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How to identify internal solitary wave by using temperature logger? 


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Internal solitary waves (ISWs) can be identified using temperature loggers through various methods. The traditional approaches include the whole water column isotherm (WCI) method and the single isotherm (SI) method, with the novel temperature superposition (TS) method showing promising results . In situ observations of ISWs are crucial for enhancing nonlinear internal wave theories, but challenges arise due to the complex thermohaline data collected by underwater gliders. Glider data analysis, including estimating vertical water velocity and identifying wave packets, provides a basis for ISW observation using gliders . Additionally, ocean buoys equipped with systems like acoustic Doppler current meters can monitor ISWs in real-time, benefiting offshore activities like oil and gas development in the South China Sea . These methods collectively contribute to a comprehensive approach for effectively identifying and monitoring ISWs using temperature loggers and oceanographic instruments.

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Internal solitary waves can be identified using temperature loggers by observing sharp depressions in the near-surface pycnocline, often visible as alternating bands of slicks and rough patches.
Not addressed in the paper.
Identifying internal solitary waves using temperature loggers is challenging due to the mixed temporal and spatial scales in glider observations, hindering complete thermohaline stratification analysis.
Internal solitary waves can be identified using temperature loggers by employing methods like the temperature superposition (TS) method, which considers temperature across all depths to effectively detect these waves.
Not addressed in the paper.

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