This is my first call on the potential December 20-22 blizzard event. Let's do a model rundown first, then review the teleconnections before we get into the forecast.
We start now with the American's GFS model on the evening of December 19th. Pictured above are 850mb temperatures in the dashed lines, sea level pressure values in solid black lines, and precipitation values as filled in colors. The rain/snow line is the farthest-south dashed blue line. Any precipitation above that southernmost dashed blue line is supposedly snow. The GFS predicts we see our storm system coming out of the Rockies on the evening of December 19th, with a snow event ongoing in the Plains. Accumulations could range from 1-3 inches at this time in the forecast. The presence of a ridge of high pressure in the Southeast tells me that this storm system will be forced more towards the north rather than along the Gulf Coast.
This forecast is for 12 hours later, and is valid on the morning of December 20th. We now see the storm system has fled northeast into Chicago, and the central minimum pressure is approaching 990mb. Precipitation shown above tells me that a light snow event would be ongoing in Wisconsin and possibly Iowa, probably accumulations of 1-4 inches. In the southeast quadrant of this storm system, heavy rain and thunderstorms are ongoing. The tight pressure gradient, tight temperature gradient and overall strength of this storm system tells me a linear severe weather threat certainly is possible for much of the southern Midwest, southern Ohio Valley and general Southeast US.
Snow accumulation forecasts favor Wisconsin as the big winner per the GFS:
So the GFS takes the system into Illinois and gives Wisconsin the big snows. Let's now turn to the European model.
The ECMWF model, regarded as a more trustworthy model than the GFS, shows the storm system ejecting from the Plains in Oklahoma with a central minimum pressure of 995 millibars. Again, we see that high pressure system in the Southeast which will support the prospect of this storm system staying into the Midwest and Ohio Valley. This forecast is valid for the evening of December 19th.
Moving into the evening of December 20th, we see that our storm system has now strengthened greatly since the 24 hours before, with the central minimum pressure now at 981 millibars. That is a change of 12 millibars in 24 hours- not a common sight away from the Northeast. The tight pressure gradient tells me that this will be a very windy event, and if cold air factors into the equation after the storm departs, lake effect snow could be on overdrive. Also, note that piece of lower pressure jutting out of the southern side of the storm system. This could be a push at another storm system developing, one which could go into the Northeast, but that remains to be seen.
A few images of the ECMWF's precipitation and temperature forecast centered over the Midwest:
Now that we've covered the two big models, let's visit a couple other forecast models not as reliable, but still worth a glimpse.
This is the Canadian's GGEM model forecast for the afternoon of December 19th. Pictured above are sea level pressure (SLP) values for this timeframe, and the colored areas depict 10 meter wind speeds. We can see our storm system in north Texas, being squeezed towards the northeast as pressure from the ridge offshore the Southeast increases. The storm system has no choice but to shoot northeast- that's one thing we're confident in at the moment. The GGEM predicts the system will be much weaker when it exits the Rockies than other models are predicting.
Moving ahead to the morning of December 20th, we now see that the GGEM has taken the system into Indiana with a central minimum pressure of 994 millibars, indicating that some strengthening has occurred. Despite this, the system remains weaker than the GFS and ECMWF are predicting. Even though a strength difference may seem like nothing, I can assure you it can have significant implications. If the system is weaker than is being forecasted, the track can (and would) significantly change. Let's hope that doesn't happen, or this whole post would be moot. We still see that high pressure in the waters off the Southeast. Despite the presence of a tight pressure gradient, 10 meter winds are not showing up too strong, which I can understand, considering the GGEM is weaker than the GFS/ECMWF at this point in time. I am hesitant to disregard the GGEM, because it is in line with the GFS, meaning the two may be on to some sort of consensus.
