Abstract
In general, the sea and land breezes are said to have a much effect on the heat island convection. The characteristics of sea and land breeze, however, depend much on daily larger scale conditions, such as the mesoscale pressure distribution. Thus it is needed to tolerate the local heat island phenomena. This study is, therfore, aimed firstly at investigating the existing sea and land breeze effect on the heat island phenomena in this area, and then at evaluating the effect of geostrophic wind on the convection.
