Djmiles
Barndoor Holroyd
Just outside of Aberystwyth , even the sheep have pacamacs .
I’m going to take a guess at....BORTH
Just outside of Aberystwyth , even the sheep have pacamacs .
I’m going to take a guess at....BORTH
Jesus I’m not that lucky , that’s quite cosmopolitan compared to Llanbadarn-fawr
Hi mate,
This area of netweather might be useful to have a browse through, I think it should cover all of your questions:
https://www.netweather.tv/forum/forum/69-learners-area/
A quick one on these questions :Uppers. Toppling heights. Northerly blocking. Zonality. What is the Polar Vortex and what does it 'do'? That sorta thing really.
So when someone mentions uppers they are talking about the temperature that's at 850HPa, i.e. around 2 miles (I think that's right? Papa?).
Northerly Blocking is a term which is ideally what we need to see to get any cold weather our way. Our default weather pattern is from the West (as it is across the whole northern Hemisphere) however when we get Northerly Blocking, that means there is a high pressure over the Pole (or ideally over Greenland) which "blocks" the westerly flow of weather for us and starts turning weather to come in from the East or North East.
Generally in winter this is coming off a huge landmass so is (normally) bitterly cold and we tap into that. This is where we get the "Beast from the East" saying and generally the direction we get most of our snow.
The Polar Vortex is the killer of any cold weather in Winter! This is a huge body of extremely cold airmass from the troposphere (where clouds form) to the Stratosphere (up to the edge of space) which forms normally from September through to Feb/March due to lack of sunlight over the pole. Temps can get down to -90, so with this in place and our much milder temps over the equator and north of there, where these two airmasses meet, is where you get the jet stream. The jet stream is the dividing line between Cold airmass and milder/warmer airmass.
In winter if you want snow, you want the jet stream to head south over the Med or spilt out in the Atlantic, vice versa in summer you want it over Iceland!
Along this jet stream/boundary is where you get (generally) the Low pressures form. The faster the jet stream (if a big temp differential between the two airmasses), the bigger/windier Low Pressures form. If the jet stream is anywhere near the British Isles (which it usually is) then those low pressures go either through us or just to north.
However the Polar Vortex can be "attacked" so to speak what what's called wave 1 and wave 2 formations (these are high pressures around the Northern Hemisphere). These pump milder air into the Artic which can disrupt the Polar Vortex from being so cold and actually warm it up a little. When this happens the temp differential becomes less which reduces the strength of the jet stream, which in turn means less strong Low Pressures and it allows the jet to meander. This in turn could allow High pressure to form over us or further North/East.
A SSW basically kills the Polar Vortex in Winter and all that cold air is forced outwards to our latitude around the Northern Hemisphere, which in turn sometimes means we have a cold spell (like it did back in Feb/March).
So for weather nerds who want snow, a SSW is the Holy Grail! Next best thing is some blocking to our North/North East to get some snow.
Sorry for rattling on, but just wanted to get some points across! haha! Hopefully Papa can verify what I've said, but do have a look at that learning area, it is very useful. )