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Freddofrog said...
In summer it's called a land breeze, so yes opposite of a seabreaze.
After sunset, land cools faster so air above land sinks. Ocean cools slower so relatively speaking is warmer than the land so air above the ocean rises. The air descending over land moves towards the ocean to fill the void left the the rising ocean. That's where you get your easterlies from.
This is a localised effect and has very little to do with pressure systems.
In winter the landbreeze effect doesn't happen so any easterly are due to pressure systems.
Strongest land and sea breezes are when there is greater temp differences between land and sea. When they are similar, eg after a week of 35C, you get very still days. No good for kiting but awesome for evening beach bbqs.
The theory is good except land cools slower than sea and also heats up slower. The morning easterlies are because the land temperature is lower than the sea temp and stops when the land starts heating up. Air will always move from cool to hot due to hot air rising and the cold air moving in to replace on the land/ocean surface.
You find that when you don't get a sea breeze in simmer is because there is no low sitting in the top of WA and a high in the bight. This means a really strong high pressure system is sitting in the bight and it therefore counteracts the sea breeze in the afternoon. A low at the top of WA helps bring on s stronger arvo sea breeze.