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Water, water everywhere

Categories: Weather

So we had some rain today.

January is starting out with a bang-it didn’t get above 0 degrees for several days last week, and this morning was 50 degrees and raining. Rain of biblical proportions, with the rain gauge at the track saying .88″ of rain, most of it falling between 7:30-10:30, up to a half inch an hour at times. I’m not going to answer the Middbeat question of “What’s the deal with the weather”, except to say we’ve got some lower atlantic moisture sliding up the coast on the side of the polar vortex in the middle of the country. When low pressure systems like that get squeezed on the sides by intense high pressure, all sorts of funky things happen, like lots of quick rain, or high winds. We had both.

And with the deep freeze last week, storm drains were plugged, iced over, or covered in snowbanks. Rain can’t soak into frozen ground, taxing storm drains even when they are available and working. The landscape department went into overdrive, breaking up ice dams and opening storm drains. The most worrisome spot was solved quickly, that of Voter basement. You know, (or maybe you don’t), that place with all the computer servers. That would be a heck of an excuse for a banner web crash, wouldn’t it?

The northwest door of McCullough, the one that heads either straight towards Munroe and Mead Chapel, or head up the stairs towards Stewart, sits at the bottom of that whole slope below Mead. That entire side slope seems to drain right towards that door. There are several storm drains near there, including what turns out to be a critical one to the right of the door way. This is Jaime and Buzz, wearing hip waders, looking for the storm drain with ice picks and an iron bar. (As always, click on the picture to enlarge)

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And this is the doorway in question, where water was flowing a foot deep through the doors and down the stairs. We actually got the backhoe in there and broke up the iced over snow banks around the entry, and got the water moving down. The plastic and snow was acting like a temporary dam blocking some of the water.

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The Gamut room, in the Gifford pit, started flooding too. That’s Buzz and Jaime again, looking for the tiny little drain somewhere at their feet.

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Yes, I’m the one taking all these pictures. Only barn boots, no hip waders, and I don’t know how to swim.

The drain for this pit is simply down the hill below Mead Chapel. Bet you’ve been sledding over the top of it. Broke the ice around this drain and the pit was cleared in about 15 minutes.

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The last spot we’re still worrying about is on the north west alcove of Battell. This drain is frozen solid, barely flowing at all. We use bags of calcium chloride, and dump them on top of the drain. It acts like a non toxic drain cleaner, flowing down the drain and melting the ice. I’m hopeful this drain will be fixed by tomorrow. I’m not the most patient person you know.

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The true heroes for the day, though, I don’t have any pictures of. There is an entire custodial team known as ‘floor crew’. I don’t even know how many of them there are, but the ones I know on it are all pretty cool. They ran around all day with wet vacs, carpet extractors, blowers, mops, and various other implements of mass destruction. Wherever water was pouring into basements or doorways, they were there, fixing the mess, saving the floors and buildings (and maybe your room!) from the water mess.

 

Cut Off Low

Categories: Weather

All professions seem to have their own language, most of it inscrutable. What’s impressed me about meteorology is their ability to take seemingly innocuous plain words and string them together in ways to make them terribly confusing. While doing a little digging to figure out just what’s been going on with the weather these last couple of weeks I came across the phrase “cut-off low”.

Apparently all of our moist, tropical air we’ve been (not really) enjoying is thanks to the jet stream, which has made up its mind this year to take an exceptionally strange dip southward across the plains. This leaves a path for the heat and moisture to stream northward into New England. A Weather Underground map from yesterday shows it pretty well.

2xus_jt

Not only is the dip odd, but the fact that the jet stream is staying like this for several weeks is striking forecasters as peculiar as well. This is setting us up for what we’ve seen for the last week or two, hot muggy days with the ability to build thunderstorms, the late summer tropical kind with torrential rain only fun to play in when you’re young.

Working, not so much.

Last night’s storm, however, was a cut-off low. Cut off, it seems, from the jet stream. While it should have missed us altogether, instead it meandered up north and east, dumping an impressive amount of rain in northern New York (the forecast called for it to be over us, but it stayed a little to the west).

2xus_sf

Now it is going to poke around Quebec for a while, probably exiting out the Saint Lawrence seaway at some point, once it gets caught back up again in the jet stream. The dip is forecast to be around for a while, so the rest of the week we’re looking at more warm, muggy, tropical August weather. We got .75″ of rain last night, bringing June up to 5.47″ of rain. Last year June had 2.3″ of rain, two years ago 3.1″. That’s why my boots aren’t drying out anytime soon.