Now, for the last model we look at, we see SLP values in solid black lines, 850mb temperatures in dashed lines (the same rain/snow rule as the GFS applies here), and precipitation values in colors. This is the NOGAPS forecast, made by the Navy but not regarded as a solid model that you can trust. I'm including it moreso to give some spread to the forecast, not so much to find a solution from the NOGAPS. This model starts out with the system ejecting from the Rockies at a minimum pressure of 993 millibars in the early morning hours of December 19th. Again, watch that timing difference! An already-tight pressure gradient in OK/AR/TX/MO tells me a severe weather situation may be trying to form in that area.
Moving ahead to the early morning hours of December 20th, we find the NOGAPS projecting this system to possibly have split in two. We see one storm system with a 1005mb minimum pressure centered in Arkansas, and another storm system centered in Wisconsin with a central minimum pressure of 1000 millibars. I will refer to them as System 1 and System 2, respectively. System 1 shows a more linear alignment of precipitation, telling me that if this solution verified, we would probably see a mesoscale convective system (MCS) or small squall line in the area as a result of tight temperature and pressure gradients in the region. As for System 2, this looks to be the main piece of energy. The precipitation looks to be a modest snowstorm, with accumulations around the 3-6 inch mark based solely on this image. If the two systems had stuck together, a solution similar to the other models may have evolved. Needless to say, I am discounting the NOGAPS model.
Teleconnections are also a big deal, in terms of the North Atlantic Oscillation (NAO). When the NAO is in its negative phase, you'll see a tendency for storm systems to move up the Northeast coast and strengthen rapidly into Nor'easters. This comes in response to the highly meridional flow set up by the high pressure system in Greenland and the storm system in the Northeast. There are two sub-categories of the NAO, and that is west-based and east-based. In a west-based negative NAO, you'll see the high pressure to the west of Greenland, hence the term west-based. Likewise, in an east-based negative NAO, you have the high pressure system to the east of Greenland. The difference is which one affects which areas. In a west-based negative NAO, you'll see the East US getting in on the most cold and storms, while the East-based negative NAO keeps the cold and storms in the Plains and Midwest. The forecasts for the west-based negative NAO are stronger than the east-based, so it is plausible to think that the East Coast has an advantage. However, because of that Southeast ridge, we'll see the track take a detour north and then go northeast through the Great Lakes. The whole situation is very complicated, but in summary, the NAO does favor a track being shown by the ECMWF or even the GFS, maybe a bit farther south if the negative PNA holds in place.
This image shows what the meteorologists at the Hydrometeorological Prediction Center (HPC) think in terms of best model choice for the next 7 days. Looking at the D4 and D5 areas, we see that the HPC generally leaned towards the ECMWF model, the ECMWF Ensembles (ECMWF EPS) and the Canadian model. Surprisingly, no mention of the GFS model is recorded.
Going off of all the models printed above, the teleconnection forecasts and the HPC forecast preferences, I have made my first call as printed below.
Forecast Preference: ECMWF/ECMWF EPS
Confidence: 55%
Andrew
We start now with the American's GFS model on the evening of December 19th. Pictured above are 850mb temperatures in the dashed lines, sea level pressure values in solid black lines, and precipitation values as filled in colors. The rain/snow line is the farthest-south dashed blue line. Any precipitation above that southernmost dashed blue line is supposedly snow. The GFS predicts we see our storm system coming out of the Rockies on the evening of December 19th, with a snow event ongoing in the Plains. Accumulations could range from 1-3 inches at this time in the forecast. The presence of a ridge of high pressure in the Southeast tells me that this storm system will be forced more towards the north rather than along the Gulf Coast.
This forecast is for 12 hours later, and is valid on the morning of December 20th. We now see the storm system has fled northeast into Chicago, and the central minimum pressure is approaching 990mb. Precipitation shown above tells me that a light snow event would be ongoing in Wisconsin and possibly Iowa, probably accumulations of 1-4 inches. In the southeast quadrant of this storm system, heavy rain and thunderstorms are ongoing. The tight pressure gradient, tight temperature gradient and overall strength of this storm system tells me a linear severe weather threat certainly is possible for much of the southern Midwest, southern Ohio Valley and general Southeast US.
