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4 hours ago, Volcanic Winter said:

I have to mention @psuhoffman because he demonstrated with clear data on the M/A forum how in the 20th century we snowed frequently in the previous -PDO cycle with a predominantly negative PNA. In order to accomplish that we needed -NAO blocking (basically a favorable Atlantic) that would overcome a hostile Pacific and produce snow, and it did. Granted there will be some differences between the DC area where he focuses and NYC, of course. But the general theme was pretty clear that the PNA wasn’t historically a death knell for east coast winters, and it’s concerning that it’s beginning to be. 
 

I think logically a chunk of that is temperature climo, we’re warming and missing borderline events that may have been mild to moderate events in colder decades. That’s just my thoughts on it, not his. It’s probably more complicated. 

But I found his presentations and analyses compelling and grounded in observable fact. It’s more the conclusions that are open to interpretation. Hopefully it’s just “bad luck” worsened by decadal warming. 

It’s a good observation. -PNA and +AO patterns of the 1950s and 1960s didn’t have the SE Ridge. So those patterns were colder and snowier than what we have been getting recently. The Gulf Stream is much warmer and pumps the SE Ridge.

11F1A3C1-F356-4695-A8BC-1804F20C9681.png.81cdb404ca4044bd005dc5cc89b7c6f0.png
F921EA6D-5702-48D1-96BC-B89A751B2BE9.png.b9f8f38e877315170a6cde9d8213aeb0.png

624875BD-EC24-4FD4-B8DC-F26FA674245D.png.ac8e5b38f6dff4aedfb885bf21789907.png
 

 

 

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The next 8 days are averaging    57degs.(49/66) or +7.

Reached  52 here yesterday at 11:30pm.

Today:    64-69, wind e. to s., increasing clouds, 52 tomorrow AM.

50*(82%RH) here at 7am.     53* at 8am.      56* at 9am.      58* at Noon.       60* at 1pm.      Reached 63* at 3pm.        60* at 4pm.      57* at 5pm.

NB.  Average April  53.7

         Record April   57.9[+4.2] in 2010.

Using GFSEns. for the next 16 days  gives 58(49/67) or +6---a record pace---(already +3.7).      April looked BN on some LR outlooks and ended up Too Close to Call.

Clear sailing except near the 9th.

1680588000-OrqkwjkOY04.png

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Will be interested to see if the Mets wimp out and postpone Thursday or not...models have not budged from a 4-6pm arrival on that front really which is late enough to not impact the starting pitcher but the Yanks canned opening day last year 24 hours out given the open date available as is customary...could see Mets just doing the same.  I'm not sure why the Euro seems so enthused with convective potential relative to other models.  I am not impressed with the instability overall

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The March -2.35 -PDO was the lowest in March since 1956 when the reading was -2.93. March 2009 was the last time below -2 in March at -2.06. Near record trough along the West Coast driving the SST pattern. So these are the warmest SSTs anomalies near the coast of South America in March for such a cold PDO.

https://www.ncei.noaa.gov/pub/data/cmb/ersst/v5/index/ersst.v5.pdo.dat

41DC461A-5072-47EA-955D-6C6DDDCEA7CA.png.067c3d2d8b056f72adc9e4de6754d70f.png

90B34184-EFB0-48D5-A81A-D23E0C3DC9B9.png.44c87d3e44095c18edd5e0f182afb0ce.png

2F6407BB-05AD-4869-95B3-7064BA477570.png.937d66ca305ad298d0dd5e3888e92385.png

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Its hard to say if the NATL SSTs are solely responsible for that change though, there may be some other factor we just are not aware of which is leading to it.  I know many in the meteorology world argue that SSTs really do not impact atmospheric heights and that its an overblown theory...we see this in the GOA every year when the argument breaks out whether its the chicken or the egg

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21 hours ago, BucksCO_PA said:

5/21/1992:

Indian Mills, NJ

High 88 / Low 28

Millville, NJ

High 82 / Low 30

ACY (Pomona, NJ)

high 84 / Low 28

some of those are truly mindblowing I didn't know it was possible in our area to have temps near 90 during the day and in the 20s at night....anything like this from Westhampton (FOK) or Marthas Vineyard (MVY)..... those are the other two places I know of that radiate really well.

