Wednesday, March 13, 2013

Severe Weather Risk Increases Next Few Weeks

I anticipate the risk of severe weather to increase across the South Plains in the next week or more.

Shown above is a forecast chart of 850 millibar dewpoints. In areas of elevated dewpoint values, the atmosphere is considered richer and more supportive for convection in those areas. The American model predicts a nearly constant flow of moisture from the South and into the Plains to allow for more than one shot at a severe weather event across states such as Texas, Oklahoma, Arkansas, and more. The formation of this flow from the Gulf into the Plains may be enhanced by predictions of high pressure formation in the Plains in the medium range forecast time period. My personal expectation on this potential is we should see the beginning of severe weather season in the next 7-10 days. Granted, we have already seen a fairly active start to the severe weather season, but the official season may very well begin in the next 7-10 days if a storm system is able to intercept this ample moisture in the southern Plains.

Andrew

March 18-20 Potential Winter Storm

The March 18-20 timeframe is being watched for a potential winter storm.

Shown above is a forecast for 500 millibar heights just 5 days from today. We see a sharp dip in the height contours and a cooling of temperatures over the Northern Plains, and it is fron this that we gather where the storm system is. A couple days ago, I was telling of how models would most likely shift back  south and give snow to the heart of the Midwest. Right now, model guidance is in good agreement that the storm track will give the heaviest snow to the Upper Midwest and North Plains.

The reason for this track change is the persistent high pressure in the Southeast. If you look closely, you may be able to see how the height contours (in solid black) begin to spread out when you get into the Northeast and Mid-Atlantic. This is symbolic of high pressure in the area, and we know how high pressure deflects low pressure. The problem with this storm system is that it will not be able to dive deep enough south to move in a track favorable for the heart of the Midwest. If high pressure in the West Coast was stronger, the storm would be persuaded to dive further south into the central Plains. If the high pressure in the East was weaker and not as spread across the Eastern Seaboard as it is projected to be, the storm would have an easier time moving more to the east than northeast. The northeast movement is preferred if there is dominant high pressure spread across the East US, as we will see with this storm system.

Andrew

Long Range Overview - March 13, 2013

6-10 Day 500mb height anomalies from European (left) and American (right) model guidance.
Discussion: Medium range model guidance differs moderately in how the pattern will take shape over the Northern Hemisphere in the next couple of weeks. Both model systems agree in unusually strong high pressure over the Northern Hemisphere. This strong dominance of high pressure will allow low pressure anomalies to form and remain stagnant in perts of the globe. European model differs from American model in potential formation of low pressure in Canada. The American model is much more enthusiastic and allows for low pressure encompassing Canada and bringing about a very zonal (jet stream is west-to-east, no big cold blasts or warm shots) pattern. The European model prefers two centers of considerably stronger low pressure in the Gulf of Alaska and New England. This sort of pattern would allow high pressure to attempt to form in the Plains and Midwest, possibly able to connect to the dominant high pressure over the Arctic Circle.

Negative West Pacific Oscillation index will be provoked in either scenario with strong high pressure in the Bering Sea. The tendency of high pressure in the Bering Sea allows a pattern more supported by the European model, with lower pressure placed in a portion of Canada and not elongated throughout the entire region. Additionally, high pressure instigated by the negative WPO in the Southwest US is more enhanced by the European model, and it is this solution I favor for the next little while. Regardless of which model guidance prediction is correct, a weakly amplified pattern appears to be in store for the United States, and this should allow for a more stagnant pattern- not many sudden temperature swings due to a wild jet stream.

Andrew

Monday, March 11, 2013

March 18-20 Potential Winter Storm

There is potential for a winter storm from March 18 to 20.

Latest forecast from the European forecast model shows our system entering the northern Rockies in the image above, which depicts 500 millibar height anomalies. Cold colors show low pressure, and warm colors show high pressure. I drew arrows for three masses of height anomalies; if you look closely, you will see high pressure systems are shown with red arrows and low pressure shown with blue arrows. The European model allows the storm system to dive into the southern Plains in the next several hours, as high pressure advances east into the West Coast and another body of high pressure in the Southeast advecting north and smothering the East US, as the next image will show.

24 hours later, still using the European model and 500mb height anomalies, we see our system has dropped into the Plains and possesses a neutral tilt. For future notice, if the highest vorticity values are pointing to the southwest (southeast), the tilt is determined to be positive (negative). A positive tilt means the storm is not yet mature, while a negative tilt signifies a fully-mature storm system. A neutral tilt means it is close to becoming a mature storm. As the arrow depiction in the above image showed, the high pressure offshore the West Coast has moved inland and is forcing the storm system to move south-southeast. Corresponding high pressure in the Southeast has made its way into the Ohio Valley and East US.



These first two images are showing the textbook example of a positive Pacific-North American pattern. In the positive PNA pattern, a storm system can dart south as high pressure in the West Coast allows the jet stream to take on a highly meridional (wavy jet stream) flow. As the system reaches the Southern Plains in a positive PNA situation, the energy emerges out of the Plains to move either east-northeast or just northeast, as variable high pressure in the Southeast allows for winter weather potential in the Midwest and Ohio Valley. As an example, the Groundhog Day Blizzard in 2011 occurred during a positive PNA pattern, so you get the gist of where storms can go during a +PNA.

