05/16/10 11:05 AM
Upper level disturbances can be a real pain in the next. For example, this morning a very weak upper level disturbance was able to push just far enough north to bring a few widely scattered sprinkles and variable clouds to the region. Those clouds are breaking up now, but they can create havoc with a forecast. Another rather annoying type of disturbance is the upper low that gets cut off and trapped under a building ridge. These types of disturbances are usually poorly forecasted by model guidance and typically have a couple of tricks to pull on your forecaster.
To the left is the culprit that will bring a rather unsettled periods of weather for the northern Mid Atlantic. This upper level disturbance over the Plains this morning will march towards the Ohio Valley by Monday night and slowly move through the northern Mid Atlantic on Tuesday and Wednesday. Now, there are some issues here that are bothering me with the way that the model guidance is handling this disturbance. I’ll name them in a minute, but I’m having a hard time buying into the complete wash out idea on the variety of model guidance, and I have a pretty good idea why the model guidance in some example is pounding locations with heavy rainfall.
When I look at the whole nature of this disturbance in the Plains, the facts come clear to me that this disturbance is not the primary “pattern driver”. What I mean is that this disturbance is moving within the steering currents, not driving them. That’s an important distinction to me. What is happening this week in the grander scheme is that the pattern is shift just as I thought it would to a much warmer pattern for the end of May and for likely much of June. As a result, a large ridge is building over the eastern two-thirds of the United States as the Polar Vortex lifts north and the negative NAO pattern shifts east towards Iceland (not like they don’t have enough problems there with those Volcanoes). Now, what’s happening is that this disturbance is being cut off under this ridge from tonight through Monday night, meandering and WEAKENING as the disturbance drifts towards the Ohio Valley. Why the Ohio Valley? Because the upper level ridge building towards the Great Lakes is forcing the disturbance in that direction!
Okay, so what does this all mean for the up coming week? Well, what this tells me is that the disturbance is nothing more than a weakening connection to the Polar Vortex lifting north, which means that this disturbance will likely end up further north than even currently forecasted. I should note that previous guidance had this disturbance moving through through southern Mid Atlantic and Southeast, and now the trough axis is further north towards New England. So that means the moisture advection from the Atlantic will not be as impressive as shown in guidance as we move forward because all the dynamics will be drawn towards the lowest pressure/heights in Canada.
So let’s piece this all together! I expect tranquil conditions through Monday with variable clouds at times. Moisture in the atmosphere will increase due to the growing moisture advection from the Gulf of Mexico right up the coast. This disturbance will interact with this moisture and create areas of scattered showers and a few embedded thunderstorms Tuesday through Wednesday. However, this is not a disturbance driven on isentropic lifting, but rather increased instability from the mid levels to the upper levels. So, I expect the showers to increase in coverage in the afternoon and weaken in the evening and overnight on both days. The basic rule for both Tuesday and Wednesday is that showers will be an on and off threat. Due to the nature of the atmosphere, these showers will create heavy downpours at times and will be slow to move. Thus while one location remains dry all day, another will have a rather wet day. Again, this isn’t a region wide wash out situation to me, but a day much like what is being seen in the Tennessee River Valley with some locations under the influence of showers and a period of heavy rain while others remaining dry or clearing out fast, and remember this is when the disturbance is much strong than what I expect later on in the week.
Once this disturbance exits, the weather conditions rapidly improve for the end of the week and into the weekend. High pressure will take hold with clear skies and increasing humidity. High temperatures will be in the 70′s to mid 80′s. Still waiting on some data, but I would not be surprised if I have to bump up the high temperatures for the end of the week into the upper 80′s for the Delaware River Valley, which will depend on some wind orientation and subsidence.
Overall though, after dodging some showers this week, the weather pattern will transition to a very pleasant pattern indeed!
For details for your location, check out the seven day forecast!
-- Weather When Posted --
- Temperature: 62°F;
- Humidity: 48%;
- Heat Index: 62°F;
- Wind Chill: 62°F;
- Pressure: 30.16 in.;
7:56 AM
A major change in the pattern is about to take hold if stratospheric considerations are added into the equation.
Over the past several weeks, the Pacific been in a constant shift back and forth between an upper low over the Gulf of Alaska and an upper low over the Aleutian Islands. As a result, much like shaking a long rope, waves of ridges and troughs have passed through the United States with shorts of transient warm and cold conditions. It is interesting to note however that when the troughs aligned that a coastal storm did transpire even under progressive upper level conditions.
Many are keeping an eye on the north Pacific Sea Surface temperatures to determine the coming pattern. I believe this is a mistake. Note that the waters in the north Pacific warmed in October because the upper low was constantly over the Aleutian Islands then the waters cooled as the upper low was wavering into central Alaska and the Gulf of Alaska. The PDO state, in my opinion, is an indication of the pattern but NOT a pattern driver like the ENSO events are. I think this is an important distinction to keep in mind.

The past few days, I have been studying the developments in the stratosphere to see if any warming is developing. With a negative QBO state, the potential for warming in the stratosphere is more favorable and such warming would have a significant impact on the Polar Jet Stream.
I started at 10 MB where I noted significant warming developing above the average rate of temperatures at this level. While warming at this level IS important. What is more important is to see if that warming is working down to the lower levels of the stratosphere. The charts to the left illustrate above normal warming developing at 10
MB, 30 MB, 50 MB, and 70 MB. This is a significant development as we can observe warming working down from 10 MB down to 70 MB, and one also examine the continued warming down into the troposphere as well. Remember, that warming in the stratosphere works much like an air conditioner in your home. Since the warm
air does escape into space, the warm air is forced down onto the troposphere. The pressure on the troposphere causes cooling and pressure falls in the areas of greatest warming. That last statement is very important. Where the warming is greatest is where the troughs tend to form and the jet stream pattern begins to take shape.
So where is the greatest warming developing?
The warming events are centered over key locations that I think will have a significant impact on the Polar jet stream in the coming weeks. First, note over eastern Asia and the Sea of Japan that very warm temperatures are showing up, which would lead to significant cooling in this location and lower heights. A trough in this location STRONGLY points to a negative EPO pattern developing in the coming days. Next, we go to the Canadian Maritimes where once again around 50N/50W, warming is developing. Follow the ideas above, strong warming at the stratosphere leads to lower heights. Lower heights at 50N/50 W suggest an upper low, which would lead to a negative NAO pattern. Finallly, we have cooler anomalies focused over eastern and central Asia, which would suggest the development of a ridge in this location in the troposphere. A ridge in this location is called the Kahir’s connection, which supported colder surface and mid level temperatures in North America. It is also important to note that a great deal of the warming overall is focused over northern Canada, where the cold air supply for the region is located.
Regardless what the models suggest at this run or the next, the stratospheric indications are pointing me to a period of weather for the end of November and early December of colder and stormy conditions for the Eastern United States. The development of the negative EPO pattern will likely force a positive PDO for those that are following these trends. The moderate El Nino will keep the Sub Tropical Jet Stream active and plenty of moisture available.
One should note, that these warming signals do not seem to be waning but rather increasing in intensity. An interesting 90 days are in front of us.
-- Weather When Posted --
- Temperature: 48°F;
- Humidity: 70%;
- Heat Index: 48°F;
- Wind Chill: 43°F;
- Pressure: 30.32 in.;