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- W2106335024 abstract "-2 ). In contrast, during winter, the upper thermohaline layer of the northeastern Arabian Sea exhibited colder sea surface temperature (SST, 25-26°C), and deeper mixed layer depth (MLD, >70 m). This area was distinguished by less oxygenated ( 2 µM) and high productive (surface - >10 mgC m -3 d -1 & column - >800 mgC m -2 d -1 ) waters. I can be stated that the physically forced chemical changes occurred in the upper layers of both southeastern and northeastern Arabian Sea, appeared in an oscillating manner with respect to monsoonal changes, seemed to trigger the enhancement of phytoplankton productivity of the area. (Keywords: Upwelling, Winter cooling, Nutrients, Chlorophyll a, Primary production)" @default.
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- W2106335024 date "2014-01-01" @default.
- W2106335024 modified "2023-09-23" @default.
- W2106335024 title "Oscillating environmental responses of the eastern Arabian Sea" @default.
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