ON THE MECHANISM OF THE EFFECTS OF OZONE AND SEA SURFACE TEMPERATURE ON THE SUMMER ATMOSPHERIC FIELDS

By the use of a numerical model with global domain,three numerical experiments are conducted.Results show that the inclusion of O3 increases the heating rates at upper leves.It also influences the heating component of cumulus condensation.as well as the heating rates at the lower levels.The inclusion of the ocean mixing layer has directs effects on SST,mainly through the changes of the sensible heat flux and the evaporation amount.