I don't see Toms River in here (MJX) either, which I thought they would be

 

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12 hours ago, Stormlover74 said:

Up to 9

 

FB_IMG_1680569011247.jpg

8.... that last one says straight line winds

Breaks the record of 7 in one day for NJ from the notorious and lethal outbreak from November 16, 1989 that I remember so well (the one that killed 10 kids at East Coldenham High School in Orange County.)

also there was an EF3 in Delaware, wow?!  I think that's the one that ended up being lethal?

 

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14 hours ago, bluewave said:

It’s a good observation. -PNA and +AO patterns of the 1950s and 1960s didn’t have the SE Ridge. So those patterns were colder and snowier than what we have been getting recently. The Gulf Stream is much warmer and pumps the SE Ridge.

11F1A3C1-F356-4695-A8BC-1804F20C9681.png.81cdb404ca4044bd005dc5cc89b7c6f0.png
F921EA6D-5702-48D1-96BC-B89A751B2BE9.png.b9f8f38e877315170a6cde9d8213aeb0.png

624875BD-EC24-4FD4-B8DC-F26FA674245D.png.ac8e5b38f6dff4aedfb885bf21789907.png
 

 

 

One thing I am puzzled about, with the Gulf Stream warming so much how come we haven't seen a hurricane like Hugo hit us (not that I want that of course, but that was a hurricane that warmed up rapidly because of the Gulf Stream.)  Hurricanes still seem to rapidly weaken before they get to our region.

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1 hour ago, SnowGoose69 said:

Its hard to say if the NATL SSTs are solely responsible for that change though, there may be some other factor we just are not aware of which is leading to it.  I know many in the meteorology world argue that SSTs really do not impact atmospheric heights and that its an overblown theory...we see this in the GOA every year when the argument breaks out whether its the chicken or the egg

The GOA SSTs are mostly a function of Rossby waves being driven from the subtropical and tropical parts of the Pacific. So record SSTs to the south of that area are probably driving that process. Same goes for the increasing SE Ridge or WAR in our region. A 7° increase in the Gulf Stream off the Mid-Atlantic subtropics can cause an expansion of the subtropical ridge into our area. Notice how the models consistently underestimate the SE Ridge in the day 11-15 forecast. Also look back at winter forecasts for the US from all the private and public forecasters. The seasonal maps have underestimated the warmth in area. So we have to look into changes with the Gulf Stream we see a very anomalous 8 warmer than average winters in a row for the Northeast.
 

FB3B62BA-FFBC-4C49-BBC7-41137F722AF5.thumb.jpeg.488c3a0bbb1abc35785e5056c997fc20.jpeg

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14 hours ago, bluewave said:

It’s a good observation. -PNA and +AO patterns of the 1950s and 1960s didn’t have the SE Ridge. So those patterns were colder and snowier than what we have been getting recently. The Gulf Stream is much warmer and pumps the SE Ridge.

11F1A3C1-F356-4695-A8BC-1804F20C9681.png.81cdb404ca4044bd005dc5cc89b7c6f0.png
F921EA6D-5702-48D1-96BC-B89A751B2BE9.png.b9f8f38e877315170a6cde9d8213aeb0.png

624875BD-EC24-4FD4-B8DC-F26FA674245D.png.ac8e5b38f6dff4aedfb885bf21789907.png
 

 

 

when you look at the actual values of the anomalies the past western troughs were actually deeper than this year's

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50 minutes ago, forkyfork said:

when you look at the actual values of the anomalies the past western troughs were actually deeper than this year's

Same goes for the PNA. We used to get much more negative values back in the 1950s to the 1970s. March was the deepest the trough got this year. 



