Fig. 2From: Potential impact of sea surface temperature on rainfall over the western PhilippinesClimatological monthly 850 hPa level winds (m s−1) from 1982 to 2012 over domain 2, calculated by the CTL simulation (d–f) and compared with the JRA55 (a–c). Monsoon strength, denoted by the zonal wind component, is shown as shaded contours in the figureBack to article page