A Better Weather Forecast

Categories: Weather

Thanks to an Environmental Grant several years ago, the Landscape department has been running a personal weather station down at the track off of Porter Field Road, with a second more recent station up at Breadloaf campus. We depend on these stations for primarily for snow removal and IPM strategies. The data are also streamed to the Weather Underground, a weather web site that accumulates and posts data for over 10,000 stations across the US.

Any compulsive weather addicts know how tricky it is to forecast weather for a region-most people say the forecasters are “wrong”. A better interpretation would probably be to say they aren’t accurate, and Vermont is a great example of why. The National Weather Service has various offices, and ours is in Burlington at the airport. They cover a large area, from Lake Placid to Montpelier, and from the Canadian Border to Killington. The only way to accurately forecast an area this large is to break it into regions. For example, our region is number 9, Western Addison, including the cities of Vergennes and Middlebury. And here lies the problem with forecasting, particularly in the winter. Middlebury campus is under the same forecast as Lake Champlain, and Vergennes shares the forecast with Brandon. It’s a huge geographical area, and one forecast for such a space is bound to lose accuracy across the region. Addison may get an 1″ of snow, low in the valley, while East Middlebury may be getting hammered with 6 times that, under the same forecast.

The Weather Underground has been taking the National Weather Service forecast, and re-packaging it on their website, along with access to some great radar maps, blogs, photos, etc. Recently, however, they’ve starting forecasting themselves, called Best Forecast, and what makes this different is the data, not only from all of the NWS weather stations, but all of the personal weather stations such as ours. Slate just wrote a great article explaining this. Suffice it to say that Best Forecast is now taking into account microclimates, so when pulling up a Middlebury forecast on the WU, we are getting a Middlebury campus forecast.

How accurate? We’ll find out tonight and tomorrow. The NWS is forecasting a dusting to 2″ of snow tonight, with an additional 3-5″ possible tomorrow before it changes to rain. Temperatures mid 20’s tonight, mid 30’s tomorrow. Best Forecast? Lows of 28 tonight, 50% chance of snow or rain, high of 45 tomorrow, snow than rain in the afternoon, snow accumulations of 1″ possible. I’m not placing bets on who is correct here, but the Best Forecast feels right to me. I’ll post an update when all is said and done.

UPDATE 4PM: The NWS issues forecasts at fairly regular times, 3 PM or so being fairly regular. Their update for the western addison zone has changed slightly, 2-4″ during the day tomorrow, changing to rain in the afternoon, back to snow Friday night with an additional 1-3″. Mid 30’s tomorrow, mid 20’s tomorrow night. Best Forecast has changed little-snow and rain tomorrow, accumulation 1″, chance of ice pellets, snow and rain friday night, only 60% chance, no accumulation mentioned.

UPDATE 12 NOON FRIDAY: The NWS has changed their forecast, as the storm seems to have slowed down from the west. No snow last night, and only light snow now at noon, not accumulating. So do we call this a win for Best Forecast? Both forecasts now are in line with each other for snowfall tonight, 4-6″, but Best Forecast is calling for temps today around 45, with the NWS saying mid 30’s, which it is now. I’d be surprised if temps rise today.

Lightning 1, Spruce 0

Categories: Landscape, Trees, Weather

Anyone around this summer, or past readers of this blog, will remember a large thunderstorm that ripped through Middlebury two days after Independence Day.  Several trees were struck by lightning, which I wrote about after the storm.

The largest tree struck was the Norway spruce in the Main Quad, one of the ones remaining after we removed part of the line. I wrote this summer how the tree was struck at the top, and exhibited a spiral shaped scar all the way down the trunk, exiting at the root flare. We didn’t know if the tree was going to make it or not, but had hopes.

It’s not the voltage that kills trees, but the water. Over 100 million volts strikes the tree, but it is the water heating quickly turning to explosive steam that causes failures. (Another blog post, on a lightning stuck Ginkgo, has much more detail) Damage in trees can be tricky, often with the worst of the damage unseen.

There was damage seen immediately. Long strips of bark went flying across the quad, and a scar opened up, spiral shaped, following the grain of the wood down the trunk. The high sap content of spruce makes it susceptible to such long scars.

I’d been worried about this tree all summer, and was watching it closely. All the limbs near the scar started to die, and the color of the remaining ones seemed a little off, but still green.

