IF you live in the Northeast and want warm wx...
Posted: Thu Oct 21, 2004 4:53 pm
Forget about it.
YET ANOTHER significant blocking episode likely to set up for the end of OCT.
The cutoff upper low off the east coast on D4 (Monday) should lift northward and eventually phase with PJ energy on WED developing huge and cold Newfoundland low by D7.
http://vortex.plymouth.edu/gifs/041021202811.gif
The development of the closed low will pump the downstream ridge toward Greenland and send the NAO negative. Notice the OMEGA-STYLE block located right above the 50/50 low indicative of a strong –NAO
http://vortex.plymouth.edu/gifs/041021203118.gif
Notice even out to day 10 how the REX Blocking pattern (and split flow) over the Northwest Atlantic remains in tact. This is a COLD PATTERN for the northeast and one that one would have to watch extremely closely for big trouble if this were the middle of winter or even DEC for that matter.
Here are the NAO ensembles which support the ECMWF’s interpretation
EXTREMELY cold times would be ahead for the EUS if we had a favorable east pacific signal, but since we don’t it’s a war of the teleconnetions w/ the PNA indicating the trough in the west and the strong PAC jet courtesy of the +EPO arguing for the development of the dreaded plateau high.
Why is the EPO positive? It’s the result of the positioning of the PV over eastern Asia into far western North America w/ ridging to the south of it over the North PAC. What happens is the height gradient increases over a shorter distance (note the tightly packed 500mb Isohypses over the north pacific near/west of the Aleutian Islands) resulting in the intensification of the jet over the north pacific-- You can see that clearly by taking a look at the length of the arrows on the 500mb plot above.
http://vortex.plymouth.edu/gifs/041021205808.gif
The central US will continue to be under the influence of the ridge for the time being, which will help to keep things near or above normal in that region through D10 but for the northeast, no such luck. Note the 5400m eights over the northeast on the D8-10 average valid at 0z on 10/31.
http://vortex.plymouth.edu/gifs/041021205951.gif
Bottom line, NO pronounced or long-lasting EUS warm up through the end of the month.
Now b/c im ambitious, well take a look even further out into NOV, where I believe two things will be critical to determining how things unfold.
1… +EPO / -PNA and strong corresponding PAC jet (as long as the SSTA profile doesn’t change on me during the month, which is something im afraid of happening). This results in a strong plateau high and downstream ridge over the EUS. Cool/stormy pattern in the west.
2… Frequently –NAO helping to keep the ridge suppressed in the east and warm-ups short lived.
The Eastern Pacific signal is in the most Jeopardy of changing. IF the warm water gets into the GOA during the middle to later half of the month and a cool pool forms northwest of Hawaii like NOV/DEC 2002 the trough will head right back into the EUS in the means since the PAC jet is choked off, and you get the tendency for a split flow and mainly +PNA.
Here are the verifications from 2002-03
http://www.cpc.ncep.noaa.gov/products/p ... x.2002.gif
Now compare that to the SSTA profile in OND-NDJ 2002-03. You should also check out the 1993-94 and 1986-87 set-ups, they are equally impressive.
http://www.longpaddock.qld.gov.au/Seaso ... 02/Oct.gif
http://www.longpaddock.qld.gov.au/Seaso ... 02/Nov.gif
ttp://www.longpaddock.qld.gov.au/Season ... 02/Dec.gif
http://www.longpaddock.qld.gov.au/Seaso ... 03/Jan.gif
The GFS ensembles show much of the same through NOV 5 w/ blocking over the North Atlantic that at times may extend into QUEBEC, Baffin Island and over the Davis Strait opposing the –PNA pattern and Pacific jet.
http://www.cdc.noaa.gov/map/images/ens/ ... times.html
Basic idea here is that November or at leas the first 15 days of the month should play out like I have said; it’s the later part of the month where things really begin to get interesting. ill elaborate more as time goes on.
YET ANOTHER significant blocking episode likely to set up for the end of OCT.
The cutoff upper low off the east coast on D4 (Monday) should lift northward and eventually phase with PJ energy on WED developing huge and cold Newfoundland low by D7.
http://vortex.plymouth.edu/gifs/041021202811.gif
The development of the closed low will pump the downstream ridge toward Greenland and send the NAO negative. Notice the OMEGA-STYLE block located right above the 50/50 low indicative of a strong –NAO
http://vortex.plymouth.edu/gifs/041021203118.gif
Notice even out to day 10 how the REX Blocking pattern (and split flow) over the Northwest Atlantic remains in tact. This is a COLD PATTERN for the northeast and one that one would have to watch extremely closely for big trouble if this were the middle of winter or even DEC for that matter.
Here are the NAO ensembles which support the ECMWF’s interpretation

EXTREMELY cold times would be ahead for the EUS if we had a favorable east pacific signal, but since we don’t it’s a war of the teleconnetions w/ the PNA indicating the trough in the west and the strong PAC jet courtesy of the +EPO arguing for the development of the dreaded plateau high.
Why is the EPO positive? It’s the result of the positioning of the PV over eastern Asia into far western North America w/ ridging to the south of it over the North PAC. What happens is the height gradient increases over a shorter distance (note the tightly packed 500mb Isohypses over the north pacific near/west of the Aleutian Islands) resulting in the intensification of the jet over the north pacific-- You can see that clearly by taking a look at the length of the arrows on the 500mb plot above.
http://vortex.plymouth.edu/gifs/041021205808.gif
The central US will continue to be under the influence of the ridge for the time being, which will help to keep things near or above normal in that region through D10 but for the northeast, no such luck. Note the 5400m eights over the northeast on the D8-10 average valid at 0z on 10/31.
http://vortex.plymouth.edu/gifs/041021205951.gif
Bottom line, NO pronounced or long-lasting EUS warm up through the end of the month.
Now b/c im ambitious, well take a look even further out into NOV, where I believe two things will be critical to determining how things unfold.
1… +EPO / -PNA and strong corresponding PAC jet (as long as the SSTA profile doesn’t change on me during the month, which is something im afraid of happening). This results in a strong plateau high and downstream ridge over the EUS. Cool/stormy pattern in the west.
2… Frequently –NAO helping to keep the ridge suppressed in the east and warm-ups short lived.
The Eastern Pacific signal is in the most Jeopardy of changing. IF the warm water gets into the GOA during the middle to later half of the month and a cool pool forms northwest of Hawaii like NOV/DEC 2002 the trough will head right back into the EUS in the means since the PAC jet is choked off, and you get the tendency for a split flow and mainly +PNA.
Here are the verifications from 2002-03
http://www.cpc.ncep.noaa.gov/products/p ... x.2002.gif
Now compare that to the SSTA profile in OND-NDJ 2002-03. You should also check out the 1993-94 and 1986-87 set-ups, they are equally impressive.
http://www.longpaddock.qld.gov.au/Seaso ... 02/Oct.gif
http://www.longpaddock.qld.gov.au/Seaso ... 02/Nov.gif
ttp://www.longpaddock.qld.gov.au/Season ... 02/Dec.gif
http://www.longpaddock.qld.gov.au/Seaso ... 03/Jan.gif
The GFS ensembles show much of the same through NOV 5 w/ blocking over the North Atlantic that at times may extend into QUEBEC, Baffin Island and over the Davis Strait opposing the –PNA pattern and Pacific jet.
http://www.cdc.noaa.gov/map/images/ens/ ... times.html
Basic idea here is that November or at leas the first 15 days of the month should play out like I have said; it’s the later part of the month where things really begin to get interesting. ill elaborate more as time goes on.