Welcome to the weather blog! While the web address has changed, the blog will still be the same Monday through Friday discussion - with some improvements! Over the course of the next few weeks and months, you'll find me experimenting and adding new features. Maps, pictures, and other multimedia are enhancements I'm hoping to be able to make as I learn more about how to maximize the new site. Format will be similar to the old version - you'll find a general non-technical weather summary below, and when available (most days) a detailed technical meteorological discussion will follow. If no technical discussion is available when you check in during the morning, check back later as it often comes after the Weather Summary - I try to indicate at the end of the general weather summary when/if a technical discussion is coming. My email is contact@mattnoyes.net. This blog is for you, so I hope you enjoy it! -Matt Noyes
For latest radar imagery, to check for watches and warnings, and for links to sites in the world of weather, feel free to click over to my website: www.mattnoyes.net
Matt's Weather Summary:
6:15 PM: Please monitor NECN for updates on the following situation: About 2,000 people are now being evacuated from their homes in Taunton, Mass. - due to possible structural problems with the Whittenden Dam. Anyone near the dam is asked to move to higher ground or to a temporary shelter at Taunton High School.
After a busy weekend of flooding followed by wind damage, things will begin to quiet down in the weather world today. The moisture and energy that brought the flooding rains to New England this weekend merged to form a powerful storm center just northeast of Maine, and it's this storm that delivered the shot of powerful Sunday winds. As this storm very slowly weakens and drifts eastward, away from New England, today, winds will still gust over 30 mph regionwide, but that's significantly weaker than the 40 to 50 mph winds from Sunday, and the threat for damage should be behind us now. As for flooding, those rivers that have not yet receded will begin to do so during the day on Monday, except for portions of the Connecticut river and a few other exceptions. Later this morning, I will update my flood page, linked off of the main www.mattnoyes.net webpage.
So how about the weather from here on out? The overall pattern of the jet stream is going to change markedly for the next week. Remember that the jet stream is the fast river of air aloft in the atmosphere that steers our storm systems and acts as a thermostat, separating cool air to the north, from warmer air to the south. The jet stream for the past several days has been pumping in warm and moist air aloft from the Tropical Atlantic, but now has shifted to a pattern that flows from Northwestern Canada to New England. This will keep energetic but fast moving storm centers diving across New England through the week, each delivering a shot of slightly cooler air.
The first fast-moving jet stream disturbance to affect us is moving across the Great Lakes Monday morning. As it continues its push eastward, it will help to kick out the large storm east of Maine, but not before this departing storm throws back enough moisture for another round of showers in Northern Vermont, New Hampshire and Maine Monday afternoon between breaks of sun. Farther south, a blend of sun and clouds will rule the roost for Monday, where there simply won't be enough moisture available for showers to develop. But a new incoming disturbance will also mean we don't have much time to enjoy entirely quiet weather. As this new disturbance moves east with its attendant low pressure center and cold front, clouds will thicken Monday night and winds will swing around to blow out of the southwest. These southwest winds will bring a breezy day on Tuesday, and while they will be ushering in a warmer airmass, with lots of clouds and a few showers around - especially from mid-morning through mid-afternoon, and throughout the day in Northern New England - high temperatures will be hard pressed to rise much beyond 60, even as the sun tries to break through by late Tuesday afternoon.
Wednesday begins with sunshine after a cool and quiet night Tuesday night, but yet another disturbance at the jet stream level will be swooping in from Canada, caught in the fast winds aloft. This means clouds should increase yet again Wednesday afternoon. This time, however, it appears as though there won't be much moisture to squeeze out in Southern New England, and right now I'm thinking any showers will be confined to the North Country late Wednesday and Wednesday night. The problem for Northern New England is that...with each disturbance pulling through a cold front at the surface...enough cold air may be in place by late Wednesday night into Thursday morning for snow to fall close to the Canadian border. At this point, it's not looking too significant - just a sure sign that winter's not far away.
For the rest of us, the passage of Wednesday Night's cold front may be dry, but it still marks the leading edge to a reinforcing shot of cool air that will bring breezy and brisk conditions on Thursday. In this fast flow of weather disturbances, clouds will thicken again later Friday with rain showers possible Friday night into Saturday, then a steadier rain on Sunday (not our weekend!!) as another jet stream disturbance and the associated surface low pressure center move through. It's still early, though, and I don't like the idea of rain on my weekend anymore than you do, so let's give it time and see what happens.
