11/16/25

Winter 2025-26 in Southeast Michigan; Will it be as Rough as Many Say it Will? THE ANALOGUES ~/PART'S I & II Merged/ - /Dec 1st 2025/ Meteorological Updates Routinely Added

SOUTHEAST LOWER MICHIGAN WINTER OUTLOOK 2025-26


Temperatures:

Both this set of winter's set of analogues and extended model monthly guidance for December  spell out a colder beginning of winter than average; especially the early part of the winter. Analogues paint a cold picture for December, contrasting the recent pictures in Southeast Michigan Inhabitant's minds of numerous mild Decembers since 2000 (see rest of Outlook). While a milder mid December is expected to break the cold snap - latest guidance strongly backs up a below normal average December temperature on the whole with colder weather returning, later.

Analogues for the rest of the winter at this early juncture do intimate a mid winter thaw (most likely our old friend "January Thaw") and another milder period possibly in February (mid-late) but surrounded by cold. Overall temperatures should average 1-3 degrees below normal but subject to change with the aggressive, fast moving winter patterns expected. Dominant periods of cold should be tempered by quick milder air masses. Timing of the patterns will be as much of an issue as much as the expected winter weather in the final analysis.

Snowfall and Precipitation

Snowfall and precipitation is a big toss-up this year with not only mixed precipitation goofing things up but storm tracks being rather fickle. Someone's going to get clobbered when upper energy phases (as the Arctic Stream, Polar Jet and Sub-tropical vying for dominance) but who & when is the question? Looking at what's briefly transpired; Lake Effect communities, Upper Midwest and Great Lakes look primed but what of the rest of the winter? If La Nina follows a general pattern; the Lower Great Lakes and Ohio Valley look vulnerable, anytime. Stay Tuned. As for now; near normal or average snow for Southeast Michigan but subject to change with the wind. 

AN OBSERVATION -

Never have I seen so many Winter Outlooks on the Net as I have seen this fall - and never have so many of them been so dire. Dire meaning; calling for a brutally cold and/or stormy winter across the Great Lakes and subsequent surrounding areas. It seems everyone and their mother are doing Winter Outlooks - whether qualified or not (educated and experienced). I must say; when I started doing Season Outlooks for Southeast Lower Michigan while employed by the National Weather Service some 27 years ago (The Super El Nino of 1997-98), I was in barren territory. The only other creators of Outlooks that I saw were the NWS Climate Prediction Center for the whole country and maybe a scant few private companies. A few surrounding WSFO meteorologists starting joining me in Weather Outlooks in the late 90s - early 2000s in the Great Lakes Region as "Down-scaling" got underway. Down-scaling involved looking at familiar hemispheric patterns known at the time; researched by meteorologists and climatologists nationally then, subsequently studying smaller climate and local patterns and making a winter forecast.

FORMAT - 

A new format? I've decided to split up my outlook to get my Winter Analogues out first /Part - 1/; then discuss how the hemispheric patterns should affect the up-coming Winter 2025-26 pattern /Part -2/. Finally; expected winter weather forecast discussed and final forecast issued after Thanksgiving. Basically, this will be during the month of November and into the climatological winter period of December - February. Snowfall projections will be for entire snowfall season into climatological spring. Lastly; Look for Model Outlooks for the Winter.

WINTER 2025 - 26 ANALOGUES 

This new set of analogues goes back to the mid 20th century. Gone for this run are the earlier analogues (pre-1940s) as many were during cold periods with lower actual temperature data and normals. Over the past several decades (mainly since the 1980s); average normals have risen about a degree and a half with time when combining the recent climatological warming period along with the urban climate warming at Detroit /DTW Airport/. For example; the winter normal average temperature is now 28.3 degrees for the 30 year period from 1991-2020. The 100 year temperature average /1891-1990/ before that time by my estimation was about 26.9 degrees.  That leaves approximated departure of around a degree and a half /+1.4/ and that 100 year average is also included in the analogue data chart.

