Changes in the Austral Winter Hadley Circulation and the Impact on Stationary Rossby Waves Propagation
Figure 1
Zonal mean variables for strong, normal, and weak HC cases: (a) meridional wind (ms−1) at 200 hPa, (b) zonal wind (ms−1) at 200 hPa, (c) omega (Pa/s) at 500 hPa, and (d) divergence (×10−6 s−1) at 200 hPa.
