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震測海洋學（英語：Sesimic oceanography）是聲測海洋學的一種形式。 … 震測海洋學（英語：Sesimic oceanography）是聲測海洋學的一種形式。用聲波研究海洋的物理特性和動力學。它能提供海水溫度和鹽度變化的圖像。震測海洋學使用頻率低於 500 Hz 的聲波，與大多數聲測海洋學的成像方法不同。它們使用頻率是大於 10,000 Hz 的聲波。這種使用低頻聲測的優點是它能夠提供高度詳細，廣而深的海洋結構圖像，其圖像水平距離跨越數百公里，以及圖像深度由海面延伸到海床。自 2003 年成立以來，震測海洋學已被用於對各種海洋現象進行成像，包括水體邊界(fronts)、 渦流、溫鹽階梯、混濁層 和冷甲烷滲漏。 除了提供壯觀的圖像外，震測海洋學還對諸如內波運動。和海水的湍流混合等過程提供定量分析數據。供壯觀的圖像外，震測海洋學還對諸如內波運動。和海水的湍流混合等過程提供定量分析數據。
, Seismic oceanography is a form of acoustic … Seismic oceanography is a form of acoustic oceanography, in which sound waves are used to study the physical properties and dynamics of the ocean. It provides images of changes in the temperature and salinity of seawater. Unlike most oceanographic acoustic imaging methods, which use sound waves with frequencies greater than 10,000 Hz, seismic oceanography uses sound waves with frequencies lower than 500 Hz. Use of low-frequency sound means that seismic oceanography is unique in its ability to provide highly detailed images of oceanographic structure that span horizontal distances of hundreds of kilometres and which extend from the sea surface to the seabed. Since its inception in 2003, seismic oceanography has been used to image a wide variety of oceanographic phenomena, including fronts, eddies, thermohaline staircases, turbid layers and cold methane seeps. In addition to providing spectacular images, seismic oceanographic data have given quantitative insight into processes such as movement of internal waves and turbulent mixing of seawater.al waves and turbulent mixing of seawater.
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Seismic oceanography is a form of acoustic … Seismic oceanography is a form of acoustic oceanography, in which sound waves are used to study the physical properties and dynamics of the ocean. It provides images of changes in the temperature and salinity of seawater. Unlike most oceanographic acoustic imaging methods, which use sound waves with frequencies greater than 10,000 Hz, seismic oceanography uses sound waves with frequencies lower than 500 Hz. Use of low-frequency sound means that seismic oceanography is unique in its ability to provide highly detailed images of oceanographic structure that span horizontal distances of hundreds of kilometres and which extend from the sea surface to the seabed. Since its inception in 2003, seismic oceanography has been used to image a wide variety of oceanographic phenomena, including fronts, ceanographic phenomena, including fronts,
, 震測海洋學（英語：Sesimic oceanography）是聲測海洋學的一種形式。 … 震測海洋學（英語：Sesimic oceanography）是聲測海洋學的一種形式。用聲波研究海洋的物理特性和動力學。它能提供海水溫度和鹽度變化的圖像。震測海洋學使用頻率低於 500 Hz 的聲波，與大多數聲測海洋學的成像方法不同。它們使用頻率是大於 10,000 Hz 的聲波。這種使用低頻聲測的優點是它能夠提供高度詳細，廣而深的海洋結構圖像，其圖像水平距離跨越數百公里，以及圖像深度由海面延伸到海床。自 2003 年成立以來，震測海洋學已被用於對各種海洋現象進行成像，包括水體邊界(fronts)、 渦流、溫鹽階梯、混濁層 和冷甲烷滲漏。 除了提供壯觀的圖像外，震測海洋學還對諸如內波運動。和海水的湍流混合等過程提供定量分析數據。供壯觀的圖像外，震測海洋學還對諸如內波運動。和海水的湍流混合等過程提供定量分析數據。
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震測海洋學
, Seismic oceanography
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