Fig. 1: Results of initial COCO simulation.
From: Deep ocean mixing mismatch between model and observational estimates
a The meridional overturning circulation (MOC) in the global ocean. b The zonally averaged distribution (left) and vertical profile (right) of potential temperature bias in the global ocean. c The same as (b) but for salinity bias in the global ocean. d–f The same as (a–c) but in the Atlantic Ocean. g–i The same as (a–c) but in the Pacific Ocean. j–l The same as (a–c) but in the Indian Ocean. Counter intervals are 2 Sv (106 m3s−1) for MOC. The units for temperature and salinity are °C and ‰, respectively. Results with the vertical diffusivity of T00 (Tsujino et al. 2000) are shown here.
