I. Vilibić

Observational Evidence for Accelerated Warming and Salinification Propagating Into the Deep Mediterranean

Acceleration, rather than a gradual linear response, is emerging as a defining feature of ocean change in the Anthropocene. Surface‐forced warming propagates into the deep ocean over decades to centuries, but semi‐enclosed basins such as the Mediterranean Sea may respond more rapidly. Here, we analyse an in situ Medite...