During a closer hazard evaluation this summer I discovered two things, one bad, the other worse. The first was the size of the scar, and while this shouldn’t have surprised me, it did.

The scar that formed in the summer seemed minimal. While very long, it only seemed an inch or so wide.

Scar in summer

The bark hid quite a bit of damage, and another small crack that wasn’t even open this summer showed another major wound. Peeling away at the wound showed extensive damage, much larger than we’d first thought. Overall, it seems about 1/3 of the sapwood (the live wood beneath the bark that conducts water and nutrients) around the trunk has died, severely compromising the tree.

I’ve seen trees limp along with scars like this for many years, most often in a forest setting. Trees in communities are connected in several ways, relying on each other for support and nutrients. They also tend to be the best trees for the site, adapted to soil and weather conditions. Trees in an urban or landscape setting are under more stress, either from a singular status in the landscape, more exposed to wind by themselves, or stress from poor soil conditions its genetics just can’t handle gracefully.

This fall was a good one for fungus, with cool moist conditions. The base of this spruce showed a colony of fungi following along one of the major roots of the tree. Later that same month the same fungus appeared following a different root. This indicates a root rot, a type of fungus eating away at the roots of the tree.

I’ve spoken with an arborist friend of mine who suggests immediate removal. He’s seen similar cases, where trees exhibiting root rot like this suffer from wind throw, heaving over in a storm. The clay soils of our quad make this species very susceptible to this, spruce not being a deep rooted tree to begin with, in clay soils even more so.

While I like this tree quite a bit, the chance this tree could suffer a catastophic failure in such a busy location on campus is too much of a chance to take. The remaining tree, the large Norway spruce with the interesting trunk, will remain.

Irene Still Hanging Around

Categories: Weather

Like a guest that just won’t leave, the effects of Irene the Hurricane still seem to be around Middlebury. Primarily what we’re watching now is the Otter Creek.

South Street-flooding in the fields

It takes a while. All the headwaters that feed into the creek have been slowly dropping, like my own muddy Lemon Fair River, and so the Otter Creek is rising. How fast? The football team, at Middlebury for pre-season practice, skipped the weight lifting today and went to fill and stack sandbags at Jackson’s on the River (the old Tully and Marie’s to you alumni) ( The old Woodie’s to you older alumni). (Great little article here).

Another stream feeding the deluge is the North Branch River, the one that falls along Route 125, heading up to Breadloaf and the Snow Bowl. Last I heard, the road is still closed (picture here), although Breadloaf is still accessible by back roads.

Otter Creek Levels-via National Weather Service

As I write, the Otter Creek in Middlebury is at 6.9′, within the top 20 crests of all time, and is thought to reach peak tonight around midnight. Not wanting to wait that long, I took some pictures downtown to try and capture the feel of a simply amazing amount of water, brown and muddy, crashing through town. One of our seasonal landscapers was a dairy farmer in Orwell for 30+ years, and in his experience he’s never seen water so muddy. Another guy in our shop is at home, an island experience, surrounded by water on all sides unable to come to work.

On Battell Bridge Looking East

Jackson's on the River

The Falls

Looking under Battell Bridge

The Bottom of the Sluice

 

 

Irene visits Middlebury

Categories: Weather

Given all the flooding and destruction in the state, I feel very fortunate here at Middlebury, and at my house overlooking the Lemon Fair (flooded, but looks like a normal spring). While we certainly had some damage on campus, it feels relativly minor compared to friends in East Middlebury in need of a new backyard.

Irene brought 3.21″ of rain to the main campus weather station, to bring a wet August total to about 7 3/4″ of rain. The peak wind registered was 37 mph, at about 6:30 yesterday. Breadloaf campus saw 5.13″ of rain, bringing their August rain to 11.27″. They saw a peak wind gust of 39 mph, later in the evening than down in the valley.

No major problems occured on campus. Facilities was busy with their usual leaks here and there, but it didn’t seem any more significant than another big rain. We’d spent a chunk of Friday mobilizing for the storm; gassing and sharpening chain saws, getting wet vacs ready, checking pumps.

Monday morning dawned clear and fresh, and revealed a mid September amount of fallen leaves, along with a plethora of sticks. Some large branches broke in the wind, as well as having a couple of trees topple over. Overall, however, I was pleased with the relative lack of tree damage. This late in the year weak trees are already shedding their leaves, or have thinner than usual crowns, so the more storm prone trees have less “sail” to catch the wind. A large limb heavy with black walnuts fell behind Turner house, but other fruit bearing trees did fine.