A07D586F-9642-40C5-BAA1-396BE8281F02.png.6065fd0060604363b22b08db094123e3.png

 

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Records:

 

Highs:

 

EWR:  82 (1950)
NYC: 80 (1892)
LGA: 76 (2010)


Lows:


EWR: 23 (1954)
NYC: 21 (1874)
LGA: 24 (1954)

 

Historical:

 

1804 - A large tornado crossed six Georgia counties killing at least eleven persons near Augusta. (David Ludlum)

 

1923: An estimated F4 tornado killed 15 people and injured 150 at Alexandria and Pineville, LA. 142 homes and businesses in Pineville were destroyed.

1933 - Pigeon River Bridge, MN, reported 28 inches of snow, which established the state 24 hour snowfall record. (4th-5th) (The Weather Channel)

 

1966: One of the strongest tornadoes in Florida's history moved in from the Gulf of Mexico and ripped through Pinellas, Hillsborough, Polk, and Osceola County. Damage was very severe in the towns of Gibsonia and Galloway in Polk County. 11 people were killed, and 350 were injured. The tornado was classified as F4.

1973 - Sandia Crest, NM, reported a snow depth of 95 inches, a record for the state of New Mexico. (The Weather Channel)

1983 - Colorado was in the midst of a three day winter storm. Buckhorn Mountain, located west of Fort Collins, received 64 inches of snow. (Storm Data)

1987 - Rains of five to eight inches drenched eastern New York State, and ten persons were killed in a bridge collapse over Schoharie Creek. (The National Weather Summary) (Storm Data)

1988 - Sunny and warm weather prevailed across the nation. Fort Smith AR reported a record high of 90 degrees. (The National Weather Summary)

1989 - Thunderstorms produced severe weather from the Lower Mississippi Valley to the Southern Appalachians. The thunderstorms spawned seventeen tornadoes, including one which caused two million dollars damage at Baldwin AL. Thunderstorm winds gusted to 90 mph at Bremen GA. (The National Weather Summary) (Storm Data)

1990 - A deep low pressure system in northern New York State brought heavy snow to parts of western and central New York during the day. The snowfall total of 5.8 inches at Buffalo was a record for the date, and 9.5 inches was reported at Rochester. Snowfall totals ranged up to 11 inches at Warsaw. (The National Weather Summary) (Storm Data)

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1 hour ago, LibertyBell said:

One thing I am puzzled about, with the Gulf Stream warming so much how come we haven't seen a hurricane like Hugo hit us (not that I want that of course, but that was a hurricane that warmed up rapidly because of the Gulf Stream.)  Hurricanes still seem to rapidly weaken before they get to our region.

You need a stupidly odd pattern to really get a Cat 3 or 4 up here and even then its probably likely to be a warm seclusion type thing which many now think 1938 was.  It has to be a case of a trof over the lakes interacting with a strong ridge where the system is pulled N or NNW because anything else will want to bend NNE naturally as it comes north and any storm which is near or touches the NC coast will usually weaken and be west of the warmest Gulf stream waters.

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14 minutes ago, SnowGoose69 said:

You need a stupidly odd pattern to really get a Cat 3 or 4 up here and even then its probably likely to be a warm seclusion type thing which many now think 1938 was.  It has to be a case of a trof over the lakes interacting with a strong ridge where the system is pulled N or NNW because anything else will want to bend NNE naturally as it comes north and any storm which is near or touches the NC coast will usually weaken and be west of the warmest Gulf stream waters.

Add to all of this it needs to be moving rapidly.  Warm seclusion can be a slower mover (they can do plenty of damage) but to get a Cat 3 pure hurricane up here it has to be moving fast.  Very much agree with a NNW movement as well, anything west of north in terms of track would be more favorable to get pure tropical system up here from an east of Hatteras location.  Having said all this those western Atlantic waters are quite warm so I would think that ups the ante of a possible strong tropical hit if the right steering is in place.

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Wasn’t there a supposed high end hurricane that landfalled on south NJ in 1821? And then I thought I read something about finding sedimentary evidence for a potentially Cat 4 hitting in the 15th century, though this would seem  a bit more speculative depending on how they determined its intensity  

Probably had to be extremely fast moving storms with not much chance to weaken. 

