본 연구는 장기 해양관측(1966-1995)자료, 위성관측자료 및 수치모델기법을 이용하여 한국 남서해역에서 하계에 형성되는 조석전선괴 저수온역의 시공간적 변화를 파악하였다. 한국 남서 연안해역에서는 6월과 8월에 대흑산도~진도간 해역의 표면에서 주변 해역보다 2~3℃ 낮은 저수온역이 분포하면서 조석전선역이 형성됨을 확인할 수 있었다. 수온수평경도가 0.3℃/km 이상인 조석전선은 성층계수 2.0~2.5 범위이며, 0.03℃/km 이상인 저수온역은 성층계수 2.5~3.0의 범위와 일치하였다. 소조시에서 대조시까지 조석주기가 변하는 동안 조석전선의 위치변동은 전선은 25~75km, 저수온역의 범위는 60~90km로 조류의 세기에 정비례하여 이동 범위가 커지는 것으로 나타났다. 또한, 남서쪽 외해역으로 저수온역이 확장되는 원인은 진도 남서쪽으로 향하는 10cm/s 이상의 강한 조석잔차류에 의한 것으로 판단된다.

This study investigated the weather conditions, fine particle concentration, and ion components in PM2.5 when two cold fronts passed through Busan in succession on February 1 and 2, 2021. A analysis of the surface weather chart, AWS, and backward trajectory revealed that the first cold front passed through the Busan at 0900 LST on February 1, 2021, with the second cold front arriving at 0100 LST on February 2, 2021. According to the PM10 concentration of the KMA, the timing of the cold front passage had a close relationship with the occurrence of the highest concentration of fine particles. The transport time of the cold front from Baengnyeongdo to Mt. Gudeok was approximately 11 hours . The PM10 and PM2.5 concentrations in Busan started to increase after the first cold front had passed, and the maximum concentration occurred two hours after the second cold front passed. The SO4 2-, NO3 -, and NH4 + concentration in PM2.5 started to increase from 1100 to 1200 LST on February 1, after the first cold front passed, and peaked at 0100 LST to 0300 LST on February 2. However, the highest Ca2+ concentration was recorded 2-3 hours after the second cold front had passed.

This research investigated the characteristics of fine particles during cold front passage in Busan, on March 19, 2020. The cold front speed was 17.4 m/s (about 63k km/hr), moving from the northwest to the southeast, and with a width of about 64 km. The backward trajectory analysis showed that a southern sea air parcel flowed into Busan before the cold front passage, carrying continental materials from China transported into Busan after cold front passage. The PM10 concentration in Busan showed a rapid increase after passing through the cold front, with PM2.5 showing a high concentration during cold front passage. The PM2.5/PM10 ratio was 0.10 - 0.30. When the cold front passed, SO4 2-, NO3 -, Ca2+, NH4 +, Na+, and K+ in PM2.5 showed a rapid increase, with SO4 2- showing the most significant increase. These results indicated that understanding the characteristics of fine particles during cold front passage in Busan could provide insight into establishing a strategy to control urban air quality.