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Eddy can intensify solitary wave in andaman sea? 


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Eddies can indeed intensify solitary waves in the Andaman Sea. Research indicates that the interaction of internal solitary-like waves (ISWs) with eddies can lead to a potential 4-fold increase in ISW amplitude, forming stem-like structures under realistic oceanic conditions . Additionally, the presence of eddies can enhance the amplitudes of eastward-propagating ISWs generated from specific locations, such as the sill of the Great Channel, through constructive interference of internal tide generation . Furthermore, the generation of internal waves, including mode-1 and mode-2 ISWs, can be influenced by the impingement of internal tidal beams on critical bathymetry, nonlinear disintegration of internal tide modes, and lee wave forming mechanisms, all of which are associated with eddy interactions in the Andaman Sea .

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Papers (5)Insight
Eddies can intensify solitary waves in the Andaman Sea, potentially leading to a 4-fold increase in amplitude due to the development of stem-like internal solitary-like waves.
Journal ArticleDOI
A. R. Osborne, T. L. Burch 
02 May 1980-Science
699 Citations
Not addressed in the paper.
Open accessProceedings ArticleDOI
J. C. B. da Silva, J.M. Magalhaes 
19 Oct 2016
17 Citations
Not addressed in the paper.
Eddies are not discussed in the paper. The study focuses on the generation and propagation of internal solitary waves in the southern Andaman Sea due to bottom topography and tidal forcing.
Not addressed in the paper.

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Amplitude of the andaman's internal tide5 answersThe amplitude of internal tides in the Andaman Sea varies significantly. Studies show that the semidiurnal internal tides in this region can reach maximum isopycnal displacements of up to 46 meters. Additionally, the amplification of internal tides in the north-central Bay of Bengal, which is around 450 km away from their generation sites, has been observed with amplitudes comparable to those near the potential generation sites like the Andaman-Nicobar Ridge. The presence of large-amplitude internal waves in the Andaman Sea has been a known phenomenon since the nineteenth century, indicating the significant variability and impact of internal tides in this region.
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