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Pattern Jarring January

This is interesting
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This is a solid analysis of the literal NAO index and it identifies a major problem with how it is computed. Unfortunately, a negative NAO in and of itself is analyzed over too broad of an area. The key is in the positioning of the ridging over Greenland and the tropospheric vortex.

See the examples below: in what is arbitrarily defined as an "east-based" negative NAO, the anomalies are located further east such that temperatures across the eastern U.S. are actually above-average even though the NAO is strongly negative! In the "west-based" negative NAO example, the blocking ridge over Greenland and trapped tropospheric vortex are further west, keeping a signature arctic tap straight from Alaska into the eastern and southeastern U.S.

Positional_NAO.png


In an analysis I did while working at the State Climate Office of NC I did find that the number of snow days where at least one station reported 1" or more of snowfall (excluding the mountains) increased by 25% in all El Nino winter months, and 2/4 La Nina winter months.

NAO_Interactions.png


If this same analysis was performed for west-based NAO regimes, I am confident the signal would be even stronger. And it is no surprise than in my big RDU snowstorms H5 analysis that the west-based NAO regime is clearly present. This is an important lesson to remember about climate pattern indices - not all regimes are created equal and just because a chart says an index is in a favorable phase doesn't mean the results are going to turn out as expected without further investigation.

http://climate.ncsu.edu/climate/patterns/nc-snowfall

1300,
Great response! In light of what you're saying about the NAO index sometimes being deceiving, I was wondering if you would please post H5 anomaly maps for these days, which are 5 days before some major SE snowstorms:

2/4/1967, 2/4/1973, 2/25/1980, 3/19/1983, 2/1/1984, 1/2/1988, 2/12/1989, 2/19/2015
 
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Amen ... ;)
Glad someone with cred is preaching what this idiot has been spouting for years ... :eek:

I agree. I don't "expect" anything in particular when an index is whatever. I use them as tools in combination with other indices to give me an idea of the tendencies. Example: a significantly higher % of +PNA days will be cold in the SE US vs that for -PNA days. Same could be said for -AO, -NAO, -EPO, and weak MJO phases on left side of chart. Does that mean any one day you look at has to work out this way? Not in the least. There are many exceptions. The indices should be used as guidelines rather than as crystal balls.
 
I agree. I don't "expect" anything in particular when an index is whatever. I use them as tools in combination with other indices to give me an idea of the tendencies. Example: a significantly higher % of +PNA days will be cold in the SE US vs that for -PNA days. Same could be said for -AO, -NAO, -EPO, and weak MJO phases on left side of chart. Does that mean any one day you look at has to work out this way? Not in the least. There are many exceptions. The indices should be used as guidelines rather than as crystal balls.
Damn, Larry,
I thought I might get the Bard pin ... exceptional and succinct post!
Best!
Phil
 
This is a solid analysis of the literal NAO index and it identifies a major problem with how it is computed. Unfortunately, a negative NAO in and of itself is analyzed over too broad of an area. The key is in the positioning of the ridging over Greenland and the tropospheric vortex.

See the examples below: in what is arbitrarily defined as an "east-based" negative NAO, the anomalies are located further east such that temperatures across the eastern U.S. are actually above-average even though the NAO is strongly negative! In the "west-based" negative NAO example, the blocking ridge over Greenland and trapped tropospheric vortex are further west, keeping a signature arctic tap straight from Alaska into the eastern and southeastern U.S.

Positional_NAO.png


In an analysis I did while working at the State Climate Office of NC I did find that the number of snow days where at least one station reported 1" or more of snowfall (excluding the mountains) increased by 25% in all El Nino winter months, and 2/4 La Nina winter months.

NAO_Interactions.png


If this same analysis was performed for west-based NAO regimes, I am confident the signal would be even stronger. And it is no surprise than in my big RDU snowstorms H5 analysis that the west-based NAO regime is clearly present. This is an important lesson to remember about climate pattern indices - not all regimes are created equal and just because a chart says an index is in a favorable phase doesn't mean the results are going to turn out as expected without further investigation.

http://climate.ncsu.edu/climate/patterns/nc-snowfall
Great post. Wonder if we’ll ever see a west-based -NAO in the heart of winter again in our lifetimes?
 
Supposed to hit 70 here Friday. I expect to see some wintry weather coming a week later.
 
I'm going to let the cat out of the bag a little here - I am pretty close to a climate change skeptic. I do not deny that some warming has occurred over the past 30 years, but I do not believe in the magnitude of change that is generally accepted, and I definitely don't believe that anthropogenic forcing is the primary driver. I have done research on the degree of warming in NC and it is less than half at non-urban locations as it is at rural sites like RDU. I struggle to see any significant correlations between a "warming Earth" and our current weather.

