ES23030Increased stratification intensifies surface marine heatwaves north-east of Aotearoa New Zealand in New Zealand’s Earth System model
We found that the main drivers of projected intensified surface marine heatwaves north-east of New Zealand are changes in the vertical distribution of heat transport and increased stratification, trapping heat near the ocean surface, and heat convergence within the region increasing in parallel with higher greenhouse gas emissions. This explains why the surface and shallow subsurface heating is projected to become more intense, and enables a more nuanced ecosystem vulnerability assessment in relation to marine heatwaves.
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