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1 hour ago, SnowGoose69 said:

You need a stupidly odd pattern to really get a Cat 3 or 4 up here and even then its probably likely to be a warm seclusion type thing which many now think 1938 was.  It has to be a case of a trof over the lakes interacting with a strong ridge where the system is pulled N or NNW because anything else will want to bend NNE naturally as it comes north and any storm which is near or touches the NC coast will usually weaken and be west of the warmest Gulf stream waters.

It seems to be easier to get a Cat 1 to do that, looking over the 20th century, the only hurricanes that have bent back into the coast were all Cat 1s.

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36 minutes ago, Volcanic Winter said:

Wasn’t there a supposed high end hurricane that landfalled on south NJ in 1821? And then I thought I read something about finding sedimentary evidence for a potentially Cat 4 hitting in the 15th century, though this would seem  a bit more speculative depending on how they determined its intensity  

Probably had to be extremely fast moving storms with not much chance to weaken. 

Yes to both, the 1821 hurricane was known as the Norfolk and Long Island Hurricane, though how it maintained Cat 4 intensity to Cape May and Cat 3 intensity when it hit Manhattan, I have NO idea.  If you look at the track, it looks a lot like Irene's (except slightly farther to the west-- which should mean even more land interaction!)

PreColumbine era yes-- there's also evidence of a high end supertsunami resulting from an asteroid impact (maybe the same one that formed Chesapeake Bay....which may have broken into two parts, the second of which landed just east of Toms River!)

 

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1 hour ago, MANDA said:

Add to all of this it needs to be moving rapidly.  Warm seclusion can be a slower mover (they can do plenty of damage) but to get a Cat 3 pure hurricane up here it has to be moving fast.  Very much agree with a NNW movement as well, anything west of north in terms of track would be more favorable to get pure tropical system up here from an east of Hatteras location.  Having said all this those western Atlantic waters are quite warm so I would think that ups the ante of a possible strong tropical hit if the right steering is in place.

Think of Sandy 2 months earlier...would stay mostly over the gulf stream

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4 hours ago, LibertyBell said:

One thing I am puzzled about, with the Gulf Stream warming so much how come we haven't seen a hurricane like Hugo hit us (not that I want that of course, but that was a hurricane that warmed up rapidly because of the Gulf Stream.)  Hurricanes still seem to rapidly weaken before they get to our region.

I believe it comes down to the steering currents during the hurricane season. Bob was the last New England hurricane back in 1991. All the high impact events like Sandy had the eye come ashore south of 40N. From what I can see, the much warmer SSTs have allowed the subtropical ridge to push up into New England and Eastern Canada. So the high impact hurricanes have all come in further down the coast. Like the hurricanes have been squeezing under. The Gulf has been the main focus for most of the landfalling major hurricanes in the last 30 years. During the previous 40, it was more evenly divided between Gulf and East Coast. 
 

https://www.aoml.noaa.gov/hrd/hurdat/All_U.S._Hurricanes.html


A11450DC-22A4-4B47-9CDD-AD386D341AD2.png.257e13619a4692badd5624d539d7f270.png


 