Why am I putting this unpopular, and very criticized, opinion out here in a discussion about the NAO?! Because to me, the lack of winter-time negative NAO regimes is probably one of the largest climate-related changes I see and I don't have an answer for it. Is it something about the change in ice cover over the Greenland region? Even in strongly negative winter-time AO regimes over the past 5 years the NAO really has not responded. There have been numerous occasions where NWP suggest a major negative west-based NAO episode only to greatly diminish it as verification nears. I do believe that something in the climate has shifted to cause the winter-time west-based neg. NAO to disappear, but I don't have the answer to what that is exactly.
I’m largely in your camp here. Regarding the wintertime -NAO, I haven’t heard any compelling rationale as to why we don’t see it much anymore other than having to do with climate change. I guess we have to blame it on that since there’s no other obvious reason. I don’t really like settling for that answer, but it’s also hard to accept that we’re just in an unprecedented period of bad luck. Something has to be causing it.
 
I’m largely in your camp here. Regarding the wintertime -NAO, I haven’t heard any compelling rationale as to why we don’t see it much anymore other than having to do with climate change. I guess we have to blame it on that since there’s no other obvious reason. I don’t really like settling for that answer, but it’s also hard to accept that we’re just in an unprecedented period of bad luck. Something has to be causing it.

I’m thinking the enormous amount of sea ice loss has something to do with it by disturbing the polar vortex.


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I'm on GW side of the coin as 1300m. In my opinion the reason why the west based Neg Nao( or any neg Nao for that matter) has been so absent is because of a lesser amount of sea ice in that region. However on the the Pacific side you have the same thing happening and the net effect is seeing the EPO behave the way it has. The EPO is in turn deflating and influencing the NAO even when you get stretches of neg AO. The NAO is downstream of the results being produced in the Pacific and even though a neg AO argues we should see a neg nao, the EPO signal trumps orverwhelms any neg AO trickle down effect. Hope that makes sense and just an opinion as to possibly why we don't see a neg nao due to the cycle we are currently in.
 
Looks like we need another mechanism to get deep snow in central NC.


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I'm going to let the cat out of the bag a little here - I am pretty close to a climate change skeptic. I do not deny that some warming has occurred over the past 30 years, but I do not believe in the magnitude of change that is generally accepted, and I definitely don't believe that anthropogenic forcing is the primary driver. I have done research on the degree of warming in NC and it is less than half at non-urban locations as it is at sites like RDU. I struggle to see any significant correlations between a "warming Earth" and our current weather.

Why am I putting this unpopular, and very criticized, opinion out here in a discussion about the NAO?! Because to me, the lack of winter-time negative NAO regimes is probably one of the largest climate-related changes I see and I don't have an answer for it. Is it something about the change in ice cover over the Greenland region? Even in strongly negative winter-time AO regimes over the past 5 years the NAO really has not responded. There have been numerous occasions where NWP suggest a major negative west-based NAO episode only to greatly diminish it as verification nears. I do believe that something in the climate has shifted to cause the winter-time west-based neg. NAO to disappear, but I don't have the answer to what that is exactly.

Enjoy your posts, they are very informative.

As your original post indicated the NAO is the single most significant feature that Raleigh depends on for big snows.

The last 5 6”+ events for Raleigh all had -NAO. Let’s hope climate change isn’t the cause of the recent period of +NAO winters, rather a long term cycle.

12/26/2010
02/27/2004
01/01/2002
01/26/2000
01/07/1996
 
I'm honestly not convinced it is entirely due to climate change. If it were, how did we go from one of the strongest west-based neg. NAO episodes ever in December 2010 to January 2011 to basically a non-existent NAO since then? It's hard for me to believe something that dramatic shifted from January 2011 onward related to the climate change issue that caused such a dramatic change in the NAO. I'm not saying it may not be contributing, and maybe there was a critical amount of Greenland ice cover that was surpassed after 2011 that has resulted in this - but for it to be so sudden and dramatic raises questions.
Yep, agree. It’s possible that a tipping point was reached, as you say, but I haven’t seen any research on it that has resulted in a definitive conclusion. Tipping points are hard to forecast and also hard to see in real-time. But they should be easier to identify in hindsight. Maybe someone will do a study on it someday.
 
Didn't we snap on Webb for just mentioning a warming background state, while these guys have a nice discussion on Climate change in the wrong thread? Fair is fair folks.. Take this discussion to the Climate Change thread.
 