Snow accumulation forecasts favor Wisconsin as the big winner per the GFS:
So the GFS takes the system into Illinois and gives Wisconsin the big snows. Let's now turn to the European model.
The ECMWF model, regarded as a more trustworthy model than the GFS, shows the storm system ejecting from the Plains in Oklahoma with a central minimum pressure of 995 millibars. Again, we see that high pressure system in the Southeast which will support the prospect of this storm system staying into the Midwest and Ohio Valley. This forecast is valid for the evening of December 19th.
Moving into the evening of December 20th, we see that our storm system has now strengthened greatly since the 24 hours before, with the central minimum pressure now at 981 millibars. That is a change of 12 millibars in 24 hours- not a common sight away from the Northeast. The tight pressure gradient tells me that this will be a very windy event, and if cold air factors into the equation after the storm departs, lake effect snow could be on overdrive. Also, note that piece of lower pressure jutting out of the southern side of the storm system. This could be a push at another storm system developing, one which could go into the Northeast, but that remains to be seen.
A few images of the ECMWF's precipitation and temperature forecast centered over the Midwest:
Valid the morning of December 20th. |
Valid the afternoon of December 20th. |
Valid the evening of December 20th. |
This is the Canadian's GGEM model forecast for the afternoon of December 19th. Pictured above are sea level pressure (SLP) values for this timeframe, and the colored areas depict 10 meter wind speeds. We can see our storm system in north Texas, being squeezed towards the northeast as pressure from the ridge offshore the Southeast increases. The storm system has no choice but to shoot northeast- that's one thing we're confident in at the moment. The GGEM predicts the system will be much weaker when it exits the Rockies than other models are predicting.
Moving ahead to the morning of December 20th, we now see that the GGEM has taken the system into Indiana with a central minimum pressure of 994 millibars, indicating that some strengthening has occurred. Despite this, the system remains weaker than the GFS and ECMWF are predicting. Even though a strength difference may seem like nothing, I can assure you it can have significant implications. If the system is weaker than is being forecasted, the track can (and would) significantly change. Let's hope that doesn't happen, or this whole post would be moot. We still see that high pressure in the waters off the Southeast. Despite the presence of a tight pressure gradient, 10 meter winds are not showing up too strong, which I can understand, considering the GGEM is weaker than the GFS/ECMWF at this point in time. I am hesitant to disregard the GGEM, because it is in line with the GFS, meaning the two may be on to some sort of consensus.
Now, for the last model we look at, we see SLP values in solid black lines, 850mb temperatures in dashed lines (the same rain/snow rule as the GFS applies here), and precipitation values in colors. This is the NOGAPS forecast, made by the Navy but not regarded as a solid model that you can trust. I'm including it moreso to give some spread to the forecast, not so much to find a solution from the NOGAPS. This model starts out with the system ejecting from the Rockies at a minimum pressure of 993 millibars in the early morning hours of December 19th. Again, watch that timing difference! An already-tight pressure gradient in OK/AR/TX/MO tells me a severe weather situation may be trying to form in that area.
Moving ahead to the early morning hours of December 20th, we find the NOGAPS projecting this system to possibly have split in two. We see one storm system with a 1005mb minimum pressure centered in Arkansas, and another storm system centered in Wisconsin with a central minimum pressure of 1000 millibars. I will refer to them as System 1 and System 2, respectively. System 1 shows a more linear alignment of precipitation, telling me that if this solution verified, we would probably see a mesoscale convective system (MCS) or small squall line in the area as a result of tight temperature and pressure gradients in the region. As for System 2, this looks to be the main piece of energy. The precipitation looks to be a modest snowstorm, with accumulations around the 3-6 inch mark based solely on this image. If the two systems had stuck together, a solution similar to the other models may have evolved. Needless to say, I am discounting the NOGAPS model.
