Figure 7
From: Role of subsurface ocean in decadal climate predictability over the South Atlantic
(a,b) Year-to-year variations of the detrended subsurface ocean temperature tendency anomalies (in 10−7 °C s−1) averaged over the SEAO region (black box in Fig. 1c) from the CTR and 3DVAR experiments, respectively. (c,d) Same as in (a,b), but for the contributions from convergence anomalies of the horizontal heat transport (in 10−7 °C s−1) to the total temperature tendency anomalies. (e,f) Same as in (c,d), but for the contribution from convergence anomalies of the meridional heat transport (in 10−7 °C s−1) to the total temperature tendency anomalies. (g,h) Same as in (c,d), but for the contribution from the residual heat transport (in 10−7 °C s−1). The maps were generated using Grid Analysis and Display System (GrADS) Version 2.1.a3 (http://cola.gmu.edu/grads/downloads.php).