Didn't we snap on Webb for just mentioning a warming background state, while these guys have a nice discussion on Climate change in the wrong thread? Fair is fair folks.. Take this discussion to the Climate Change thread.
I don't remember that happening exactly. It may have been a more lengthy conversation the other time, and once it gets too long off it can be an issue. If it happened then I'm not sure when.
 
I'm honestly not convinced it is entirely due to climate change. If it were, how did we go from one of the strongest west-based neg. NAO episodes ever in December 2010 to January 2011 to basically a non-existent NAO since then? It's hard for me to believe something that dramatic shifted from January 2011 onward related to the climate change issue that caused such a dramatic change in the NAO. I'm not saying it may not be contributing, and maybe there was a critical amount of Greenland ice cover that was surpassed after 2011 that has resulted in this - but for it to be so sudden and dramatic raises questions.

There's a considerable amount of interannual variability that masks long-term changes, and clearly in 2010-11 the major icelandic volcano eruption likely had a lot to do w/ why the -NAO was so incredibly impressive. The relationships wrt NAO/AO variability and extratropical volcanic eruptions are more elusive however it could be argued that the placement of the eruption in the context of the NAO changed the radiative budget of the stratosphere s.t. the circulation anomalies generated by persistent absorption of incoming solar radiation by sulfate aerosols (& thus warming of the lower-mid stratosphere) may have persisted and propagated down into the troposphere by the subsequent winter of 2010-11 over the far North Atlantic where the volcanic ash was most persistent and intense. Observing a dramatic change like this from year-to-year or even a large -NAO episode or multi-year/decade period w/ increasing negative regimes doesn't necessarily negate the long-term signal in the NAO attributable to AGW which is towards an increasingly positive regime as was the case during the Medieval Warming Period. The stout +NAO signal in the MWP completely reversed in the subsequent cooling period during the Little Ice Age. I think a substantial pathway wrt how the NAO responds to the climate has to do w/ background changes in ENSO behavior attributable to large-scale global temperature change on timescales of a few-several centuries or so. During warmer regimes in the Quartnerary period, the upper ocean warms more quickly than the deeper ocean, which increases the thermal stratification that suppresses stronger warm ENSO events as suggested by Kohyama (2017) (who presented on this at the AMS conference in Austin earlier today) and favors a La Nina mean background state. This La Nina mean state modulates the trajectory and placement of an extratropical Rossby Wave train that emanates from the mean convective center in the tropics s.t. a weaker Aleutian Low & stronger Icelandic Vortex/+NAO is favored during a NINA and vis versa. The warmer climate also pushes the extratropical storm track further north due to Hadley Cell expansion and on the whole is more conducive to poleward EP flux which strengthens the mid-latitude jet stream and the exit regions of the jet (which again is conducive to a stronger Icelandic Vortex).
 
Didn't we snap on Webb for just mentioning a warming background state, while these guys have a nice discussion on Climate change in the wrong thread? Fair is fair folks.. Take this discussion to the Climate Change thread.
Climate variability and weather aren't mutually exclusive especially on timescales beyond a few days or so, thus the +NAO climate change discussion is applicable to this thread.
 
Depending on the source, the first 8 days of this month have been -13 to -15 on the average here. Of course, today skewed it warmer some.

Unless it gets really warm, January will probably end up finishing below average.
 
Proof? Although I do sense some scarcasm

It's definitely going to warm up there's no doubt about that or sarcasm, big trough going into the west coast w/ a ridge over the eastern US, classic late winter NINA pattern. Not sure when or if we'll break it but not looking too good thru most of the rest of January after the next week or so which could yield another threat of snow/ice for the mid-south
 
Well in the mean time these 50s will feel nice the next few days. I’ve noticed the temps do seem to keep going lower the next few days. Was in the lower 60s yesterday now warmest is 57.


