Welcome to the weather blog - a regular Monday through Friday discussion of the weather! 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. While the discussions usually will only come on days I'm working, I'll occasionally issue special updates when the weather warrants. This blog is for you, so I hope you enjoy it! -Matt Noyes
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Matt's Weather Summary:
Midday Update: Trends continue to indicate that damaging winds are likely through eastern New England on Wednesday, especially from mid-morning through mid-afternoon. Winds gusts to hurricane force will be possible on Cape Cod and the Islands, as well as the coast of Maine, and scattered power outages are likley in most of Eastern New England, including the Boston Metropolitan area. We'll continue to monitor this threat carefully - cool ocean temperatures will try to mitigate the wind threat a bit, but concern is that this won't be enough to keep wind gusts of over 70 mph from mixing to the surface in exposed locations and over the water, so mariners should plan to stay in port Wednesday unless you're ready for hurricane force gusts over the water, properly secure vessels in areas exposed to southeast winds, and costal residents should be advised that southeast facing shorelines may see some minor coastal flooding at the time of high tide either side of noon Wednesday.
Previous Discussion:
Dry and cold arctic air continues to modify significantly on Tuesday, but will hold on in the lower and middle levels of the atmosphere for widespread sunshine through high altitude clouds the first half of the day. But a Tuesday morning surface analysis places a storm center over the Western Great Lakes with an attendant series of fronts spread across the Eastern United States - from an eastward moving, moisture-laden cold front in the Mississippi Valley, to a warm front pushing northward across the Mid-Atlantic and heading for New England. This warm front marks the leading edge to warmth and moisture at ground level, but aloft, this new airmass has already begun streaming into New England, and is marked by cirrus clouds spreading into the upper levels of the atmosphere.
This influx of moisture aloft will allow clouds to lower and thicken later Tuesday, as precipitation will move gradually up the Eastern Seaboard and close in on New England. Though this increase in clouds will slow our temperature rise by filtering the sunshine, many communities in Southern New England will still rise above the freezing mark. As precipitation spreads into Southwestern CT around 4 or 5 PM, then, it will fall as a light mixture of rain and snow. This band of precipitation will migrate northeast across the remainder of Southern New England Tuesday evening, reaching Worcester around 7-8 PM as mostly snow, and then continuing to spread northeast - you can always follow the precipitation on radar through my homepage, www.mattnoyes.net. Admittedly, there's some uncertainty with this band of precipitation - our guidance products insist on holding precipitation off until later in the overnight period (around midnight) but it's typical to see a thrust of warm and moist air spread precipitation northward faster than forecasted, and I want to stay on the ball with this regard. While there won't be a lot of moisture that falls with this initial burst of precipitation - less than an inch of snow in most of Southern New England - temperatures will drop close to or below freezing as the band moves through, and roads may become slick for the first part of the overnight. After midnight, most of Southern New England will see a turn to plain rain showers that will fall periodically, however, as temperatures rise. Farther north across the Mountains of Northeast Vermont, New Hampshire and Maine, snow will fall Tuesday night and a plowable snow is likely with accumulations either side of half a foot. See accumlation forecast maps for details of Southern and Northern New England.
The Tuesday night precipitation will be the result of the warm and moist surge of air ahead of the approaching storm center - not the passage of the actual storm. New Englanders will wait until Wednesday for this storm and its attendant cold front to move through, and before its passage, persistent southerly winds will help to flood New England - especially Southern New England - with mild air, and temperatures are likely to rise into the 50's on Wednesday amidst periods of rain, heavy at times, areas of fog and gusty winds. Even the mountains of the north, after Tuesday night snow, will be unable to ward off this warm air, and will see a transition to rainfall, with freezing rain in the deeper valleys of the White Mountains and Mountains of Maine that are most protected from a southeast wind. In Northern Maine, the time table is delayed by about 8 hours, but the results are similar, with a few inches of Wednesday morning snow changing to Wednesday afternoon sleet, snow, freezing rain and rain.
With a widespread 1"-2" of rain expected through much of New England, flooding is a concern for many riverbank communities, especially where flooding has already occurred and will be aggravated. Thunderstorms are likely to swing through New England Wednesday afternoon with the passage of a cold front and as the center of low pressure moves north of New England, and winds ahead of this front will gust over 40 mph in most locales, over 55 mph in the mountains, and up to 70 mph along the coast of Maine and the South Coast of New England! I wouldn't be surprised to see some areas record hurricane force gusts (74 mph or greater) and these winds will bring a threat for scattered power outages to coastal and hilltop locations, especially.