Have a wonderful Monday!
Technical Discussion: See Below.
Matt
Matt's Technical Meteorological Discussion: Updated Monday, October 17 at 3:30 PM
River flood page has been updated for the final time for those of you looking for everything in one place. Will likely remove the link from mattnoyes.net main page later Tuesday.
Transition to fast flow is underway as upper low east of Maine will pull east and decay while broad weestern ridge/eastern trough pattern sets up across the northern tier of the US. Caught in the fast jet stream flow will be multiple energetic shortwaves that will dive SE across NewEng the next several days, with the amount and intensity of precip they produce dependent largely on available low-level moisture. This broad northeast troughing will persist until the middle to end of the last week of October as lower heights are left in the wake of the current large cyclone and serve as a sink for shortwaves ejecting east from the monster energy diving over and S of Alaska to create a rather intense Aleutian low. While 500 mb heights will remain anomalously high over Northern and Central Canada, effects of the season are enough to result in building cold air across the higher latitudes. Therefore, as energy ejects east and then southeast across Canada heading for NewEng, it will bring with it installments of cool air through the end of October. Thereafter, signs are for the Aleutian low to weaken but remain intact, keeping ridging across the Intermountain region and weak troughing in the Northeast. But the cold shots over the next two weeks may largely exhaust what's available for cold air in Central Canada, and with high heights in that region, warmth building across the western US may morph into a larger scale near to above normal temperature regime for the US, with the Northeast on the outer fringes and still subject to modified cool shots with our weak persisting trough.
Those are my thoughts on the overall longwave pattern, but in the short term winds today are going to gust over 30 mph most areas - some over 35 - but not high enough for damage in most spots. Sunday's 45-50 mph gusts (some higher) were enough to do most of the damage. Still, mentioned that today's winds are enough to cause problems for construction sites, those with tents, and those with banners outside. Tons of low level moisture lingers in the north as well as upslope flow, hence the clouds throughout the day while Southern New England enjoys sunshine excepting the Berkshires and areas downwind of the Berks where upslope developed clouds are being carried by the WNW wind flow.
Tonight skies clear in Central/Southern NewEng briefly but increase again in advance of shortwave and associated low pressure center. Should be a period in Southern NewEng with slackening winds and mainly clear skies which allows temps to drop into 40's...farther north the low level clouds hang on longer and by the time they break up high clouds are streaming in and winds are ready to shift to SW and increase so uniform 40's.
Tuesday intense vort and crashing heights cross NewEng. Increased instability with cooling aloft means plenty of clouds thru the day most spots, tho drying aloft works in behind the vort late and some parts of SW NewEng especially may break clouds to sun before sunset. SW wind tries to advect surface warmth but with most of NewEng hard pressed for sunshine, temps will not be eager to rise. Based on forecast of sunshine breaking thru late, we can get low 60's Southern NewEng, but 40's and 50's north under day-long clouds. Most areas of NewEng see showers with period of greatest dynamic forcing and cyclonic vorticity advection from mid-morning thru early to mid-afternoon. Feature which may have some effect would be surface wave of low pressure developing under the vort and traveling from BTV to Gulf of Maine Tuesday 18Z to 00Z. This will probably keep mid and Downeast coast of Maine locked in fog most of day as well...at least until winds shift behind wave late.
Morning sunshine mixes atmosphere to bring temps back near 60 on average for Wednesday, but I'm not buying widespread mid 60's MOS guidance is touting just yet. Too much chill comes in behind Tuesday's shortwave to retreat it so quickly even with warm advection ahead of Wednesday night's shortwave. My initial thinking was that, without much moisture available, we may even see a dry frontal passage in Southern NewEng but I'm reconsidering give 850 Theta-E shows plume of moisture straight out of the Pacific comes across Plains and OH Valley and interacts with front. This moist tongue may penetrate far enough northeast to produce precip. Farther north, enough energy for strong forcing to crank out rain showers that will change to snow showers later Wednesday night into Thu AM along the Canadian border. Thursday morning an extended period of snow showers is likely in Northern NewEng with the combination of a shot of cool air to the tune of -6 C at 850 mb and upslope flow. Otherwise, downsloping combined with drying brings the sun back out in Southern NewEng and along the coastal plain.
