Just having a look back through my pics, I've been through two of these dry line type ones come to think of it. With the first one a good thunderstorm formed but quickly went offshore and me and Steven Graham only got to see a little of it as it went by quickly. That was on the 21st December 2004. We got to see another Cb form which it then went into a small storm with 5 or 6 lightning flashes and then it dissapated only giving very brief rain. Isobar map for this day at 1pm attached.
The second was on the 7th Jan 2005. There was some initial development that looked good near Glentunnel and it went to a small Cb but then dissapated giving not much rain at all. Picture below.
Another two nice looking clouds formed but they didn't get anywhere, one of which is in that photo comp, this one:
http://www.weatherforum.org.nz/forum/do ... hp?id=1019
Looking at the first situation wunderground shows that at 2pm/3pm the dewpoint went from 12 C to 4C so that shows the NW finally coming through, so yes I think this was a dryline type one.
Then with the second situation (7th Jan 05) the NE stuck around at the NZCH AWS, but here:
http://www.nrfa.org.nz/fire_weather/wea ... 050107.jpg
you can see that it was NW inland which it was when I was out there.
I think in the first instance there was too much mixing of the air after the first storm at the surface resulting in lower dewpoints than what the NZCH AWS said of 12 C, the representation in terms of instability could've been only around 8 or 9 C? Upper cold air could've been another factor in terms of it not being cold enough but I think it was ok, the thunderstorm in the morning showed that. The second storm that was weak (will post pic tomorrow) was so I think because of the lower moisture at the surface overall. In the second situation there was a lack of cold upper air as the NE was doing well so there would've been a good boundry there, just no instability in the upper levels to support it.
There was great storms in Otago on the 7th Jan formed by the same dryline principal but upper air was colder so storms formed much better!
I got caught out on the day of that Timaru funnel NZstorm so now I know this stuff I'll know for next time!
Bahh! I rambling on but find it fun to learn about this stuff!
Cheers.
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