Simple analysis of about fifteen years of monthly total ozone data in
the light of associated meteorological processes has been carried out
in the tropical and subtropical regions of northern hemisphere. A well
marked trough in total ozone has been observed in July and August ove
r the most humid part of the region, which comes under the influence o
f monsoon circulation. It appears that the occurrence of the trough ma
y be due to the lifting of air mass by the intense convective activity
over areas of the low level convergence, which is fed normally from t
he equatorial belt. Also, the possible occurrence of stratospheric fou
ntain due to the existence of the coldest air around the tropopause ov
er the entire Southeast Asia and adjacent west Pacific ocean, may be p
laying some role to produce this feature.