With deep layer NW flow storms typically will not make it far into Auckland.David wrote:That is usually what happens. But I'm not too sure why it happens so often...MadDog wrote:I have been watching the thunderstorms approach Auckland from the NW. It seems as though the thunderstorms died out as they hit the coastline. Can anyone explain why they didn't make much ground inland?
The exceptions to the rule are if the storms are elevated or if there is a decent surface NE.
I think the hill country to the west is a big blocker as well as the cool land at this time of year. Also the instability numbers with these set is not very high and it doesn't take much to kill it off.