The Sensitivity of Characteristics of Large Scale Baroclinic Unstable Waves in Southern Hemisphere to the Underlying Climate

Table 1

Absolute sensitivity 𝑆_𝜎 as a function of zonal wavenumber 𝑘_𝑧 for different values of static stability parameter 𝜎₀.

𝜎0 m^2 Pa^−2 s^−2	Zonal wave number 𝑘𝑧
	1	2	3	4	5	6	7
1.0×10^−6	−0.0157	−0.1251	−0.4175	−0.9772	−1.8879	−3.2470	−5.2005
1.5×10^−6	−0.0157	−0.1245	−0.4139	−0.9675	−1.8794	−3.3014	−5.5927
2.0×10^−6	−0.0157	−0.1240	−0.4110	−0.9626	−1.8979	−3.4964	−6.9371
2.5×10^−6	−0.0157	−0.1234	−0.4088	−0.9629	−1.9509	−3.9665	−23.0031
3.0×10^−6	−0.0157	−0.1230	−0.4071	−0.9691	−2.0540	−5.3057