Interdecadal variability in thermal structure of water in the upper active layer in the northwestern Pacific Ocean

Resumo

The self-oscillation process of heat redistribution in the system ocean–atmosphere–continent should be considered as one of the mechanisms of multidecade climate variability. Based on the data of monitoring for the period 1960–2014, interdecadal variations in heat capacity in the upper active layer are estimated for the northwestern part of the Pacific Ocean, which is one of the most informative regions of the World Ocean.