The immense rain in a short amount of time causes the most damage for trees. The soil below the tree turns to soup, roots lose their holding capability, and trees can topple in the wind. A good example is a Basswood lost right below Gifford, at the base of the ledge. All the water percolates a little ways down the soil profile, until it hits the ledge, then drains downhill right towards this tree. Combine that with the lack of roots on the ledge side of the tree, and the reason this tree fell is pretty clear.

Basswood below Gifford Hall and Mead Chapel

Another tree with a compromised root system was a Poplar growing out of a stone wall behind the Hadley House Barn. One of our crew members commented how the roots went right through the wall, and this was a good reason to remove sucker trees before they get too large.

Poplar Tree at Hadley House

The rotting root system in the wall

Overall, we did fine. Here’s another couple of pictures of some damage, we’ll have it cleaned up in another day or so.

Blue Spruce by Fletcher House

This one was tricky. A Black Maple on the east side of Old Chapel lost a large limb, breaking another couple, but the limb was held up in the tree by an old cabling system, so extracting the limb from the tree involved some minor rigging and rope work.

Last picture-weeping willows always look so dramatic when broken. This one, located behind the esteemed Francois’ house, lost two major limbs, but had the good grace to avoid the power line right below. He and his dog watched it fall. No, the dog was not in the crate at the time…

A Wednesday Thunderstorm

Categories: Trees, Weather

Last wednesday we had a rip-banger. Thunderstorms developed in the hot summer air over Northern New York, and built as they tracked across the lake. The line continued to build once across the lake, and erupted on top of Middlebury.

I was sitting at home, (I was at work early), watching lightening strike all around us, many up on the ridge of Snake Mountain, some in the fields below. The wind was howling, and sheets of rain poured down. The Middlebury weather station recorded a 20 degree temperature drop in less than a half of an hour, and more than a half an inch of rain in the same amount of time. Peak wind gust came in at 40 mph.

The college weathered the storm ok, but 3 trees took it quite hard. A Green Ash behind Emma Willard (Admissions) took a lightning strike-that was interesting, as it was the shortest tree around, but it was all by itself in the center of the back yard.

Another tree we lost, not surprising, but still sad, was a large Weeping Willow on the northwest side of Battell Beach (the upper Quidditch Pitch). We almost always see Adirondack chairs underneath this tree. The center two stems of this tree had a fast moving fungus that caused a rot in the sapwood of the two center trunks. The sapwood is what carries water upwards to the branches, as well as nutrients throughout the tree, so having this vital structure rot away was a irrecoverable death in waiting. High winds torqued one of the trunks, and broke it away to lean against one of the remaining ones. We removed the tree the next day, before it broke further on someone sitting in a chair.

The final tree may or may not be a casualty, time will tell. One of the large Norway spruces we left in the Main Quad Tree Removal, the most southern one, was hit by lightning. Friends at work in the service building told me it was the most impressive lightning strike they’d heard in a long time. The tree shows a classic spiral scar from the top of the tree all the way down to the bottom root flare. Bark like shrapnel was scattered all over the quad in long 3′ strips, and filled the back of one of our gators. The prognosis of the tree is unknown. The roots seem to be intact-while there is bark peeling on the root flare, it does not seem too bad. Certainly I’ve seen trees recover from worse. We’ll know in a couple of weeks-if the tree is going to die quickly we’ll know soon.

Lake Flooding

Categories: Weather

We’re a little removed from Lake Champlain up in Middlebury, but probably not as far as you think. My own house sits above the Lemon Fair River, draining into the Otter Creek north of Middlebury, which empties into Lake Champlain just north of Vergennes. The lake itself also drains to the north, out the St. Laurence Seaway, which seems counter-intuitive. Everything is supposed to flow south and down, right? Wikipedia says the residence time (the amount of time the lake turns itself over) is 3.3 years. That’s some serious water flow.

The lake peaked a day or so ago at 103.25 feet, that’s the elevation above sea level. It is considered above flood stage at anything over 100′, and seems to spend most of the summer at about 95.5′ above sea level. That means the lake is 7 3/4 feet (!) higher than normal. The previous record, which I remember from a job being a caretaker on a lakefront property, was 101.88′. So all that snow we were cursing this winter? It’s still around.

