As a follow-up study, the procedure in systematically perturbing the initial field is employed to examine the impact of perturbations collocated with the high and low ADSSV sensitivity on the model simulations. Results show that experiments with the perturbed initial conditions located at the high ADSSV signal (i.e., the midlatitude trough and the subtropical high) lead to more track deflection relative to the control run than experiments with perturbations in the nonsensitive area. The evolution of deep-layer mean steering flow and the comparison with the direction of ADSSV are also shown to interpret and validate its physical meaning. Furthermore, the effect of perturbations only in the sensitive vertical layers is investigated. It is indicated that perturbations within the sensitive layers grow as comparably as those in the thick-layer troposphere.
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