Aanlysis has been made of the features of temperature and pressure fields with respect to sea/land breezes along the coast of South China during May, 1978. It is shown from the analysis that the vector of sea/land breezes is approximately perpendicular to the isolines of temperature and pressure anomalies, pointing from the cold high to the warm low. Both temperature and pressure have the greatest gradients along the coastal area with sea/land breezes reaching the maximum. The transitional period from the building-up of temperature and pressure fields with respect to sea/land breezes to the formation of the latter is very brief. It is found that sea/land breezes have an abating effect on the temperature and pressure fields, thus setting a limit to their own development. It is also found that the convergence field due to sea/land breezes is closely related to the center of precipitation along the coast of South China.
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