurnal variation in wind is more frequently observed along the coast in tropical regions due to differential heating of land and sea, and this has attributed to the NL pattern at the site. The period of measurement is also favorable for the formation of such localized circulation since it is the sunny unclouded period prior to the Bay of Bengal cyclone season and the northeast monsoon.
机译:已对2010年9月在孟加拉西南部浅湾记录的环境噪声进行了分析,以分析0.1-5.0 kHz频带内的频谱特征。在一天的大部分时间内,噪声水平(NL)在0.5-2.0 kHz频段表现出昼夜周期性。该站点的原地风数据与NL很好地相关,这也显示出昼夜周期。小波分析进一步建立了在晴天天气条件下,局部风效应影响下风/ NL模式的昼夜周期性。小波相干表明风和噪声同相或风向噪声。由于陆地和海洋的热量差异,在热带地区的沿海地区,风的昼夜变化更为频繁,这归因于该地点的NL模式。测量期也有利于这种局部环流的形成,因为它是孟加拉湾气旋季节和东北季风之前的晴天,没有阴天。

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