bluewave

The EPS has been handling this pattern pretty well over the last week or so. It has been fairly steady with the MJO 6 500 mb pattern dominating. Longer duration MJO 6 patterns tend to show a poleward shift with more ridging returning to Plains and East after the first 10 days. This matches the moderation the EPS has been showing in the pattern for mid month. So the first 10 days or so will probably be the coldest part of December relative to the means.

It’s climo for recent gradient patterns no matter what winter month it is. We warm up enough for mostly rain near the coast with amped systems. This was the case last February. But since February is colder we were able to get a little more snow on the front end before the changeover.

A new tropical oscillation called the TWISO has been recently discovered. So maybe the reason we are getting a strong MJO 6 gradient pattern in early December is somehow related to it being out of phase with the MJO. Plus the split forcing between the Maritime Continent and the Western Hemisphere could also be creating an interference pattern. Models showing a MJO 6 interference gradient pattern in early December https://www.pnas.org/doi/10.1073/pnas.2511549122 The tropical climate variability is characterized by various oscillations across a range of timescales. Oscillations that imprint the tropical mean state are generally attributed to slow processes, such as the seasonal cycle or interannual variability. Here, we identify a pronounced tropics-wide intraseasonal oscillation (TWISO) in satellite observations and reanalyses. This oscillation, with a period of 30 to 60 d, is evident across multiple variables and involves interactions between convection, radiation, surface fluxes, and large-scale circulation. It is primarily manifested as convective perturbations in the tropical Indo-Pacific warm pool accompanied by oscillations in the large-scale tropical overturning circulation. Here, we examine the relationship between TWISO, the Madden–Julian Oscillation (MJO), and the instability of radiative-convective equilibrium. Certain phases of TWISO coincide with specific phases of the MJO, suggesting a potential connection between the two. However, although the MJO can amplify the oscillation amplitude of TWISO, it is not essential for TWISO to occur. Finally, due to its broad manifestation across the tropics, TWISO potentially exerts widespread influence on tropical weather and climate at regional scales.

That being said, gradient patterns in recent years have been setting up just north of NYC. We haven’t been near a gradient pattern jackpot zone since February 2014 and 1994. The WAR amps just enough on the storm days and the highs move east of New England. This is what the current models runs are showing for early December.

I am hoping we can get follow up storm systems tracking south of Long Island in the coming weeks and months when it’s colder. We saw a storm take a similar track on 12-5-20 to our south with mostly rain along the coast. With very amped systems early in the season we need strong Arctic high pressure over New England like we got back on 11-15-18.

Big story this year continues to be the strong W to NW flow behind the lows racing by to our north. So far this year has had 63 days at Newark with wind gusts reaching 40 mph or higher. This resulted in the impressive sieche on Lake Erie

Looks like a split decision showing up for the first week of December. Long range models shifted colder with the trough into the East instead of the ridge from previous runs. But the large storm on the 2nd and 3rd shifted warmer with a further north track and stronger WAR. Main issue with the storm is the very fast flow and lack of blocking allowed the high over New England to move off the coast. So the further north storm and slightly stronger WAR on the day of the storm pushed the rain to snow gradient just to the north and west of NYC. Since the colder start to December is a new pattern not showing up until day 6-10, it’s uncertain how the current day 11-15 and beyond will actually play out. If you look back on our recent Decembers, they have a tendency to start out cold from the 1st through 15th. Then we get the warm up every year since 2011 between the 17th and 25th. So it will be interesting to see how things actually play out vs what the models are currently showing. We would want to eventually see a colder storm for our area while we still have the cold. This is very important during La Nina’s since we need to get over 4” of snow in December to match the above vs below seasonal snowfall that I outlined a few days back in this thread. So hopefully we can connect with at least one storm next few weeks while the colder start is still nearby. New early December pattern colder than old runs Old run too warm for early December New run warmer storm further north on the 2nd and 3rd Old run storm track colder to the south and more suppressed

Split forcing between the Maritime Continent and the Western Hemisphere appears to be causing an interference pattern resembling a phase 6 in early December. It could also be why the models have been showing so much volatility between runs over the last week as we head into December. A Northeast Pacific +TNH with a a cold upper low centered near Hudson Bay more closely resembles a phase 6 composite. So trying to guess what composite or pattern we end up with in mid to late December is anyone’s guess at this point. We will just have to let things play out next few weeks to see which area of forcing eventually wins out.

When we subtract the recent strongest El Niños from the era before the warming of the WPAC warm pool, it shows what I have been talking about. The WPAC hasn’t been cooling down like it used to during strong El Niños. So this leads to the forcing shifting further west than it previously did during El Niños. This is why we had Niña-like elements combining with the 2015-2016 and 2023-2024 events. During the weaker 2018-2019 and 2019-2020 events they couldn’t even couple and the La Niña background more completely dominated.