Leaving out the "colder period" analogues pre-1940 made little difference in this winter's sample as the temperature analogues since those analogues averaged notably below normal, anyway. 

Snowfall and Precipitation meanwhile varied considerably and really are a factor of prevailing storm tracks. Snowfalls varied from 18.0" /1960-61/ to a whopping 94.9" during the relatively recent cold and snowy winter of 2013-14. Maybe it's not surprising the "average" snowfall for the entire set landed just a shade (of snowfall) above the 45.0"norm at 45.6". Overall; snowfall norms have been rising slowly the past several decades from the mid-upper 30s to the mid 40s. You wouldn't know that the past three winters with the below average snowfalls officially at Detroit /DTW/. Troublesome this season as mention above is the extreme snowfall brackets from well below normal to well above - "relinquishing to normal". Overall, below normal precipitation was dominant when averaged however; there were 4 better than an inch below normal, 3 better than an inch above and 5 within an inch of normal - really split. But in that case, around normal precipitation is the dominant (and again, that would be within an inch of normal). After looking at the analogue winters; Lake-effect snows across the Great Lakes should be relatively active seeing the cold, blustery conditions predominant in several of the early - mid winters/cold time periods.

Predominant Storm Tracks have made themselves known early in the game this winter by starting out solidly in November. This is reflective of the lower heights (and jet streams). Even the more infrequent "Gulf Low" (non-predominant) is occasionally showing up on model output and I suspect we'll see some action there too. The winter is starting out busy but we will surely get breaks and the occasional mild spells. 

Snowfalls in the analogues over Southeast Michigan were nearly on the same level as precipitation; 6 analogues were below normal, 4 above and 3 within 5.0"of normal. While there's a bit of a lean toward below normal snow in the actual numbers - at the same time, 4 were snowy and 3 contained normal snow winters - so it's pretty much a toss-up. There is a slight preference for the higher totals for the northern and western sections in Southeast Michigan this winter (more typical). This includes the northern and western parts of Metro Detroit. 

 

Another interesting thing I noticed in the data from the Novembers preceding many of the analogues (including Nov '25), they contained the predominance of normal to below normal temperatures. When normal to below normal November temperatures dominated in the analogues; the winter temperature were below normal.  Even two of the November's; 1960 and 1985 that contained above normal temperatures still were followed by colder winters!

Observing the Temperature Departure Map below when all analogues were plotted; below normal temperature departures of -2.0 to -3.0 degrees were observed on average.  Be advised: these are past analogue winters and do not necessarily reflect exactly this upcoming cold season. I'm more interested at not the particular data for each analogue but the overall trend (and even when widely variable, do have dominating patterns discussed in this Outlook).

Analogue 2025-26 Cold Season November through March Temperature Departure

 

 














ADETROITTEMPS
PCPN
NSEASONDECJANFEBWNT AVEWINTERNAO/SCSEASONDEC-FEBWINTERQBOEST FIRST
A1942-43-n25.621.728.025.11N/SC--1942-43-n7.191MFROST
L1960-61-a25.223.130.826.42N/SC-1960-61-b2.871E-10/1
O1962-63-b25.117.218.820.43N-/SC-1962-63-b2.362E9/20
G1967-68-mb30.920.924.325.44N-/SC++1967-68-n8.971E-9/23
U1978-79--b28.918.616.521.35N-/SC++1978-79-n4.903W-10/08
E1981-82--n27.817.120.721.96N/SC+1981-82-b6.912E09/24
S1985-86-a22.223.924.623.67N/SC--1985-86-ma6.273W-10/02

1993-94-n30.817.323.523.98N+/SC--1993-94-n4.954E-9/30

1996-97-mb31.523.030.628.41N-N+/SC-1996-97-mb9.052E-/W-10/03
W2001-02-ma35.932.732.933.81N+/SC-2001-02-n7.504W-10/06
E2013-14-b26.816.419.420.99N/SC+2013-14-n8.163W10/19
A2017-18-b26.624.631.027.42N+/SC--2017-18-ma7.115E+10/26
K2024-25-ma33.223.026.127.43N+/SC++2024-25-n5.796W10/17













