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Title

temperature salinity andaman sea

Authors

Summary

s denty in salinity, of temperature, and variations The values the Bay of Bengal and the Andaman Sea depend largely on ht± omn, onal regime.Inwind, rain, and land drainage cause a year-round low-salinity surface layer to form.Toward the end of the northeawt monsoon, the surface waters in the Bay of Bengal ahA Andaman sea become warmer and more saline, reaching the year's maximum for temperature and salinity in May.A the the warm, highly coast of India, approaches the east southwest monsoon stratified surface layers cool, tumble, and mix thoroughly.Although rain sharply affects both the temperature and salinity of the surface layers, the greatest change in salinity occurs during the period of maximum river drainage in September and October.Thedisposition of the runoff-induced, low-salinity water varies according to the directicn of the monso

Keywords

salinity temperature, temperature variations, regimein addition, addition semienclosed, semienclosed geography, souththe, drainage year-round, year-round low-salinity, northeawt, maximum, southwest, thoroughlyalthough, september octoberthe, octoberthe disposition, disposition runoff-induced, directicn,

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