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.

• Kim, Kyung-Eak(Department of Astronomy and Atmospheric Sciences, Kyungpook National University)
• Ko, Hye-Young(Institute of Meteorological Research) | Ko, Hye-Young
• Heo, Bok-Haeng(Korea Meteorological Administration, Meteorological Advancement Council) | Heo, Bok-Haeng
• Ha, Kyung-Ja(Division of Earth Environmental System, Pusan National University)) | Ha, Kyung-Ja