Fig. 7: Future changes in freshwater content (FWC), sea surface height (SSH) and surface geostrophic current (SGC) speeds in high-resolution simulations.
From: Dominant inflation of the Arctic Ocean’s Beaufort Gyre in a warming climate
a–c Changes in (a) FWC, (b) SSH and (c) SGC between 1981–2000 and 2081–2100 in the simulation without wind corrections. d–f, The same as (a–c), but for the simulation with wind corrections. In the latter simulation, wind biases associated with the sea level pressure biases depicted in Fig. 8g are subtracted from the applied wind forcing.
