Winter Outlook 2011-2012
Issue Date: October 17, 2011
Forecaster: Trevor Cole
Introduction:
Winter is right around the corner, so it’s time to take a look at what we’ll expect across the Ohio Valley. We are in times of major change in the weather world, with colder air becoming dominant over warmer air globally. Widespread records have been shattered each and every winter for the last several years across the US and beyond, including the Ohio Valley. December 2010 went down as the fourth snowiest on record with 16.6” (or over 70% of our average yearly total in one month) in Cincinnati. In addition to being very snowy, last winter was also fairly cold overall. This upcoming winter season looks to bring much of the same.
La Nina:
One of the most important factors in long range forecasting is the current ENSO state. This refers to whether the equatorial Pacific is warmer (El Nino) or colder (La Nina) than normal. The state of the ocean has major implications on North American weather. We are headed towards another La Nina winter (similar to last year), with some forecast models dropping the SSTs (sea-surface temperatures) across the Nino 3.4 region to record cold levels. As of the latest reading, La Nina is fairly weak with around a -0.5 degree temperature anomaly. At this point in time, I do not see this episode cooling to strong levels, but more-so a moderate event. It is very rare for a second-year Nina to be stronger than the first, which is one reason why the current CFS (Climate Forecast System) projection seems unlikely (though not impossible).
The image below depicts a typical La Nina winter:

A typical La Nina winter across the Ohio Valley features above average precipitation and above average temperatures. However, the overall setup is not typical, and is why the above graphic needs to be edited this time around. Let’s take a look as to why…
NAO (North Atlantic Oscillation):
The NAO is another important factor when making long-range forecasts. It is essentially a relationship or fluctuation between the two major pressure systems over the Atlantic—the Azores High (subtropical) and the Icelandic Low (subpolar). The way they are set up distinguishes a positive or negative phase. A positive phase can be described as having a stronger than normal Azores High, thus leading to a more northerly storm track across the US and milder temperatures across the Eastern US. A negative phase is just the opposite with a stronger Icelandic Low leading to a more southerly storm track and colder temperatures. The NAO has been in an overall negative phase for the past several months, with brief positive spikes. The NAO is known for frequent fluctuations, which provides for changing weather as opposed to static conditions. I expect this to remain the same through the winter, which will allow for periods of bitter cold, along with periods of milder air.
From the above description, a –NAO favors increased cold and snowy weather across the Ohio Valley and Eastern US during the winter months.
Below is an image of the last few months of NAO readings, along with the CPC (Climate Prediction Center) forecast:

PDO (Pacific Decadal Oscillation):
The PDO, like the NAO, is yet another factor to take into account. The PDO is described as a warming or cooling of Pacific waters around and north of 20 degrees north latitude (which helps distinguish it from the ENSO zone). In a +PDO, the waters across the West Pacific warm while the East Pacific cools. A –PDO is just the opposite. Unlike the NAO, the PDO tends to be multi-decadal. In other words, one phase will typically last over 20 years. Currently, the Pacific is in a –PDO state. One reason why I believe this is an important tidbit is that the storms entering the Western US will be tracking over these colder waters and thus, not bringing a ton of mild air with them. When adding in the fact that the Gulf of Mexico continues to run cooler as well, it will be harder for periods of milder air to hang on this winter.
Clipper Train vs. Major Storms
One thing to begin to think about when forecasting for an upcoming winter season is the main storm type or mode. There are usually two types of storms to choose from, which are either clipper systems or a storm originating in the Pacific or Gulf. This is when things begin to get pretty tricky. If we wind up being around average or slightly below temperature-wise for the season, that’ll mean that we run a higher risk of bigger storms (capable of producing rain, a mix, and/or). This is mainly due to the fact that in this scenario, the persistence of major blasts of bitter air will be lessened, which will allow for storms to track further north rather than suppression occurring. If cold is the rule, then we have a decreased risk for bigger storms and an enhanced risk for clipper-type systems. The NAO plays a significant role in this.
To further complicate things, a snowier than normal winter can occur in either scenario. If the cold wins out and we have clipper after clipper tracking through with high snow to liquid ratios (like last winter), it can really add up. If the opposite occurs, we can have less in the way of frequent snow, but rather two or three bigger events that take us to or above normal by season’s end. For this upcoming winter, I believe we’ll have a mix of the two. I expect frequent, intense cold blasts which bring a favorable setup for high ratio clippers. On the flip-side, I also expect periods of milder conditions to be mixed in as well which either give us risks for rain (and even severe t-storms) or a rain changing to heavy snow event with big accumulations. Heck, if the NAO is just right, we could even run the risk for a massive snow event or potential blizzard with this kind of setup.
Conclusion:
So now let’s get past all of the jargon and get to the point. Overall, I’m expecting below average temperatures and above average snowfall for this upcoming winter. In a typical winter, Cincinnati receives around 23.5” of snow. I’m expecting anywhere between 25-35” for the upcoming winter season. Some areas could see more, some less. It all just depends on the storm track and precipitation type. However, I believe 25-35” is a nice average to represent the entire tri-state area. We’ll have a variety of jet stream setups that should allow for us to see the potential for frequent clipper snows, along with some rain events, ice events, and potentially a large snowstorm or two. I know some forecasters like to go month by month, but I feel that the situation and setup is just too unpredictable to do so. Thus, I’ll keep things simple with a general overview.
