Good early morning bloggers,
Snow is falling and becoming somewhat heavy early this morning, but this has been an isolated area of snow. The National Weather Service issued a Winter Weather Advisory for the Kansas City Metro area through early this morning. This area of snow is surrounded by rain and the snow will likely change back to rain soon, but some accumulation will be likely on grassy surfaces, on the tops of cars, and possibly briefly on bridges and overpasses. As I am writing this it is snowing moderately in Overland Park, Olathe, Leavenworth, and crossing the state line east to Odessa, MO. But, it is raining just north of this area in Gladstone, MO showing the small area where the snow is actually falling. It is 39º at Chillicothe with rain and 33º in Downtown Kansas City at 4 AM and snowing. Take a look at the radar image from 4 AM:

We will continue monitoring this strong disturbance rotating around the powerful upper level storm. We are expecting it to change back over to rain, but will we get our first inch on the Plaza before this happens? It looks like it will be only around a dusting to 1/2" before this band exits the area by around sunrise. Meteorologist Brett Anthony will keep you updated on NBC Action News in HD all morning. The Winter Forecast was issued last night and we are expecting quite a bit of snow this winter. You can read it below, and watch the video from our main website at www.NBCActionNews.com.
WINTER FORECAST 2009-2010
The United States is about to experience an unusually wet winter, as a unique weather pattern has set up across North America and the entire Northern Hemisphere. The weather pattern is cycling and will repeat according to my theory, Lezak’s Recurring Cycle (LRC). This forecast is based on the LRC:
Lezak’s Recurring Cycle (The LRC)
- A unique weather pattern sets up every year between October 1st and November 10th
- The weather pattern cycles, repeats, and continues through winter, spring and into summer. Identifying the cycle length helps tremendously when making long range weather predictions.
- Long term long-wave troughs and ridges become established and also repeat at regular times within the cycle. These dominant repeating features are a clue to where storm systems will reach peak strength, and where they will be their weakest.
- The LRC is a winter-long pattern! There is a pattern! It isn’t just one long-wave trough, storm system, or ridge. It is a sequence of troughs and ridges that are cycling across the Northern Hemisphere. We use our forecasting experience to piece together the LRC for a particular year, and the LRC helps us analyze the upcoming weather.
Analysis of this year’s LRC
Ski areas across Colorado will tell you that something very different is happening this year as they are having a great beginning to their season with many wet snowstorms hitting the high country and some resorts having their earliest-ever opening. The United States as a whole had its wettest October on record. These early storm systems are just the beginning as a unique seasonal pattern sets up.
Here are the dominant features that are becoming evident for 2009-2010 and where they are likely to set up for the LRC.
- A trough near Colorado
- A ridge across the eastern Pacific Ocean between 135º W and 155º W
- A ridge from the Gulf of Mexico extending northeast to the Atlantic Ocean east of the southeastern United States
As usual the jet stream energy will intensify significantly between now and when it reaches peak strength in late January. But remember: the same long-term long waves will still exist through the winter, spring, and into the early summer months. As energy increases into the flow across the Northern Hemisphere, the long waves noted above may look very different at times, and the surface weather may vary, but storm systems will still be falling into the long-wave troughs and rising up over the long-wave ridges. The “same pattern” will seem to have a different look at times, but I will argue that it is still the same one all the way through, with seasonal variations.
Here is a closer look at the main features that will likely affect the weather pattern this winter:
Dominant feature #1: Long-term long-wave trough stretching from Montana south through the Four Corners states.

The above map shows where we believe there is a strong long-wave trough. Energetic flow will quite often strengthen across the eastern Pacific Ocean and drop into the mean trough position regularly during the cycling pattern. This will lead to the development of very wet storm systems across much of the United States. The flow aloft will likely split and amplify at times, providing different looks to this same pattern.
Dominant Features #2 and #3: A long-term long-wave ridge exists from off the California coast at around 140w extending north into the Gulf of Alaska. Another long-wave ridge is located off the southeast coast.

