Abstract
Hydrographic changes in the NW Arabian Sea are mainly controlled by the monsoon system. This results in a strong seasonal and vertical gradient in surface water properties, such as temperature, nutrients, carbonate chemistry and the isotopic composition of dissolved inorganic carbon (δ
Original language | English |
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Pages (from-to) | 269-291 |
Journal | Global and Planetary Change |
Volume | 34 |
Issue number | 3-4 |
DOIs | |
Publication status | Published - 2002 |