While colder air will be poised to charge in behind this departing storm center, it does not appear as though the same magnitude of arctic cold will be available that we saw this time around, and that will mean a signficantly modified chill for Wednesday night and Thursday, and a quicker return to warmer air. But remember that a change in airmass often is marked by clouds and sometimes by precipitation - we'll see that play out again late Thursday and Thursday night as the next shot of chill recedes, as well. As a result, I have increasing clouds in the forecast for Thursday with a chance of flurries or perhaps a period of light snow or snow/rain mix Thursday night. Behind this disturbance, however, milder air will have returned to New England, and temperatures will respond - even with limited sunshine through clouds - on Friday.
As for the overall pattern and changes that may be in store...we are likely in the process of turning the corner this week, but it will not be a sudden or abrupt change, and instead we may ease toward a colder pattern over the next couple of weeks. The overall weather setup will feature a strong bulging of warm air from the lower latitudes (southern areas) of North America persisting for at least a couple of weeks longer. At the same time, cold air building over Alaska will begin spilling into Canada little by little. The result of this evolution here in New England will be the availability of shots of shallow cold air near the surface over the next 10-14 days, while the active stream of energy and moisture will continue to feed off the Pacific Ocean and across the Lower 48. What this means for us is a delicate balance for a couple of weeks between cold air pulses, and warmth/moisture returns. Time this out right, and we're looking at snow...propensity will be for rain especially in southern New England with Northern New England and the mountains hanging onto every cold shot of air, and the words of meteorologists as to how long the cold can hold as each successive storm draws near. It's undeniable, though, that the overall TREND will be to cool things off in New England over the next two weeks. And as the active pattern continues, that means the overall TREND will gradually be toward a colder and snowier scenario. As mentioned over the past couple of weeks - this could make for a very interesting and active February and March.
Have a great Tuesday!
Matt
Matt's Technical Meteorological Discussion: Updated Tuesday, January 17 at 1:55 PM
A truly extraordinary meteorological specimen is in the making for NewEng over the next 30 hours. What will make this storm so amazing is entirely different from the last storm - it's not the power of a deepening low right over us with a powerful backlash and tremendous baroclinic zone feeding its intensification, but instead this time is the difference between a 1032 mb high east of NewEng, and this 980 mb low that will be closing in. The tightening pressure gradient will be the driving force behind a potentially destructive wind event for Eastern New England.
But let's not get too far ahead of ourselves and take this one step at a time. Cirrus clouds have continued to spill into NewEng from time to time but the sharp isentropic lift associated with moderate 850 mb and 700 mb positive theta-e advection moving northeast toward NewEng is truly creating a rapid thickening of clouds, so there may not be a ton of cirrus to precursor the leading thrust of warmth and moisture. Some subtle changes have been evidenced in the last couple of model runs that modify but do not negate the thought process laid forth yesterday regarding this initial band of precip slated for this evening. The first subtle change is that the sharp speed convergence at 850 mb is deflected westward, from western NewEng into NY state as compared to yesterday's guidance products. This will mean my envisioned heavier bursts of precip embedded in the band will probably verify in these areas, rather than over the heart of NewEng. Still, moderate positive theta-e advection comes thru from about 6 PM Southwest CT to 10 or 11 PM Southern NH, and this will be enuf to carry a band of precip thru. I really don't see this starting as freezing rain or sleet for most of NewEng - the thermal profile, though marginal, is entirely subfreezing excepting Southern half of CT, RI, SE MA. Esp MA Pike northward is subfreezing, and Merrimack Valley/Srn NH is subfreezing through 06Z! I am using the NAM thermal profile preferred over the GFS, but this is done on sound reasoning of superior NAM handling of boundary layer due to higher resolution, upward vertical motion cooling parcels due to expansion, and the dry air that's in place in the lower levels. So, given that the speed convergence is centered farther west, I've lowered my thinking on the burst of evening/night snow for Southern NewEng from 1"-2" to generally an inch or less (maps included in wx summary above). Still, falling after dark and in a subfreezing environment, this will have an impact on roadways and the like. Thereafter, I can justify a period of sleet and perhaps some brief freezing rain through the Worcester Hills and Berkshires, but southeast winds get cranking even tonight and this will scour out cold air at the surface rather quickly. Farther north, my thinking from yesterday holds of a general 4-8" mountain snow, though I've limited amounts in Northern Maine (Aroostook County) given a strong SE flow's ability to carry warmer air into this area.