Teleconnections are also a big deal, in terms of the North Atlantic Oscillation (NAO). When the NAO is in its negative phase, you'll see a tendency for storm systems to move up the Northeast coast and strengthen rapidly into Nor'easters. This comes in response to the highly meridional flow set up by the high pressure system in Greenland and the storm system in the Northeast. There are two sub-categories of the NAO, and that is west-based and east-based. In a west-based negative NAO, you'll see the high pressure to the west of Greenland, hence the term west-based. Likewise, in an east-based negative NAO, you have the high pressure system to the east of Greenland. The difference is which one affects which areas. In a west-based negative NAO, you'll see the East US getting in on the most cold and storms, while the East-based negative NAO keeps the cold and storms in the Plains and Midwest. The forecasts for the west-based negative NAO are stronger than the east-based, so it is plausible to think that the East Coast has an advantage. However, because of that Southeast ridge, we'll see the track take a detour north and then go northeast through the Great Lakes. The whole situation is very complicated, but in summary, the NAO does favor a track being shown by the ECMWF or even the GFS, maybe a bit farther south if the negative PNA holds in place.
This image shows what the meteorologists at the Hydrometeorological Prediction Center (HPC) think in terms of best model choice for the next 7 days. Looking at the D4 and D5 areas, we see that the HPC generally leaned towards the ECMWF model, the ECMWF Ensembles (ECMWF EPS) and the Canadian model. Surprisingly, no mention of the GFS model is recorded.
Going off of all the models printed above, the teleconnection forecasts and the HPC forecast preferences, I have made my first call as printed below.
Forecast Preference: ECMWF/ECMWF EPS
Confidence: 55%
Andrew
13 comments:
How is this looking for Colorado (Front Range-Denver area)??
Great forecast, but I'd have to disagree just a bit on your placement of the rain-to-snow area. I think that will be further south, even northern Indiana will see rain change to snow Thursday evening based on the current storm track, with several inches possible.
Awesome! Whats the latest model run for the 26-28 storm. Can you post it?
Thanks Andrew!
what will north central kansas see from this
I highly disagree. The rain/snow line is farther south
There is no blizzard going happen. Temps are to warm.
I beg to differ.I have seen many models this afternoon that point to the rain/snow line to be farther south into northern Newton and Jasper counties in NW Indiana.I have also seen models that put 4-9'' of snow way down in NW Indiana.
The south gets left out again without snow. One more sorry LA nina winter again!!!!
Just remember that this storm is still out in the Bering Sea, and is still four'ish days away, a lot can change, but as of now its looking like a good 6-10 inches of snow for northeastern Iowa southeastern Minnesota and into central Wisconsin,and blizzard conditions would be favorable for these areas as the LP System moves up into southern Canada because of the pressure gradient and that the 32 degree line would be in way southern Iowa. Just out of curiosity though, what is going to the ratio of rain to snow? Thanks Andrew for the AWESOME POST!
Looks like Chicago could get snow out of this system.Are Chicago in the green area or an purple area?
The latest trends are taking this quite a bit further south, as much as 150 miles with the ECMWF, and that would favor Chicago area for the heaviest snowfall. This forecast has the rain/snow line way to far north.
In Milwaukee!!!!!! Bring it baby!!!! Finally!!!!!!
This first call was made using the 0z models, so saying the 12z models indicate otherwise is not related to this first call.
Nicholas: Stormy weather possible. Need to nail down the track first.
Anonymous #1: See above statement.
Anonymous #2: I will try to find the time.
Anonymous #3: Track must be confirmed first. Potentially snow.
Anonymous #4: See above statement.
Storm-Chaser Wx: Indeed, but model convergence is beginning.
Rod: Rain-to-snow as of the 0z suite, all snow (possibly) as of the 12z suite.
Anonymous #5: See above statement.
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