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This sounds good in theory, but winter 2009-10 also featured a strongly negative NAO for DJF, and as you know was the sixth coldest winter on record at RDU. I'm not saying your ideas are wrong, but I'm not sure that is the entire answer either. It still appears that through that period the NAO was able to sustain a negative state and that all went away after January 2011 in the winter. We've seen the QBO flip the NAO to negative in July of 2015 and a few other sporadic episodes, but not in the wintertime other than once, March 2013.
I never said nor implied it was the entire answer but it's a very substantial piece, the NAO stint in 2009-10 was aided by the combination of a NINO which amplifies the standing planetary wave train, EQBO that deters Rossby wave momentum deposition from crossing the equator into the other hemisphere and favors wave activity flux onto the winter Hemisphere, & also aids w/ instigating intraseasonal tropical convection which can trigger SSWEs thru Rossby Wave Trains, low solar activity and favorable preceding interannual ENSO variability (more La Ninas before the 2009-10 El Niño) which favors the build up of ozone in the global tropics and subtropics that can be then opportunistically transported poleward to trigger sudden warming events and prolonged tropospheric blocking regimes if accompanied by an El Niño that accelerates the Brewer Dobson Circulation. Not to mention a properly timed and placed wave train never hurts... Again, other than a few stints like 2009-10, 2010-11, & March 2013 the overwhelming majority of winters since the mid-late 1970s have featured positive or strongly positive NAOs and their frequency has generally increased with time, with this year poised to continue the long-term trend. A few or several big NAO winters for that matter don't negate the signal or somehow imply that the climate-NAO connection is crap and should be re-evaluated. Similarly, a few cold months or winters and/or large winter storms in a period dominated by warming and less frequent snowfall also doesn't suddenly mean we aren't warming anymore, but rather the cumulative probability of attaining the "preferred" proportion of above to below normal winters is lower the less time you integrate the distribution. The frequency distribution with the integration of more winters will asymptotically tend towards the actual, preferred climate state but this also doesn't mean that a 30-40 year period is fully representative of the full spectrum of climate variability in a particular background. However, a collection of neighboring stations with longer records is likely a better answer and/or NWP simulations which are capable of reproducing a large collection of winters tens of thousands of times over in a given climate and capture variation that's not explicitly shown in observations esspecially in a short period of record (30-40 years).
 
1f57bb925cb43246b846e42d68127572.jpg

This is our best chance for a board wide storm affecting the most people.


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Wow, didn't expect to see that this morning. Guess we have something to track again. Not sure if there's anything scientific about it, but it does seem when it hits near 70 around here in winter about a week later we get a shot at snow. Maybe the rubber band snapping back.
 
GFS has this storm Tues/Wed next week , a Brownsville TX special
 
Wow, didn't expect to see that this morning. Guess we have something to track again. Not sure if there's anything scientific about it, but it does seem when it hits near 70 around here in winter about a week later we get a shot at snow. Maybe the rubber band snapping back.
Snapping back just in time to give you another 1/2 inch!
 
No one has implied that the climate-NAO connection is crap. However, I am outright stating that I do believe that the sudden shift from relatively frequent stints of negative NAOs during winter months up until 2011 to shutting it off entirely is driven by something additional. I am fully aware that the NAO has been trending more positive since the 70s, after all I made this graph about 8 years ago.

NAO_Seasonal.png
The negative regimes really weren't all that frequent before 2011 either, the NAO was even more positive in the 1990s than it is now so the mechanism that's favoring these regimes has been around for a while and not just since 2011 as you're trying to suggest. We've seen a complete reversal of the AMO over the course of the last several decades yet the NAO continues to trend positive in the longer term consistent with the increasingly unfavorable bgd climate
 
1f57bb925cb43246b846e42d68127572.jpg

This is our best chance for a board wide storm affecting the most people.


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06z GFS squashes it to oblivion with this look, not that I buy it, but it then develops a late blooming coastal that throws moisture back into NE NC for a brief light albeit high ratio snow with an inch or two.
fff71cb4696204675631c4dc9ee80e06.jpg


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06z GFS squashes it to oblivion with this look, not that I buy it, but it then develops a late blooming coastal that throws moisture back into NE NC for a brief light albeit high ratio snow with an inch or two.
fff71cb4696204675631c4dc9ee80e06.jpg


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NW trend? :D
 
Euro is close to being on board also on next Tuesday/Wednesday..
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Other than the system for western sections of our region, no other game in town, this may be our best shot.... will need some things to come together perfectly to thread the needle but not out of the question. Just enough NS for cold but not too much to crush any s/w...who knows but at least it's something.

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I'm not suggesting it, the data clearly shows it. There were numerous neg. NAO winter months between 1996 and 2011, I count approximately 24. Since January 2011 there has been 2.
Actually January-March 2013, January 2014, & January 2016 all featured a negative NAO which is at least 5 months in that period. Of course you purposely left out the early-mid 1990s that I was referring to earlier wherein the winter mean NAO was clearly even more positive which skews the data to show more frequent -NAOs in the preceding period before 2011 and makes it look like there's something dramatically different in its overall behavior between 2011-12 to present and 1990-2011, which there's not...
 
Cmc again has snow for many in the western part of the southeast next Tuesday and Wednesday

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