1991 Aug RI, 2; MA, 2; NY, 2; CT, 2 2 962 90 Bob
1992 Aug FL, SE5, SW4; LA, 3 5 922 145 Andrew
1993 Aug  * NC, 3 3 961 100 Emily
1994 None
1995 Aug FL, NW2, SE1 2 973 85 Erin
1995 Oct FL, NW3, I-AL 1 3 942 100 Opal
1996 Jul NC, 2 2 974 90 Bertha
1996 Sep NC, 3 3 954 100 Fran
1997 Jul LA, 1; AL, 1 1 984 70 Danny
1998 Aug NC, 2 2 964 95 Bonnie
1998 Sep FL, NW1 1 987 70 Earl
1998 Sep FL, SW2; MS, 2 2 964 90 Georges
1999 Aug TX, S3 3 951 100 Bret
1999 Sep NC, 2 2 956 90 Floyd
1999 Oct  * FL, SW1; NC, 2 2 964 95 Irene
2000s
2000 None
2001 None
2002 Oct LA, 1 1 963 80 Lili
2003 Jul TX, C1 1 979 80 Claudette
2003 Sep NC, 2; VA, 1 2 957 90 Isabel
2004 Aug  * NC, 1 1 972 70 Alex
2004 Aug FL, SW4, SE1, NE1; SC, 1; NC, 1 4 941 130 Charley
2004 Aug SC, 1 1 985 65 Gaston
2004 Sep FL, SE2, SW1 2 960 90 Frances
2004 Sep AL, 3; FL, NW3 3 946 105 Ivan
2004 Sep FL, SE3, SW1, NW1 3 950 105 Jeanne
2005 Jul LA, 1 1 991 65 Cindy
2005 Jul FL, NW3; I-AL 1 3 946 105 Dennis
2005 Aug FL, SE1, SW1; LA, 3; MS, 3; AL, 1 3 920 110 Katrina
2005 Sep  * NC, 1 1 982 65 Ophelia
2005 Sep FL, SW1; LA, 3; TX, N2 3 937 100 Rita
2005 Oct FL, SW3; FL, SE2 3 950 105 Wilma
2006 None
2007 Sep TX, N1; LA, 1 1 985 80 Humberto
2008 Jul TX, S1 1 967 75 Dolly
2008 Sep LA, 2 2 954 90 Gustav
2008 Sep TX, N2; LA, 1 2 950 95 Ike
2009 None
2010s
2010 None
2011 Aug NC, 1 1 952 75 Irene
2012 Aug LA, 1 1 966 70 Isaac
2012 Oct * NY, 1 1 942 65 Sandy
2013 None
2014 Jul NC, 2 2 973 85 Arthur
2015 None
2016 Sep FL, NW1 1 981 70 Hermine
2016 Oct * FL, NE2; GA, 1; SC, 1; NC, 1 2 963 85 Matthew
2017 Aug TX,C4 4 937 115 Harvey
2017 Sep FL, SW4,SE 1 4 931 115 Irma
2017 Oct LA 1, MS 1 1 983 65 Nate
2018 Sep NC, 1 1 956 80 Florence
2018 Oct FL, NW5; I-GA, 2 5 919 140 Michael
2019 Jul LA, 1 1 993 65 Barry
2019 Sep NC, 2 2 956 85 Dorian
2020s
2020 Jul TX, S1 1 973 80 Hanna
2020 Aug NC, 1; SC, 1 1 986 80 Isaias
2020 Aug LA, 4; TX, N1 4 939 130 Laura
2020 Sep AL, 2; FL, NW2 2 965 95 Sally
2020 Oct LA,2 2 970 85 Delta
2020 Oct LA,3; MS, 2; I-AL, 1 3 970 100 Zeta
2021 Aug LA,4 4 931 130 Ida
2021 Sep TX,N1 1 991 65 Nicholas
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5 minutes ago, bluewave said:

I believe it comes down to the steering currents during the hurricane season. Bob was the last New England hurricane back in 1991. All the high impact events like Sandy had the eye come ashore south of 40N. From what I can see, the much warmer SSTs have allowed the subtropical ridge to push up into New England and Eastern Canada. So the high impact hurricanes have all come in further down the coast. Like the hurricanes have been squeezing under. The Gulf has been the main focus for most of the landfalling major hurricanes in the last 30 years. During the previous 40, it was more evenly divided between Gulf and East Coast. 
 

https://www.aoml.noaa.gov/hrd/hurdat/All_U.S._Hurricanes.html


A11450DC-22A4-4B47-9CDD-AD386D341AD2.png.257e13619a4692badd5624d539d7f270.png


 

