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Ambient Sound at Challenger Deep, Mariana Trench

机译:Mariana Trench挑战者深处的环境声音

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摘要

We present a record of ambient sound obtained using a unique deep-ocean instrument package and mooring that was successfully deployed in 2015 at Challenger Deep in the Mariana Trench. The 45 m long mooring contained a hydrophone and an RBR T pressure-temperature sensor. The hydrophone recorded continuously for 24 days at a 32 kHz sample rate. The pressure logger recorded a maximum pressure of 11,161.4 decibars, corresponding to a depth of 10,829.7 m, where actual anchor depth was 10,854.7 m. Observed sound sources included earthquake acoustic signals (T phases), baleen and odontocete cetacean vocalizations, ship propeller sounds, airguns, active sonar, and the passing of a Category 4 typhoon. Overall, Challenger Deep sound levels in the ship traffic band (20-100 Hz) can be as high as noise levels caused by moderate shipping, which is likely due to persistent commercial and military ship traffic in the region. Challenger Deep sound levels due to sea surface wind/waves (500 Hz to 1 kHz band) are as high as sea state 2, but can also be very low, equivalent to sea state 0. To our knowledge, this is the first long-term (multiday to week) broadband sound record, and only the fifth in situ measurement of depth, ever made at Challenger Deep. Our study indicates that Challenger Deep, the ultimate hadal (> 6,000 m) environment, can be relatively quiet but is not as acoustically isolated as previously thought, and weatherrelated surface processes can influence the soundscape in the deepest parts of the ocean.
机译:我们提供了使用独特的深海乐器套件和系泊系统获得的环境声音的记录,该记录系统于2015年在马里亚纳海沟的挑战者深处成功部署。 45 m长的系泊系统包含水听器和RBR T压力温度传感器。水听器以32 kHz采样率连续记录24天。压力记录仪记录的最大压力为11,161.4分贝,对应于深度10,829.7 m,其中实际锚定深度为10,854.7 m。观察到的声源包括地震声信号(T相),鲸鱼和鲸类鲸的发声,船螺旋桨声,气枪,声纳和第4类台风的通过。总体而言,挑战者在船舶通行频段(20-100 Hz)中的深声音级可能与适度运输引起的噪声级一样高,这很可能是由于该地区持续的商业和军事船舶通行。挑战者由于海面风/波(500 Hz至1 kHz频带)而产生的深沉声级与海态2一样高,但也可能非常低,相当于海态0。据我们所知,这是第一个长声态, Challenger Deep进行了长期(每天至一周)宽带录音,并且仅是深度的第五次现场测量。我们的研究表明,挑战者深处是终极的哈达尔(> 6,000 m)环境,它可以相对安静,但隔音效果却不像以前想象的那样,而且与天气有关的表面过程会影响海洋最深处的声景。

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  • 来源
    《Oceanography》 |2017年第2期|186-197|共12页
  • 作者单位

    NOAA, PMEL, Newport, OR 97366 USA;

    NOAA, PMEL, Newport, OR 97366 USA|Oregon State Univ, Cooperat Inst Marine Resources Studies, Newport, OR 97366 USA;

    NOAA, PMEL, Newport, OR 97366 USA|Oregon State Univ, Cooperat Inst Marine Resources Studies, Newport, OR 97366 USA;

    NOAA, PMEL, Newport, OR 97366 USA|Oregon State Univ, Cooperat Inst Marine Resources Studies, Newport, OR 97366 USA;

    NOAA, PMEL, Newport, OR 97366 USA|Oregon State Univ, Cooperat Inst Marine Resources Studies, Newport, OR 97366 USA;

    NOAA, PMEL, Newport, OR 97366 USA|Oregon State Univ, Cooperat Inst Marine Resources Studies, Newport, OR 97366 USA;

    NOAA, PMEL, Newport, OR 97366 USA|Oregon State Univ, Cooperat Inst Marine Resources Studies, Newport, OR 97366 USA;

    Univ Washington, Joint Inst Studies Atmosphere & Ocean, Seattle, WA 98195 USA;

    NOAA, PMEL, Engn Dev Div, Seattle, WA USA;

    NOAA, PMEL, Engn Dev Div, Seattle, WA USA;

    NOAA, PMEL, Engn Dev Div, Seattle, WA USA;

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