Seasonal Variation in Radon Concentration in the Atmosphere Simultaneously Measured in Donghae on Korean Peninsula, Matsue on Shimane Peninsula, and Oki Island in the Sea of Japan

Abstract

We measured simultaneously radon concentration in the atmosphere at Donghae, Oki Island and Matsue. In Donghae, radon concentration had peaks in the winter and summer and lower values in the spring. It was the highest in the winter and lowest in the summer in Oki Island, in Matsue, the highest in the fall and lowest in the summer. The timing and frequency of arrival air mass from the ocean and the land were different among the three measuring points. The highest values in Donghae and Oki Island were because of effects of radon flow from Eurasian continent in the winter. The inversion layer often formed in the atmospheric boundary layer over the land area around the Sea of Japan caused the peak values in the summer in Donghae. The atmosphere over Oki Island is always mixed with that over the ocean because the island is small. Radon escaping from the ground of the island does not stay with the surface layer even at night; therefore, diurnal variation was almost none throughout the year. Air mass with low radon concentration coming from the Pacific Ocean caused the lowest values in the summer. In Matsue, the peak was found in the fall in which occurrences of surface inversion layer is most common in the year.