The Pacific ridge is a strong feature that showed up during the critical developing phase of this year’s LRC. You can see where this strong feature is located, above, but it seems strongest at lower latitudes. When this ridge amplifies it will look a lot like what happened in October, as shown above. However, when the flow splits, or becomes more zonal then the ridge well off the California coast would be suppressed south leading to strong western storm systems. There is also a long-wave ridge extending from the central Gulf of Mexico northeast to off the southeast USA coast. This also seems like a strong feature that will return, amplify, and affect storm systems by deflecting them away from the southeastern and mid Atlantic states.
El Niño: El Niño is the periodic warming of the eastern tropical Pacific waters centered over the equator. Warming and cooling occur on a somewhat cyclical basis and El Niño is the warm phase of this oscillation, with La Niña being the cool phase. Together, these are sometimes called the Southern Oscillation and thus the term ENSO, for El Niño-Southern Oscillation. The waters have been warming over the tropical Pacific in recent months, and most forecasts are for El Niño to at least reach moderate strength during this winter before falling apart later in 2010. This will likely have some impact on the LRC this year. The southern branch of the jet stream should be stronger and there may be an abundance of tropical moisture pulled into storm systems forming in the mid latitudes. We have weighted some El Niño influence into our winter forecast.
High amplitude and split flow scenarios

When the flow amplifies there will be the likely development of a deeper western trough with the eastern Pacific ridge in a good position to create Arctic air masses which will then slide down the lee of the Rockies. When the flow aloft amplifies it will lead to a split jet stream with an “El Niño” influence. I will talk more about El Niño below.
When the flow splits the Pacific flow will likely undercut higher heights over Canada and this will lead to major winter storms farther south. The eastern Pacific ridge will be suppressed south allowing for wet storm systems to intensify and threaten the western states with strong and wet storms. This will happen during a couple of stretches this winter, but then the ridge will recycle and develop once again over the western states.

Remember, the weather pattern is cycling. There is about a 15 day stretch that will likely repeat in each cycle where the jet stream will retreat north producing a warm period, but this is not the dominant part of the weather pattern.

Forecast Discussion:
Precipitation: Storm systems will be reaching their peak strength most often as they track inland over the western states and especially over the southern Rockies into the central and southern plains states. We are expecting above average precipitation over a large part of the United States. The exceptions being the northern tier of states and the east coast where average precipitation is expected. The most likely spot to have a drier winter and spring will be the southeastern states. This pattern shows some similarities to the classic El Niño precipitation pattern, except for the southeast being dry. Here is the precipitation forecast:

Temperature: With El Niño strengthening there will likely be some influence on the temperature anomalies across North America, but I am not expecting the usual El Niño forecasts to verify. The eastern fourth of the nation is the most likely area to have a warmer-than-average winter. The western states are the most likely area to have a colder-than-average winter due to the location of the long-wave trough through the Rockies. Thus, the pattern will be more divided between a cool west and mild east, as opposed to the usual El Niño pattern of a mild north and cool south.

Kansas City Forecast:
The weather pattern has set up for Kansas City to have a wet winter with long cloudy stretches. Temperatuures will likely be near average as the cold outbreaks should be balanced by a few warmer and drier periods. We have already experienced a few examples of what this pattern can do when it comes to rainfall, and the most recent storm system is producing snow in the region. We are expecting more storm systems like these and they will be better organized than they have been in recent years.

Last year there were very few snow days in our viewing area. Some school districts didn't even have one. With this pattern we will have at least a few snow days in every school district. Will there be any ice storms? There will likely be a few storm systems with some ice potential, but as usual this should be more likely well off to the south and east with this wet pattern we are in. A few minor icing events are still likely. The chance of a major ice storm is higher to the southeast.
How much snow are we predicting around our viewing area? We are forecasting 20" to 32" of snow. Last year, just within the immediate KC metro area, we had 13" to 22" and a range much bigger than that for the viewing area. And, we average 15" near Pleasanton, KS, and 27" near the Iowa border. So, predicting a range should not be that much of a stretch. It is what will happen this year. Could spots get much more than 32" this season? Yes! But, could a few spots get just under 20"? Probably, but I am not expecting that to happen. I am expecting above average snow and much above average rain!
If you have any questions about this winter forecast please just let us know in the comments section.
Gary Lezak