1991 Aug RI, 2; MA, 2; NY, 2; CT, 2 2 962 90 Bob
1992 Aug FL, SE5, SW4; LA, 3 5 922 145 Andrew
1993 Aug  * NC, 3 3 961 100 Emily
1994 None
1995 Aug FL, NW2, SE1 2 973 85 Erin
1995 Oct FL, NW3, I-AL 1 3 942 100 Opal
1996 Jul NC, 2 2 974 90 Bertha
1996 Sep NC, 3 3 954 100 Fran
1997 Jul LA, 1; AL, 1 1 984 70 Danny
1998 Aug NC, 2 2 964 95 Bonnie
1998 Sep FL, NW1 1 987 70 Earl
1998 Sep FL, SW2; MS, 2 2 964 90 Georges
1999 Aug TX, S3 3 951 100 Bret
1999 Sep NC, 2 2 956 90 Floyd
1999 Oct  * FL, SW1; NC, 2 2 964 95 Irene
2000s
2000 None
2001 None
2002 Oct LA, 1 1 963 80 Lili
2003 Jul TX, C1 1 979 80 Claudette
2003 Sep NC, 2; VA, 1 2 957 90 Isabel
2004 Aug  * NC, 1 1 972 70 Alex
2004 Aug FL, SW4, SE1, NE1; SC, 1; NC, 1 4 941 130 Charley
2004 Aug SC, 1 1 985 65 Gaston
2004 Sep FL, SE2, SW1 2 960 90 Frances
2004 Sep AL, 3; FL, NW3 3 946 105 Ivan
2004 Sep FL, SE3, SW1, NW1 3 950 105 Jeanne
2005 Jul LA, 1 1 991 65 Cindy
2005 Jul FL, NW3; I-AL 1 3 946 105 Dennis
2005 Aug FL, SE1, SW1; LA, 3; MS, 3; AL, 1 3 920 110 Katrina
2005 Sep  * NC, 1 1 982 65 Ophelia
2005 Sep FL, SW1; LA, 3; TX, N2 3 937 100 Rita
2005 Oct FL, SW3; FL, SE2 3 950 105 Wilma
2006 None
2007 Sep TX, N1; LA, 1 1 985 80 Humberto
2008 Jul TX, S1 1 967 75 Dolly
2008 Sep LA, 2 2 954 90 Gustav
2008 Sep TX, N2; LA, 1 2 950 95 Ike
2009 None
2010s
2010 None
2011 Aug NC, 1 1 952 75 Irene
2012 Aug LA, 1 1 966 70 Isaac
2012 Oct * NY, 1 1 942 65 Sandy
2013 None
2014 Jul NC, 2 2 973 85 Arthur
2015 None
2016 Sep FL, NW1 1 981 70 Hermine
2016 Oct * FL, NE2; GA, 1; SC, 1; NC, 1 2 963 85 Matthew
2017 Aug TX,C4 4 937 115 Harvey
2017 Sep FL, SW4,SE 1 4 931 115 Irma
2017 Oct LA 1, MS 1 1 983 65 Nate
2018 Sep NC, 1 1 956 80 Florence
2018 Oct FL, NW5; I-GA, 2 5 919 140 Michael
2019 Jul LA, 1 1 993 65 Barry
2019 Sep NC, 2 2 956 85 Dorian
2020s
2020 Jul TX, S1 1 973 80 Hanna
2020 Aug NC, 1; SC, 1 1 986 80 Isaias
2020 Aug LA, 4; TX, N1 4 939 130 Laura
2020 Sep AL, 2; FL, NW2 2 965 95 Sally
2020 Oct LA,2 2 970 85 Delta
2020 Oct LA,3; MS, 2; I-AL, 1 3 970 100 Zeta
2021 Aug LA,4 4 931 130 Ida
2021 Sep TX,N1 1 991 65 Nicholas

Thanks for this!  It also seems that although hurricanes maintain intensity further north, a lot of them get closer to Eastern Canada than they do to us.

in the above chart does * stand for post tropical?

 

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19 hours ago, bluewave said:

It’s a good observation. -PNA and +AO patterns of the 1950s and 1960s didn’t have the SE Ridge. So those patterns were colder and snowier than what we have been getting recently. The Gulf Stream is much warmer and pumps the SE Ridge.

11F1A3C1-F356-4695-A8BC-1804F20C9681.png.81cdb404ca4044bd005dc5cc89b7c6f0.png
F921EA6D-5702-48D1-96BC-B89A751B2BE9.png.b9f8f38e877315170a6cde9d8213aeb0.png

624875BD-EC24-4FD4-B8DC-F26FA674245D.png.ac8e5b38f6dff4aedfb885bf21789907.png
 

 

 

Interesting.  This conveys warm water north.  One of the theories is that the rapid warming of the ice fields could cool down the northern oceans as the ice melted and be conveyed south, possibly cooling other currents headed south?  Or even possibly touching off an ice age?