The European model is directing this storm very well with regards to playing out the positive PNA pattern at hand, so let's continue with its forecast.

Another 24 hours later, the storm system has moved northeast in a line from central Arkansas to Michigan. It must be noted that the 500 millibar images do not always show where the storm system's actual lowest mean sea level pressure will be. For example, you may think by the above images that the storm system goes from Kansas to Michigan, but analysis of the mean sea level pressure fields shows otherwise. Let's try to piece together how the system went from the Plains to Michigan. A big player in the movement was that positive PNA pattern. It was this pattern that got the idea for a northeast movement started. This track's movement, if it were to verify, would spell a major snowstorm for the Midwest in typical positive PNA fashion. Another player is that high pressure in the Southeast we mentioned earlier. This enhanced the storm's track further to the northeast rather than a more east-northeast track. I'm a little skeptical of how far north the European model has this system go, because that massive high pressure system over Greenland strongly supports that Southeast high pressure system being very much suppressed. I feel that the European model is greatly underestimating this high pressure over Greenland's effects on the storm's track, and if it was corrected, we would most likely see a storm track further to the south that would really hammer the heart of the Midwest and Ohio Valley before transferring to the coast and then threatening the Northeast. If it does go into the East Coast, I can very well envision a big snowstorm for that area, because the high pressure system over Greenland is supportive of a jet stream pattern favorable for a storm track closer to the East Coast and Northeast. This is how Nor'easters can form.

Now, the European model is fighting a very much uphill battle against other forecasting guidance. Currently, the European model is the only one latching onto this big of a threat. In its defense, the European model is known for catching big weather events in the long range (over 5 days away).

Shown above is a comparison of 500 millibar height anomalies between the American ensembles and the European model, both forecasted 168 hours from now. While both are prone to small differences this far away from the potential event, I circled a major area of difference on both images. In the American ensembles, there is a distinct lack of high pressure in the Bering Sea compared to the European model. The European model has a major system of high pressure over the Bering Sea, while the American ensembles have low pressure over that area. Let's go deeper into this particular issue, because I feel that this key difference will be a major player in the eventual track (or even formation) of this system.

Shown above is a multi-model forecast graphic for the Madden-Julian Oscillation. While some of you may feel overwhelmed by all the action here, let me explain and it should become fairly easy to understand. The Madden Julian Oscillation (MJO) involves 8 different phases. Each phase has different weather effects on the world. The closer the forecast is to the center circle, the weaker the phase of the MJO will be, and thus the effects produced by this particular MJO phase will be weaker. In a similar situation, when the MJO is on the edges of this rectangle, the MJO is in a stronger phase, so its weather consequences for that particular phase will be stronger. Multiple forecast models have the MJO moving into Phase 7 by the time this potential storm rolls around.

This image, courtesy of Americanwx, shows typical 500 millibar height anomalies during Phase 7 of the MJO in the month of March. Again, warm colors show high pressure and cold colors indicate low pressure. If we look towards the Bering Sea, we find very strong high pressure over that body of water when a Phase 7 in March is present. With all forecast models predicting an (albeit weak) Phase 7 of the MJO, it seems like the European model has a better grip on its effects over the American ensembles and other forecast systems rooting against this potential storm. Another atmospheric index that I will not go too in-depth into shows weather conditions that favor the Madden Julian Oscillation in its later stages (including Phase 7), and thus favoring this Bering Sea high pressure.

If we do see that Bering Sea high pressure system, my gut tells me this will be a solid winter storm for someone. A big caveat is that long range models are known to overdo storm systems, and this could be one of those times that this ends up being a weaker event than what current forecasts show. Nonetheless, this certainly bears watching from all parts of the nation, in my opinion.

Andrew

Saturday, March 9, 2013

Accumulating Snowfall in Plains, Midwest

Heavy accumulating snowfall looks to be on the way for parts of the Plains and Midwest in the next few days.

A storm system currently moving out of the Rockies will move northeast through the southern Plains and heart of the Midwest to deliver accumulating snowfall to the central/northern Plains and Upper Midwest. High resolution model forecasts, like the one shown above, depict snowfall reaching beyond the 12 inch mark in Iowa and portions of Nebraska. For anyone who saw yesterday's post concerning that banding in Nebraska, I find it to be no surprise that forecasts have changed yet again and shifted this heavy band. Models never handle these isolated bands of heavy snow well. The purple areas express snowfall forecasts of 6-12 inches of snow, and this looks to be in store for Wisconsin into the heart of Iowa, parts of Kansas and portions of Nebraska. Lighter snow in the 3-6 inch range will fall in the blue regions, and even lighter amounts look to be in store for the light gray colors. Winter weather alerts are posted below.

Legend
Dark Blue: Winter Storm Watch
Light Purple: Winter Weather Advisory
Pink: Winter Storm Warning
Red-orange: Blizzard Warning


Andrew