A brief review is made of some current sea breeze theories, with a view to answering some questions about sea breezes in Australia. It is concluded that no theory so far advanced is adequate satisfactorily to answer questions about the lateral extent of the circulations. A brief interim report is presented on some observations made last summer in the Kalgoorlie-Esperance area, which show rather conclusively that, on occasion, the seabreeze circulation extends iniand for at least 200 miles in a recognizable, although decadent, form.
R.H. Clarke (Thu,) studied this question.