๐—๐—ผ๐˜‚๐—ฟ๐—ป๐—ฎ๐—น ๐—ผ๐—ณ ๐—”๐˜๐—บ๐—ผ๐˜€๐—ฝ๐—ต๐—ฒ๐—ฟ๐—ถ๐—ฐ ๐—ฆ๐—ฐ๐—ถ๐—ฒ๐—ป๐—ฐ๐—ฒ ๐—ฅ๐—ฒ๐˜€๐—ฒ๐—ฎ๐—ฟ๐—ฐ๐—ต | ๐—ฉ๐—ผ๐—น๐˜‚๐—บ๐—ฒ ๐Ÿฌ๐Ÿณ | ๐—œ๐˜€๐˜€๐˜‚๐—ฒ ๐Ÿฌ๐Ÿฎ | ๐—”๐—ฝ๐—ฟ๐—ถ๐—น ๐Ÿฎ๐Ÿฌ๐Ÿฎ๐Ÿฐ

 ๐Ÿ’  Kelvin Wave Propagation over a Sloping Interface and Relationships with El Niรฑo Southern Oscillation

๐Ÿ‘‰ Internal Kelvin Wave (KW) propagation is studied about variations in the sea surface temperature anomaly (SSTA) over the tropical Pacific. 

#Kelvin_Wave_propagation #Pycnocline_depth #Sea_surface_temperature #El_Niรฑo_Southern_Oscillation

๐Ÿ”— DOI: https://doi.org/10.30564/jasr.v7i2.6228

✉ Email: jasr@bilpubgroup.com

๐Ÿ‘ฉ‍๐Ÿ’ผ Managing Editor: Lesley Lu









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