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42 minutes ago, LibertyBell said:

Thanks for this!  It also seems that although hurricanes maintain intensity further north, a lot of them get closer to Eastern Canada than they do to us.

in the above chart does * stand for post tropical?

 

Yeah, Canada sticks out further to the East. So they can catch many recurving systems that miss the US. 
 

 

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Three months from now, a forecast like this will mean EMS would be scraping people off the sidewalks.

Oh.    It is also Dry.      JB has April as BN, vis-a-vie the JMA.       The last 10 days of the month better be real cool, man.

8 to 14 Day Outlook - Temperature Probability

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1 hour ago, Dark Star said:

Interesting.  This conveys warm water north.  One of the theories is that the rapid warming of the ice fields could cool down the northern oceans as the ice melted and be conveyed south, possibly cooling other currents headed south?  Or even possibly touching off an ice age?

The AMOC slowdown pulls the Gulf Stream in closer to the Northeast and only cools a small part of the North Atlantic south of Greenland.

In the North Atlantic, the measured values differ markedly from the average global warming: the subpolar Atlantic (an area about half the size of the USA, south of Greenland) has hardly warmed up and in some cases even cooled down, contrary to the global warming trend. In contrast, a wide area along the American east coast has warmed up at an excessive rate. Both can be attributed to a weakening of the AMOC in the model simulation. The cooling is simply due to the reduced heat input from the AMOC. The excessive warming, on the other hand, is based on a somewhat more nerdy mechanism that has been known to experts for some time: if the AMOC weakens, the Gulf Stream shifts closer to the coast. (This has to do with conservation of angular momentum on the rotating globe.)

 

study by Duchez et al. (2016) shows that cold in the North Atlantic correlates with summer heat in Europe. This is due to the fact that the heat transport in the Atlantic has not yet decreased strongly enough to cause cooling also over the adjacent land areas – but the cold of the sea surface is sufficient to influence the air pressure distribution. It does that in such a way that an influx of warm air from the south into Europe is encouraged. In summer 2015, the subpolar Atlantic was colder than ever since records began in the 19th century – associated with a heat wave in Europe. Haarsma et al (2015) argue on the basis of model calculations that the weakening of the AMOC will be the main cause of changes in the summer circulation of the atmosphere over Europe in the future. Jackson et al (2015) found that the slowdown could lead to increased storm activity in Central Europe. And a number of studies suggest that if the AMOC weakens, sea levels on the US coast will rise more sharply (e.g. Yin et al. 2009). The impacts are currently being further researched, but a further AMOC slowdown cannot be considered good news. Yet, although the oscillations seen in Fig. 2 suggest the AMOC may well swing up again for a while, a long-term further weakening is what we have to expect if we let global warming continue for much longer.

 

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2 hours ago, Dark Star said:

Interesting.  This conveys warm water north.  One of the theories is that the rapid warming of the ice fields could cool down the northern oceans as the ice melted and be conveyed south, possibly cooling other currents headed south?  Or even possibly touching off an ice age?

Younger Dryas. 

Discounting the theories about a large airburst meteor strike causing the sharp return to near stadial conditions, the traditional thinking is that it was caused by the melting of the Laurentide ice sheet shutting down the AMOC (snapping it into its “slow” state, apparently the AMOC has two stable configurations, the one we’re in now and and “off” or “slow” state). When the forcing of the meltwater dissipated, temperatures sharply rebounded. 

We’re seeing something similar now with the melting of Greenland slowing the AMOC and the melting of Antarctica slowing the SMOC (new papers came out in 2023 about this, highly suggest reading). Will it be enough to terminate the overall thermohaline circulation into its other configuration? Continued slowing is a guarantee, which already implies destabilization.  
 

Edit:

This is one of the newer studies:

Paper

It’s believed the slowing SMOC by 2050 will cause something like an additional ~20% slowdown in the AMOC. 

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