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Depth-resolved phytoplankton responses to persistent marine heatwaves in the southern tropical indian ocean
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DOI：10.1016/j.jag.2026.105323.png)
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Abstract
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• Extreme positive IOD events drive distinct vertical MHW structures. • Surface-intensified MHWs primarily reduce mixed-layer productivity. • Subsurface-intensified MHWs deepen the deep chlorophyll maximum. • Subsurface-intensified MHWs trigger 30% Chla rise via photoacclimation at 80–150 m.
Keywords:
Marine heatwaves
Vertical structure
Chlorophyll a
Particulate organic carbon
Tropical indian ocean
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