LAve28.521.625.225.1
25.1Ave6.85
QBO
ANORM 30Y31.225.728.028.3100 yr ave26.9Norm6.56
E/+

Dep-2.7-4.1-2.8-3.2
-1.8Dep0.29


N



-1.2






IDETROITSNOWFALL
Oct
NSEASONOCTNOVDECJANFEBMARAPRSEA TOTSEASONSib snow**MAY
A1942-43-nT4.49.218.42.72.96.844.41
SNOW
S1960-61-bT1.04.53.35.10.43.718.01N/AT

1962-63-bT0.211.27.57.63.2T29.72N/AT
I1967-68-nT1.44.511.82.810.00.130.63B

1978-79-n0.06.16.613.33.92.73.035.64B
N1981-82-b0.10.717.320.013.313.69.074.01E
E1985-86-ma0.02.014.18.620.87.41.354.22B
U1993-94-n0.40.61.917.917.13.74.245.82BT
T1996-97-mb0.04.17.420.85.44.90.543.13MB
R2001-02-nT0.04.915.06.77.1T33.75B
A2013-14-nT1.215.539.123.412.53.994.93E
L2017-18-maTT22.59.221.05.92.461.04MB

2024-25-n0.01.83.68.912.20.41.828.76B
IAveT1.89.514.910.95.72.845.6
B

30y NormT1.98.914.012.56.21.545.0


2Dep0.0-0.10.60.9-1.6-0.51.30.6
Sib Snow
0




7

45ther* N/A
2ColorTempsDegrees
RainInches
Snow *Inches


5Legend:Below1.0>
Below1.00>
Below<5.0n

~
Normal0.0-1.0
Normal0.00-1.00
Normal>-5.0<5.0


2
Above1.0>
Above1.00>
Above>5.0


6





































LEGEND:TOP CHART
(Left to Right columns)










COLUMN
TEMPERATURE PRECIPITATION CODES
























1
Analogue Seasons (Preceding Nov temperature departure)











2-4
Dec - Feb average temperatures











5
Winter average temperatures











6
Number of analogues winter average temperatures above, normal & below by count and color scheme











7
Dominant: North Atlantic Oscillation /NAO/ & Solar Cycle /SC/











8
Analogues Seasons (Preceding Nov Precipitation)











9
Winter Precipitation Total











10
Number of analogue winter precipitation totals above, normal & below by count and color scheme











11
Dominant Quasi-Biennial Oscillation:


W(est), E(ast), M(isg)









Quasi-Biennial Oscillation (QBO) is a regular variation in stratospheric winds that influences hemispheric climatic &












subsequent local weather. It has a 28-month cycle and affects the strength of the polar vortex and jet stream.

























BOTTOM CHART (Left to Right columns)












SNOWFALL, MONTHLY TOTALS AND SEASON TOTAL



TOTALS/DEPARTURES








Nov, Mar & April snowfalls are within of an inch for below, normal & above rather than 5" for Dec-Feb












SIB - Siberian Snow Cover this October compared to that analogue year










 

Next up: Hemispheric Patterns & Meteorological Set Up - Winter Update Part II

Hemispheric Discussion 

In case you haven't surmised by now; the upcoming winter is expected to be, like last winter, a La Nina winter but with the La Nina fading early in 2026. Therefore; we are at the present at this winter's La Nina peak (late November into December). Both La Nina's are generally similar in strength, both a weak La Nina. I do look for this year's La Nina to have more of an influence on our weather than last winter's; mainly due to the atmosphere's stronger resultant La Nina pattern reaction (not dominant last winter) along with the Negative Pacific Decadal Oscillation in place.

