The Korea Meteorological Administration said recent heavy rainfall across South Korea does not constitute the official start of the summer monsoon season [1].
This distinction is critical for national disaster preparedness and agricultural planning, as the official monsoon typically signals a prolonged period of high-volume precipitation and humidity. The current weather pattern, while severe, is viewed as a precursor rather than the seasonal shift.
Heavy rains have already impacted several regions, particularly the southern coast and the East Sea coast. In Jeju’s mountainous areas and along the East Sea coast, rainfall exceeded 150 mm [1]. These totals occurred under a heavy-rain warning, driven by a low-pressure system and a stationary front combined with terrain-enhanced lift [1, 2].
Kang Hyemi, a forecast analyst for the KMA, said cold and dry air from the north will move south after June 21, 2024, pushing the stationary front further south [2]. Because of this atmospheric movement, the KMA said the current rains are not the start of the monsoon [2].
Adding to the complexity is the emergence of Typhoon No. 7, named Mekkhala [1]. The typhoon formed in the far southern sea and is currently being monitored by meteorologists. While not yet impacting the mainland, the KMA said Mekkhala could become a factor in modifying the eventual monsoon pattern [1, 2].
Local authorities continue to monitor the southern coast and Jeju as the atmospheric pressure shifts. The KMA's current assessment suggests the region is in a transitional phase before the primary summer rains establish a permanent presence over the peninsula [1, 2].
“The KMA said recent heavy rainfall across South Korea does not constitute the official start of the summer monsoon season.”
The KMA's refusal to declare the start of the monsoon despite heavy rainfall indicates a strict adherence to atmospheric criteria—specifically the stability and position of the stationary front. The presence of Typhoon Mekkhala introduces a volatile variable that could either accelerate the monsoon's onset or disrupt typical precipitation patterns, potentially leading to more erratic weather extremes for the region.



