15 July 2012

Interesting week ahead

The weather over the next couple days will be interesting in the region:
Right now, we're watching an upper level trough get ready to push through the region. This upper level trough is getting plently of assistance from an area of high pressure in the SE. This high pressure is pulling up warm and moist air from the SE and pushing it ahead of the upper level trough. At the surface, a small low pressure centre will drag a trough, which will eventually evole into a cold front, towards the region. This cold front will help advection take place ahead of it and we're going to see some rain showers and perhaps a storm or two in the region today and tonight. Now the western half of the region has questionable chances, but the chances in the east are looking a bit more favourable. Why? Just the timing of the system. The upper trough right now can be found extending from Sault Ste. Marie, ONT. down to Chicago right now. The western half of the region will not see a "Washout", but scattered rain showers and thunderstorms are going to be possible, mainly this afternoon.

Looking at the weather for tomorrow, an area of high pressure is going to slide in from the upper Plains, and though it'll be short lived and get absored by the SE high, it'll be good enough to keep the weather calm in the region for the day tomorrow and for parts of Tuesday. As this high pressure starts to fall, the high in the SE will get stronger and start to influence the weather a little bit closer to the region. However a low pressure with a cold front is going to move down from Canada, via the Plains, and head towards the region.

Tuesday night and into the day Wednesday, the cold front nears, the temperatures anmd moisture will make for an interesting run of advection in the region (I'll type more about this time slot later). And that will create rain showers and thunderstorms in the region. But there is one thing that is going to get a little interesting: the area of high pressure behind the front.

As you may or may not know, high pressures are dense...a high pressure can push a lower pressure out of the way (lows are less dense), but when two areas of high pressure with the same density meet...nobody moves. The cold front will make it to about the Ohio River and then perhaps stall out as the SE high pressure holds it ground and the Canadian high does the same. What does that mean for the region? Well I will have to look further into this and work more with the high pressure, perhaps the front will stall out closer to the region, and if it does...more rain.

I'll be working on the forecasts throughout the morning and early afternoon, so make sure that you check back for updates, because I'll have them. My extended forecasts will be revised a little later this morning. For now, that's the weather!

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