 

Here are the Hemispheric SST temperatures at the close of November 2025

 

 

The maturing weak La Nina shows up well of the coast off Northern South America extending due west across the Pacific. The La Nina boundary below normal temperatures are displayed throughout all areas: Nino 1+2, Nino 3, Nino 3.4 and Nino 4. In addition; the Negative (Cold) PDO is well established again off the West Coast like 2017.

 

 

The best likeness of this fall's SST pattern that I could find in the analogue's was indeed; the La Nina of 2017-18.  The cool phase of the Pacific Decadal Oscillation /PDO/ was also on full display that year also. The Atlantic SST's were generally not as warm in 2017 as this late fall, however along the East Coast there are pockets of mixed above and below SST's this late November as opposed to 2017. 

 


 La Nina 2025-26

 

As one can see; the La Nina of 2017-18 extended through the winter and into the early spring of 2018 unlike this season of 2025-26 when the La Nina is expected to wind down earlier during mid winter.  See the data from the ENSO SST's below from the two time periods 2017-2018 and 2025: 

                      JAN  > DEC
 
  

Another similar La Nina SST forming from a Neutral SST was just last year /Winter of 2024-25/. While this analogue La Nina too shows similar traits - there were differences. The La Nina was slower to form and remained very weak dropping to just a SST of -0.6C in January. The winter pattern of 2024-25 over Southeast Lower Michigan was very slow to evolve, unlike this winter. January and February were colder with below normal temperatures with just light amounts of snow through the season. The "real winter months" last winter - like many of the past numerous winters were January, February and March. A cold December has become more of a rarity. In this millennium, since the Winter of 2000 - out of 25 - a generous 17 Decembers have been warmer than normal with the past 8 all above normal!


North Atlantic/Arctic Oscillation - NAO/AO 

Most winters; the phase of the NAO/AO is one of the most important ingredients to the type of winter to be-had over the central and eastern part of the country; and even parts of the mountainous areas of the west at times. This is one of the most elusive oscillations to predict for more than a week or two out. The recent NAO & AO projection for the first half of December is basically calling for a negative phase which mainly relates to below normal temperatures over Southeast Lower Michigan. 

  

As of December 1st - The projected NAO/AO winter model from -

https://www.kylemacritchie.com/ - An intriguing scientist Kyle Macritchie; shows the phases expected for the NAO and AO. It should be noted this too is subject to change as new data is received and processed. While the NAO meanders in it's negative/positive phases, the AO is predominantly projected to be in a negative phase. Supporting a colder than normal winter for the region.

 

  

 


Pacific Decadal Oscillation /PDO/ and associated subset EPO

A cool phase of the PDO is represented on the right of the following example and compare it to the current state on the Pacific SST's.


                             Warm Phase of the PDO                    Cool Phase of the PDO

 
Generally warm phases coincide with El Ninos or Neutral states and rarely La Nina states while cool phases coincide with La Ninas, as in the present state. Studies propose that when the PDO and ENSO are out of phase; which is a somewhat rare event, that they may cancel out their known effects. This isn't expected to happen during the upcoming winter with La Nina and a cool phase of the the PDO in synchronicity. The two together tend to compliment one another and several times; accentuate one another effects.

"When SSTs are anomalously cool in the interior North Pacific and warm along the Pacific Coast, and when sea level pressures are below average over the North Pacific, the PDO has a positive value. When the climate anomaly patterns are reversed, with warm SST anomalies in the interior and cool SST anomalies along the North American coast, or above average sea level pressures over the North Pacific, the PDO has a negative value" (Courtesy of Mantua, 1999).
 
