will be indicated by the falling of the barometer reading, shortly followed by a rapid decrease as the storm approaches, as well as a long swell originating from the direction of the centre, and an ugly appearance of the sky.
Iyakubonakaliswa ngokuwa kwebharometa, kancinci emva koko kulandelwe ngokuhla okukhawulezileyo xa isichotho sisiza, nangokusibekela okusuka ngasembindini, nokubi besibhakabhaka obuye buvele.