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A Case Study on the Development of an Elevated Subsidence Inversion Over a Surface Low Pressure System
2010
Journal of the Korean earth science society
This study presents the development of an elevated subsidence inversion over a surface low pressure system, which was formed along the Changma front or Meiu-Baiu front. The results of our analysis strongly suggest that the inversion is dissimilar to those formed in anticyclonic situations but is instead similar to the onion-shaped sounding found in wake low. The present analysis indicates that the observed elevated inversion resulted from the intrusion of stratospheric air associated with tropopause folding.
doi:10.5467/jkess.2010.31.5.531
fatcat:pmlvkednuvdwdhgqe7cn546wdy