"The Pacific Decadal Oscillation (PDO) is a pattern of Pacific climate variability similar to ENSO in character, but which varies over a much longer time scale. The PDO can remain in the same phase for up to 20 to 30 years, while ENSO cycles typically only last 6 to 18 months. The PDO, like ENSO, consists of a warm and cool phase which alters upper level atmospheric winds. Shifts in the PDO phase can have significant implications for global climate, affecting Pacific and Atlantic hurricane activity, droughts and flooding around the Pacific basin, the productivity of marine ecosystems, and global land temperature patterns. Experts also believe the PDO can intensify or diminish the impacts of ENSO according to its phase. If both ENSO and the PDO are in the same phase, it is believed that El Niño/La Nina impacts may be magnified. Conversely, if ENSO and the PDO are out of phase, it has been proposed that they may offset one another, preventing "true" ENSO impacts from occurring". 


http://jisao.washington.edu/pdo
http://www.john-daly.com/theodor/pdotrend.htm

SOLAR CYCLE /SC/

Solar cycle actual effects on short term weather and longer term climate variability remain a controversial subject. I've read several articles which support or are against their shorter term winter relevancy. Some theorize that both natural solar cycles and man's influence affect our climate. I am in favor of the solar cycle being somewhat relevant and sometimes giving the present winter cycle a "little kick" in regard to hemispheric wind flow patterns and resulting temperatures. Numerous recent studies for example, do in fact make the connection to our climate and solar activity including wintertime effects. One of the studies stated the following:

"The Euro–Atlantic sector seems to be a region with a par-
   ticularly strong solar influence on the troposphere. In fact,
significant positive correlations between solar activity and
  surface temperature in Europe have been reported in several
 papers (e.g. Tung and Camp, 2008; Lean and Rind, 2008;
 Lockwood et al., 2010; Woollings et al., 2010), although
  long records tend to give very weak signals (van Olden-
   borgh et al., 2013). We found a weak but significant change
     in the mean late winter circulation over Europe, which re-
   sults in detectable impacts on the near-surface climate. Fig-
   ure 9 suggests that during solar minima more cold air is ad-
   vected from the Arctic, thus resulting in a slightly increased
 probability of colder winters for large parts of the continent.
 Sirocko et al. (2012) recently reached the same con-
 clusion after analyzing 140 yr in 20CR, although their results
are strongly dependent on their selection criteria for
  the solar minimum composite (van Oldenborgh et al., 2013),
    which includes only one winter for each solar cycle".

See analogues and Solar Cycles abbreviated on the Winter Analogue chart. It look's as though with a decreasing solar cycle beginning from the maximum cycle; the solar cycle will continue to have more to do with disrupting the communication factor and ignite the northern lights again.
 

 THE QBO INFLUENCE


The QBO, or Quasi-Biennial Oscillation, is an oscillation in the wind direction in the stratosphere within about 15 degrees of the equator. Over a roughly two-year period, winds tend to oscillate between westward and eastward, with the switch between west and east winds starting high in the stratosphere and then shifting lower in altitude with time. The QBO is the result of waves propagating vertically in the atmosphere that then interact with the mean flow to slowly change wind speeds and direction. These changes influence the overall global circulation patterns, which in turn influence winter weather patterns across North America. 

The amplitude of the easterly phase is about twice as strong as that of the westerly phase. At the top of the vertical QBO domain, easterlies dominate, while at the bottom, westerlies are more likely to be found. At the 30mb level, with regards to monthly mean zonal winds, the strongest recorded easterly was 29.55 m/s in November 2005, while the strongest recorded westerly was only 15.62 m/s in June 1995 (Wikipedia).

If you notice on my analogues; I included the QBO's for each available winter and compared it to the upcoming winter's QBO phase and trend. The present and expected QBO this winter is for an easterly QBO (recently switching from west since the summer shown below as a negative wind speed) and also increasing in amplitude. The set of maps below show the differing influences of the QBO dependent on phase and trend.The QBO is presently in the negative and trending more negative phase (first map). The negative /easterly/ effect supports the temperature map of the Winter Analogue:
 
 

QBO and WinterTemperatures Trends


 

Next - What do the Models say about the Winter? AI? 

 

Making weather fun while we all learn,
Bill Deedler -SEMI_WeatherHistorian

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