The 20th heaviest snowfall total through 11-26 at Marquette is very respectable. Time Series Summary for Marquette County Area, MI (ThreadEx) Click column heading to sort ascending, click again to sort descending. 1 2014-11-26 55.0 0 2 1989-11-26 49.3 0 3 1991-11-26 46.9 0 4 2000-11-26 46.8 0 5 2002-11-26 46.6 0 6 1997-11-26 44.9 0 7 2008-11-26 43.7 0 8 1988-11-26 43.3 0 9 1992-11-26 41.4 0 10 2018-11-26 40.8 0 11 2022-11-26 40.7 0 12 2005-11-26 39.8 0 13 1979-11-26 39.0 0 14 1993-11-26 38.7 0 15 1975-11-26 36.3 0 16 1976-11-26 31.1 0 17 2020-11-26 31.0 0 18 1995-11-26 29.8 0 19 1981-11-26 29.2 0 20 2025-11-26 28.9 0

Very unusual to have the warmest Thanksgiving during the 12th coldest November. Climatological Data for NY CITY CENTRAL PARK, NY - November 1933 Click column heading to sort ascending, click again to sort descending. Sum 1450 1059 - - 687 0 0.90 0.5 - Average 48.3 35.3 41.8 -6.2 - - - - 0.0 Normal 54.0 42.0 48.0 - 511 1 3.58 0.5 1933-11-01 64 49 56.5 4.0 8 0 0.00 0.0 0 1933-11-02 65 50 57.5 5.3 7 0 0.00 0.0 0 1933-11-03 63 51 57.0 5.1 8 0 0.00 0.0 0 1933-11-04 54 38 46.0 -5.6 19 0 0.00 0.0 0 1933-11-05 41 29 35.0 -16.3 30 0 0.10 0.1 0 1933-11-06 39 33 36.0 -15.0 29 0 0.33 0.1 0 1933-11-07 46 37 41.5 -9.1 23 0 T 0.0 0 1933-11-08 44 34 39.0 -11.3 26 0 T T 0 1933-11-09 44 32 38.0 -12.0 27 0 T T 0 1933-11-10 40 32 36.0 -13.7 29 0 0.00 0.0 0 1933-11-11 45 28 36.5 -12.9 28 0 0.04 0.0 0 1933-11-12 45 35 40.0 -9.1 25 0 0.00 0.0 0 1933-11-13 59 38 48.5 -0.3 16 0 0.08 0.0 0 1933-11-14 43 32 37.5 -11.0 27 0 T T 0 1933-11-15 32 21 26.5 -21.6 38 0 0.00 0.0 0 1933-11-16 30 17 23.5 -24.3 41 0 0.00 0.0 0 1933-11-17 36 19 27.5 -20.0 37 0 0.00 0.0 0 1933-11-18 41 36 38.5 -8.7 26 0 0.14 0.3 0 1933-11-19 39 34 36.5 -10.4 28 0 T T 0 1933-11-20 49 35 42.0 -4.6 23 0 0.00 0.0 0 1933-11-21 58 32 45.0 -1.3 20 0 T 0.0 0 1933-11-22 60 47 53.5 7.5 11 0 0.04 0.0 0 1933-11-23 48 37 42.5 -3.2 22 0 0.00 0.0 0 1933-11-24 43 32 37.5 -7.9 27 0 0.00 0.0 0 1933-11-25 50 36 43.0 -2.0 22 0 0.00 0.0 0 1933-11-26 55 43 49.0 4.3 16 0 0.17 0.0 0 1933-11-27 43 28 35.5 -8.9 29 0 0.00 0.0 0 1933-11-28 54 32 43.0 -1.1 22 0 0.00 0.0 0 1933-11-29 51 42 46.5 2.7 18 0 0.00 0.0 0 1933-11-30 69 50 59.5 16.0 5 0 0.00 0.0 0 Coldest November Time Series Summary for NY CITY CENTRAL PARK, NY - Month of Nov Click column heading to sort ascending, click again to sort descending. 1 1873 37.2 2 2 1871 38.8 0 3 1880 38.9 0 - 1875 38.9 0 4 1882 39.0 0 5 1901 39.7 0 6 1869 40.6 0 7 1887 41.2 0 8 1894 41.3 0 9 1872 41.4 0 10 1917 41.6 0 11 1976 41.7 0 12 1933 41.8 0

I wonder how strong of an El Nino would be necessary to completely take the record WPAC warm pool out of the equation? Even during the 2015-2016 record super event, we still got the record MJO 5 for such a strong El Nino in December 2015 leading to the +13 that month around NYC. Thankfully, there was a major improvement during January and February 2016. But our next El Nino attempts in 2018-2019 and 2019-2020 were too weak to fully couple due to that record WPAC warm pool leading to the strong La Nina background patterns. Then the borderline super event in 2023-2024 had the record forcing and SST warmth from the IO into the WPAC for such a strong El Nino. This lead to the record warmth and 500mb ridging in Canada extending down into the US with no Nino trough development in the East.

Yeah, short term is the key phrase as those near to record SSTs extend down well below the surface which were recently enhanced by the record IOD.

You can see how the long range models continue to underestimate the forcing near the Maritime Continent with the record warm pool there leading to the stronger Northern Stream of the Pacific Jet. So it interferes with the progression to a true MJO 8 500 mb and storm track pattern with the weaker Pacific Jet. This is why the RMM charts appear to show a slowdown or loop near the 7-8 border and lowering amplitude toward the circle following the higher amplitude 7. New run Old run WPAC warm pool with expansive area of +28C to +30C SSTs

Early first snow for Paris also.