The effect of a passage of land breeze front as a meteorological factor upon high concentration of NO
x was analyzed based on the observation data conducted during January, 1983 at Shinjuku Imperial Garden. At the passage of land breeze front, NO
x showed high concentration from the surface to a height of several hundred meter, and the region of this high concentration coincides with the head of land breeze. At surface level, NO
x concentration also shows quite similar pattern. However, NO
2 does not show a significant increase compared with NO
x, O
x concentration inside the land-breeze head was almost zero due to the reaction with NO. On the other hand, concentration of O
x above the level of 200 m showed several ten ppb, and the downward transport of O
x may be important at the upper boundary of land breeze head. The occurrence of high concentration of NO
x was correlated with the passage of the land breeze front, and the appearance time of peaks in NO
x inversely correlated to the N-S distance from the Tokyo Bay area.
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