The Lake Champlain Basin Program has a picture gallery up of flooding and sediment flow that’s worth a look, and below is an animated GIF from the National Weather Service of Hi-Res satellite pictures of the snow melting off the Green Mountains.

Some snow

Categories: Weather

The most remarkable thing about this last snow storm on Monday is probably the fact I almost didn’t write about it. After this punishing winter of snow removal, yet another storm didn’t seem worthy of taking the time to whine. But, after setting some records, I thought I’d write about it, if only so students can brag to their parents.

We don’t know how much snow we got here on campus, as the wind was drifting the snow so radically that some places were devoid of snow, while others were 6′ deep in drifts. I asked the guys in the landscape department how much snow we got, and the answers are unprintable. I measured 20″ in my driveway, but that was pretty windblown too. According to the National Weather Service, Cornwall got 22″, Bridport 24″, so we’re thinking somewhere in that neighborhood sounds about right.

Snow Totals Map-click for larger version

This is one for the record books, both the storm and this winter. The Burlington Weather Service office recorded 25.8″ of snow, beating our Valentine’s Day storm of 2007 by a tenth of an inch. (Incidentally, the record storm was last year, January 2-3, where they got 33.1″. I’ve erased that from my memory) This is the largest March storm, however.

In terms of our yearly records, we’re at 124.3″, third highest total. Number two comes in at 132″, in 1886-87, and the record holds at 145.4″, in 1970-71. I can see us beating 1886, but if we break the ’70 record there is going to be some sore shovelers at Middlebury.

Speaking of sore, yes, there are still some sidewalks not cleared yet. We’re trying! The problem with massive snows like this is that our regular plows just can’t handle it. You can only push a huge pile of snow for so long before the wheels start spinning or you have nowhere to put it. For these types of events we put large snowblowers on a couple of our tractors, but that’s slow going too. And because classes were still being held, the extra sidewalk traffic impeded progress all the more. Uncleared sidewalks means snow shovelers are walking through snow from building to building, dragging a snowblower through drifts.

And on top of all of that, a lot of us couldn’t even get to work. For the most part, the only workers that made it in lived in Middlebury, except for snow miraculous sidewalk tractor operators, who I’m thinking were airlifted in. My own road was roughly plowed by a Monument Farms tractor half the size of my house-the cows have to be fed-but the town plow didn’t make it until the end of the storm Monday evening.

Tired of the snow? If it makes you feel any better, the stake at the summit at the top of Mount Mansfield says they’ve got 90″. That’ll be there a while.

This Winter, explained.

Categories: Weather

Some of our winter weather is controlled by a weather oscilliation know as the North Atlantic Oscilliation, or NAO. This is defined by the difference in atmospheric pressure between an area above Iceland and above the Azores. Ordinarily, low pressure in the winter sits over Iceland, and high pressure over the Azores, and this creates the Polar Vortex, which is simply wind and weather spinning counter-clockwise around the north pole. Picture the two pressure systems as gate keepers, keeping the cold wind spinning around the pole. This strong low pressure over Iceland also draws air from the south west across Eastern North America, giving us somewhat more mild air. Weather scientists call this a teleconnection, or linking of pressure systems across broad geography.

This winter, extraordinary high pressure sat over Greenland, matched by high pressure over Alaska. This caused a breakdown in the polar vortex, causing cold arctic air to dump southward, on top of us. This cold air spilling south is replaced by warmer continental air. A similar event happened last winter as well. Scientists are blaming our colder than normal temperatures and our increased precipitation on this unusual pattern.  Much research is taking place now on this event, known as a Warm Arctic/ Cold Continent.

Average Pressure Pattern

High Pressure, February 2010

The reason for this is a disturbing lack of arctic ice. In January, there was a record setting amount of missing ice in the Arctic, about twice the size of Texas. In the summer, more heat is absorbed by the ocean, which releases in the fall, warming the air above and causing the high pressure. Ocean temperatures are well documented to influence weather patterns, such as the El Nino events, or even hurricane patterns in the Atlantic ocean. And most weather researchers are laying the blame of the lack of arctic ice right at the feet of global warming.

This weather pattern has been breaking down the last couple of weeks, as low pressure is forming in the arctic, creating more sea ice, keeping the cold air locked in the polar vortex. It may be that the groundhog was correct, and our exceptionally snowy and cold winter may be coming to an end.