After dealing with this winter weather, take your pick on the next angle to tackle. I suppose for the purposes of this discussion we'll cover rainfall since I think it's a bit more straight-forward, but from a public perspective it should be wind, wind, wind in your forecasts. As for the rain, though, expect 1-2" widespread but greater than 2" won't be hard to achieve through the mountains of Northern NewEng, and likely draped SW through Central/Western MA, as well. How ironic that as we deal with a mostly rain scenario, the GFS and NAM are in tremendously good agreement on total QPF - when is the last time this happened during a snow event? If this were snow I'd be scared to death because model agreement like this is so hard to find in these dynamic events! But, smoke 'em if you got 'em and enjoy the millions of dollars we've paid as taxpayers for the number crunching. But while you're enjoying the agreement, also notice the tremendous forcing resulting in intense 500 mb upward vertical motion lined up a la squall line from NY to NC. It's climatologically difficult to darn near impossible to get surface based severe convection in NewEng with a deep south and southeast flow preceding the frontal boundary given marine modification of the airmass, but this is so much energy - over 40 units of vorticity - that it should overpower this factor, especially given the availability of moisture in a saturated column. One area that I think needs to be especially on guard for severe convection is New Jersey where a marginally severe thunderstorm event happened last time around, and this time there's more surface and low-level based instability, and winds are south to even south-southwest which will mitigate overall ocean squelching of the convective instability, and with 700 mb flow in this region of over 100 knots (WOW!) in nearly unidirectional flow, the potential for dangerous gusts in momentum transfer alone is significant. Here in NewEng, there may not be a ton of lightning given lift decreasing before reaching high enough into warm midlevels to tap sufficient ice nuclei, but far be it from me to get fancy on this and I think what we have going is fine.
This brings us to what is looking more and more like a destructive wind event for parts of Eastern NewEng on Wednesday. I don't have a time in my recent memory in which the guidance has been so insistent over so many runs on such strong winds widespread through Eastern NewEng. I have to share two things: 1) I've begun to hit the damaging wind threat hard, 2) It's with great hesitancy that I do this. The reasons for hitting it hard are extensive, but can be summarized as follows: A tightening pressure gradient as mentioned at the beginning of this discussion will funnel air across the Atlantic waters south of NewEng and up the Eastern Seaboard. Core of strong winds extends not only through the mid-levels but also down to the top of the boundary layer, with 85 knots progged at 950 mb early to mid afternoon Wednesday. The problem here is that with the passage of the warm front early in the day, most of Southern and Central NewEng is warm sectored wtih mixing indicated by bulk richardson number extending well up into the atmosphere to at least 940-925 mb on average across Eastern Southern NewEng. Now to the reason I meet with hesitancy, which is the cool ocean waters that will, as always, try to impose a shallow cool dome for a protective inversion. More often than not, it seems this inversion wins out, but the most likely method of breaking this and keeping a mixed and therefore windy atmosphere is through pressure gradient force, rather than ageostrophic flow. So, given tremendous agreement, all of these considerations, and the most important consideration that we're talking about a significant human impact from this potential wind event, the responsible thing to do is to hit it hard. This means advising folks of possible effects on daily life as well as marine impact for commercial fishermen. Coastal flooding not impossible at time of high tide before noon at southeast facing shorelines, though worst wind comes later, so it's a close call, but a heads-up has been given in my broadcasts.
Rapid wind shift will be accompanied by cooler air late Wednesday, but certainly not the flash freezes of last storm this past weekend. That being said, temps will fall below freezing in cold advection by midnight Wednesday night, and there's likely still going to be standing water, so icing will still be a concern.
Next series of shortwaves skirt NewEng Thu with orographically induced snow showers, esp early, and mid-level clouds elsewhere Thu night. Still intervals of these clouds Fri with a few shortwaves dampening as they encounter SW flow aloft with broad ridging building SE of NewEng. Low level SW wind should stay active Fri, and felt comfortable - even with somewhat limited sunshine - of boosting temps just a scosh more than I had them.
Really bringing the warm air on for Sat in advance of digging shortwave and developing surface low that will bring rain later Saturday or Sat Night - have seen ECMWF solution of emphatically swinging cold front through before this storm, but at this point have to buy the more consistent and agreed upon solution of taking this front into NewEng, then allowing it to retreat in SW flow ahead of approaching low to perhaps afford North Country snow, but rain elsewhere with a shot of chilly air ready to drop in briefly behind it. Big motivating force in going with this milder solution is the expansive and still strengthening anticyclone near Bermuda, and the northward retreat of the high pressure bubble Friday night into Saturday from the Upper Lakes into Southern Canada.
That's all for today - tomorrow should be interesting for one and all. Good luck.
Matt