The Asymmetry of Subsurface Temperature Anomalies Associated with ENSO in the Equatorial Western Pacific
HUA Li-Juan1,2, YU Yong-Qiang1,*
Figure 3 Temperature anomalies averaged in the western Pacific Ocean 120#cod#x000b0;E-160#cod#x000b0;W and the corresponding climatological mean current for the top panels warm phase, middle panels cold phase, and bottom panels residual warm+cold in WSA left panels and SODA right panels units: #cod#x000b0;C. Units for the mean meridional currents V and vertical currents W are 1 and 0.0001 m s -1 , respectively.