After unapologetically blowing the Sunday morning ice forecast, the Philly TV forecasters are now hyping up the “snow event” for this Wednesday.
The latest models have 0.06 inches of water falling as snow on Wednesday afternoon. That amount can be random noise in the models, flurries or a light coating of snow. Hardly a ‘snow event’.
As predicted a few weeks ago, the warm phase we’ve been in over the month of December would likely end by the beginning of January and it seems that’s the case. Whether it’s due to the next phase of the -Madden-Julian Oscillation is anyone’s guess.
The models continue to have trouble with details in prediction more than 3 days in advance. Perhaps it’s because much of the energy is coming off of the Pacific where there are few observation stations.
The next uncertainty will affect us this weekend. After very cold weather for New Years Day, a low pressure system will move in from the southwest. The models have settled on a rainstorm for us Saturday night into Sunday, but there is very low confidence that this storm will really track over the Great Lakes. Development of a secondary coastal low or change in track will vastly affect our weather. So stay tuned.
Either way, if temperatures moderate over the weekend, the moderation will be brief, as a cold cyclonic jet flow will develop for next week.
Over the past few weeks, the weather forecasts beyond 3 or 4 days have been anything but reliable. Perhaps you’ve noticed?
With much of the energy coming in from the Pacific ocean where measurements are sparse, the weather system developments over the US have been difficult to pin down.
We are now going to see a major change in the overall weather pattern, perhaps due to the next phase of the Madden-Julian Oscillation. Over the next week, an anomalously large area of high pressure will settle into the Southwest and Rocky mountain states bringing extremely cold temperatures to areas that last winter were very warm.
We will get colder, but the frontal boundary of this cold air will be not too far to our south.
The disturbances hitting the west coast from the Pacific are expected to be shunted to the south below this boundary.
Here’s the rub– with this sort of scenario, it doesn’t take much for a disturbance to form along the stalled frontal boundary. So instead of just cold and dry weather (as currently predicted by the GFS) we could end up with icy or snowy storms. Stay tuned.