Research Article

Twentieth Century Winter Changes in Southern Hemisphere Synoptic Weather Modes

Table 2

Periods 𝑇 𝑑 π‘Ÿ and growth rates πœ” 𝑑 𝑖 of selected modes for the 1949–68 NCEP/NCAR basic state with standard parameterizations ( 𝐾 ξ…ž 𝑑 = 2 . 3 3 8 Γ— 1 0 1 6 m4 sβˆ’1, 𝑄 𝑑 𝐹 = 1 5 0 0 K, 𝐢 𝑑 𝐹 = 5 Γ— 1 0 βˆ’ 4 K mβˆ’1), their mode number, and class of mode. Also shown are the largest pattern correlations 𝐴 𝑐 between a given mode and the modes for the 1997–2006 NCEP/NCAR basic state with standard parameterizations and the 1997–2006 mode for which the pattern correlation is largest as well as the change in the growth rate Ξ” πœ” 𝑑 𝑖 .

Class Mode 𝑇 𝑑 π‘Ÿ πœ” 𝑑 𝑖 𝑇 𝑑 π‘Ÿ πœ” 𝑑 𝑖 𝐴 𝑐 Mode Ξ” πœ” 𝑑 𝑖
1949–68(days)(dayβˆ’1)(days)(dayβˆ’1) 1997–2006 

SH cyclogenesis11.200.42501.330.26630.896012βˆ’37.3%
ML blocking306.110.25666.270.20740.639926βˆ’19.2%
HL blocking87.400.34958.010.35000.76445+0.1%
HL blocking115.220.31844.990.30600.80286βˆ’3.9%
NWCB438.010.21007.970.30540.63747+45.4%
Antarctic613.080.362420.00.38100.90713+4.9%
Antarctic2652.10.2746 ∞ 0.28500.647510+3.8%
ISO5759.00.144425.40.18860.574433+30.6%
African EW224.140.28813.860.30350.76388+5.3%