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Hyun Mee Kim
and
Byoung-Joo Jung

regions of PV gradient changes sign, and the final SV maximum is also collocated with the regions of maximum PV gradient ( Fig. 13b ). To understand the dynamical mechanisms associated with large sensitivities in the lower level in the midlatitude, lower level temperature superposed on streamline at 850 hPa ( Fig. 14a ), and frontogenesis ( Fig. 14b ) and vertical wind ( Fig. 14c ) at 950 hPa superposed on MSLP, are shown. At the initial time of EXP1, a large low-level baroclinic zone and a front were

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