Location: West Coast Road, Manukau Peninsula, North Island
Unread postby Manukau heads obs »
there is a stable layer about half way up, and then it broke through that
so the updrafts are probably not extending enough verticaly through over enough length at a good speed to fire up lots of static charge for lightning....good theory?
That website is coming down one day soon for an upgrade.
What is a cb - cumulus buildup or what?
A cb is a cumulus buildup that has managed to grow high enough to glaciate and form a shower. Glaciation is the icing process that is typical of rain clouds.
The Sunday Star Times Lightning map show we had, for the week ending
9am Saturday 29 April 2006 we had, in and around New Zealand, 18,680 lightning cloud to ground discharges!
I saw a grand total of 6 ...grrrrrrr...!
Thanks for that explanation, NZ Storm. If further websites helping learners (am I the only one?) become available would be very grateful if you would post details.
agingaquarian wrote:Thanks for that explanation, NZ Storm. If further websites helping learners (am I the only one?) become available would be very grateful if you would post details.
Although orgionally made for christchurch Im sure the same principals can be used for Auckland or where ever you are. Made it for a friends Dad while back to do abit of Basic home forecasting.
for the week ending
9am Saturday 29 April 2006 we had, in and around New Zealand, 18,680 lightning cloud to ground discharges!
I saw a grand total of 6 ...grrrrrrr...!
Interestingly, the Met Service lightning detector only picks up the strikes on the earth(land or sea). For every earth strike, there is on average about 3 intercloud strikes. So the real total is ....get the calculator out!
But most of the lightning that occurs in the NZ region occurs over the sea
agingaquarian wrote:Thanks for that explanation, NZ Storm. If further websites helping learners (am I the only one?) become available would be very grateful if you would post details.
The Sunday Star Times Lightning map show we had, for the week ending
9am Saturday 29 April 2006 we had, in and around New Zealand, 18,680 lightning cloud to ground discharges!
I saw a grand total of 6 ...grrrrrrr...!
The lightning location system is one of the most up todate in the world.
It will pick up cloud to cloud lightning, but I understand not as well as cloud to ground lightning.
From memory, the efficiency for detecting CG strokes is about 95% to a location accuracy around 500m metres.
There are two ways of fixing a stroke location. One uses the radio signal (spheric) which has a characteristic discharge shape to determine a direction. Other antennas are then triangulated to determine a point of origin for the signal. The second method uses the time of arrival of the signal at a number of antennas. This can also determine a point of origin too. Then both determinations are then combined to give the final location.
Cameo1 wrote:
9am Saturday 29 April 2006 we had, in and around New Zealand, 18,680 lightning cloud to ground discharges!
I saw a grand total of 6 ...grrrrrrr...!
Your lucky!
The only lightning I've seen recently have been the static electricity as I take my jersey off in the dark over my head
Cameo1 wrote:
9am Saturday 29 April 2006 we had, in and around New Zealand, 18,680 lightning cloud to ground discharges!
I saw a grand total of 6 ...grrrrrrr...!
Your lucky!
The only lightning I've seen recently have been the static electricity as I take my jersey off in the dark over my head
JohnGaul
NZTS
Thanks for the laugh John before I head off to bed.
Manukau heads observer wrote:gee, you are always further east than i imagine, their, foggy, in hamilton
You Aucklander's are also so much more west than I imagine!
For comparison.. Hamilton's on the same longitude line with the most eastern point on Waihake Island.. and Raglan is on the same easting with Waitakere.