Looks like sun's back on Fri AM, but next in the line of shortwaves is ready to truck into NewEng Friday night into Sat - so clouds increase late Fri and rain develops Fri Ngt and lasts off and on thru Sat. This may not be the innocuous shower event it appears to be at first glance - this energy is the remnant of the UL low over Southern CA today, and will feed off of it's own moisture that it's currently pumping in from the Pacific. With such a fast and active flow in the Northern stream, there is every opportunity for this Southern stream low to merge with one of the energetic shortwaves embedded in the northern flow. In fact, multiple Ensemble members are picking up on this possibility and cranking out a heavy rain event for most of NewEng Saturday into Sunday as ridging amplifies over the Rockies. This amplification relates back to the strengthening Aleutian low mentioned at the start of this discussion - with an amplified Eastern Pacific trof, the Rockies ridge has no choice but to amplify in response. Following this longwave pattern, this favors a pulse deepening of the SE Canada/Ern US trof, which will allow for yet another storm to crank up vicinity NE US. Canadian Ensembles also keying in on this potential and are likely significantly underforecasting potential QPF amounts at this early juncture, marking the axis of heaviest precip from SE NY to Nrn ME with .50", but right now I'd throw that amount away, because this will either be a non-event, or a heavy QPF event and I think we're only seeing the beginning of what will be a wet and wild trend.
Part of the reason for this expected trend is that we, of course, we have Wilma to contend with, and perhaps not just Wilma. Given time constraints, I will bypass a complete tropical discussion on Wilma and the other tropical features, but we have two areas of disturbed weather that I'm most interested in over the Tropical Atlantic - one northeast of Puerto Rico and the other east of the Leeward Islands. As for Wilma, even if she passes over Honduras and is degraded - which I'm not sure will be the case given that her center lay to the north of the deep convection - while she would be torn apart she would come back over the still-warm waters of the Gulf of Mexico, and a strike on the Northern Gulf coast...at this point...seems like a pretty decent solution given the repetitive shortwaves diving into the Lower MS Valley by this weekend with the only-just-begun-to-amplify trough (just getting going Saturday). Additionally, the ridge holding firm over the Central Atlantic will not allow the circulations mentioned above to move northward and away from the US - they have two choices this week by the Leeward Islands: 1) Decay and become a non-player, 2) Move westward. At least one of these circulations should move west and hold together, if not both, though they may have different compositions, as the circulation northeast of the islands currently is non-tropical aloft and only now trying to spin up deeper convection from time to time and failing. This upper low looks unfavorable to become tropical right now, though it has an extremely important role in enhancing outflow on the northeast side of Wilma, which is so impressive it's resulting in convective bands removed well NW of her center. There are two waves located east of the Leeward Islands that are moving west, and indications are that as the leading wave encounters the upper low mentioned above, it will slow and the second wave will be the feature of concern. Though by the time this feature moves far enough west to become a player it may be too late...then again, it may not.
Too late for what? As mentioned above, Wilma looks like eventually she is going to have to come north with a weakness developing in the ridge north and northwest of her. The problem is that as she starts to come north the trough deepening explained above is already underway from the Great Lakes to the northeast. Remember what we've reviewed in these discussions in the past - deepening upper lows will serve as a sink when the pattern becomes amplified. The concern here is that the developing upper low becomes a sink ready to pull Wilma - and perhaps the additional wave east of the Leeward Islands - north/northeast and northwest, respectively. Whether this all happens at once, or one piece at a time it is too early to say, but one would have to think whatever is left of Wilma is not going to be able to ride due north over or west of the Appalachians with the height falls that will be occurring over the Ern US, and instead will have to come north to the Gulf coast, hook northeast, then would feel the effects of the Northeast upper level sink, perhaps pulling the aforementioned wave in as she curls around or over the Southeastern US.
All of this is largely speculation given variable speed of both northern and southern stream waves, and Wilma, but it's going to be hard to see such anomalously low heights over the Eastern Lakes and Northeast, and NOT see at least some of this energy and moisture be pulled into the northeast. If that's not food for thought for you, not sure what is!
Have a good Monday.
Matt