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May 2018

When One Door Closes…

When One Door Closes…

2018-05-07 11:34:54.000 – Sarah Schulte, Summit Intern

 

When One Door Closes…

…then, well, you can’t get through that door. You’ve tried, but the lock is bolted, and you don’t know the secret knock, and I think Marty might have stolen the key. Luckily, there happens to be a convenient second door to your right that’ll take you to basically the same place, so what was the point of locking the other –

My metaphor is breaking down, and so, coincidentally, is my internship. This is my last week on the summit as a weather observer intern, but I’ve been given a key to a different summit door. I’ve been offered the position of summit museum attendant, which means I’ll be sticking around just a little longer, and I’m so stoked! Experiencing a winter atop Mount Washington has been fantastic, and now I have the chance to see its warmer side.

Before I was accepted for the intern position, I was having difficulty finding a job in my field. I wasn’t sure exactly what I wanted to do, and coupling that with a lack of job-seeking success made the job hunt a very discouraging endeavor. But when I came across the Observatory during my searching, it fit the bill for an opportunity I didn’t want to miss. Research, physical duties, forecasting, public interaction, extreme weather, blog posting, an unfamiliar environment…this was the way to gain experience in many different aspects of a meteorologist’s job. For someone like me, who had begun to lose interest in the field and didn’t know which way to go, this was perfect for testing the waters, giving me a confidence boost and re-igniting my interest in weather.

 

During my four months as an intern, I’ve seen and done so many firsts that I’d lose your interest if I listed all of them. Just in the past four days alone, I’ve seen my first big thunderstorm and hail event on the mountain, gained a new sitting wind speed record of 130 mph and watched the Aurora Borealis! I even learned a new card game (courtesy of our awesome volunteers). During the more wintry weeks, I’ve climbed a snow drift that was over 10 feet tall, seen an undercast around the peaks and eaten rime ice. I’ve also stood on the tallest point in the Northeastern United States with a crowbar in 70 mph winds and beat ice off of what might be the only pitot tube anemometer of its kind in existence. If that’s not a unique intern task, I don’t know what is!

Living on a mountain peak for a week or so at a time wouldn’t be nearly as enjoyable without good people to work with, and I consider myself fortunate to have had the chance to work with some incredible observers. My heartfelt thanks to Tom, Taylor and Ryan for answering my questions (even the dumb ones), teaching me so much about meteorology, mountains and the Northeast in general, and also for putting up with me for four months! Hopefully, you can survive a few more months, as I’ll be returning with the same crew for the museum position. I’ve also loved getting to know the volunteers and the staff at the valley offices, and I’m glad that I don’t have to say goodbye just yet.

 

Working at the summit has given me new appreciation for the Observatory and its mission. Having come from a relatively flat place outside of New England, I don’t think I fully understood just how important the Observatory is for hikers, weather enthusiasts and recreationalists in the White Mountains. When some of our overnight guests told me about how they’d read my forecasts or heard them over the radio, or read my blog posts, or told me how much they loved weather in general, the importance of the Observatory’s work really began to sink in. It’s great doing work you love, but it’s even better knowing that it helps people.

Summing up such an incredible experience isn’t easy, but I’ll try to wrap things up. My internship door has closed, but the summit museum’s doors will be opening very soon! I’m looking forward to seeing the mountains in the summer, climbing one for Seek the Peek (I’m with the Cirrus Contenders) and getting into the groove of my new job. It’s wonderful to see other people get excited about the weather, the Observatory and everything in between. Thank you to everyone who listens, reads and visits; you make me smile! Come visit us this summer, and stop by the museum to say hi!

 

 

Sarah Schulte, Summit Intern

What a Week!

What a Week!

2018-05-06 13:25:15.000 – Tom Padham, Weather Observer/Education Specialist

 

What a week it’s been so far on the summit, with basically all four season’s worth of weather and more! On our way up to the summit last Wednesday we were able to take a photo next to the newly-cleared out wall of snow on the Cragway section of the road. Although we had several big melt outs this winter season, recent heavy snow in April lead to a still impressive 18+ foot wall of snow! Since then warm temperatures and the higher May sun angle have led to plenty of melting, with only patches of snow visible from the summit and the Mount Washington Auto Road should be open for the season within the next few weeks.

 Our shift (Sarah, Taylor, Tom, Ryan L-R) at the snow wall last Wednesday

Friday our next exciting event of the week occurred as a powerful storm system tracked through the Saint Lawrence River Valley. Severe thunderstorms during the late afternoon in Vermont and New York eventually made their way to the White Mountains by the evening, with several direct lightning strikes, small hail, and 120 mph winds. As if winds of this strength weren’t enough, shortly after midnight winds reached an even more impressive 130 mph. These are winds rarely observed on the summit in May, with 135 mph winds in May 1994 being the last time we’ve seen winds stronger than this system. By Saturday morning we also had dropped into the lower 20s°F, resulting in some rime ice and a return to a more wintry-looking scene.

 
Saturday, May 5th Hays Chart showing our peak gust of 130 mph just after midnight 

The cherry on top so far for the overall experience this shift was the aurora borealis (northern lights) seen last night. Night observer Ryan Knapp was able to capture some great shots before the clouds rolled in around midnight. It had been roughly 6 months since we’d last observed the northern lights on the summit, and it just so happened to be on a week when so much else was going on.

Taking in last night’s aurora 

Looking ahead we’ve got a little bit more of a quiet weather pattern for the next few days, which is actually great because we haven’t seen some nice weather since Wednesday. With all of the nice weather, observer Taylor was able to open up the submarine door at the bottom of the tower, which is usually encased in snow and ice all winter. I’m personally looking forward to being able to do some outdoor work the next few days; including some spring cleaning before our summer season starts up in just a few short weeks!

 
This open door is a sign that summer is just around the corner! 
 

 

Tom Padham, Weather Observer/Education Specialist

Chaos During the Facebook lives

Chaos During the Facebook lives

2018-05-02 09:36:05.000 – Adam Gill, Weather Observer/IT Specialist

 

Being short staffed has not been too big of deal so far since we are in between the summer and winter season so the work load is a bit less. The one thing that is being affected is our Facebook lives that we do on the weekend. If any of you joined us for our Friday Facebook live, you would have noticed that there was a distinct lack of sound. Back when Mike Carmon was on our shift, I did all the behind the scenes controlling and could monitor the video. Now it is much more of a challenge trying to control what is going on as well as being on camera. This Friday, while moving the computer into a position where I could be on the webcam as well as move through all the scenes, the microphone came partially unplugged so from our end, it had power. We did not realize until almost half way through the show that the sound was not actually getting picked up and exported to the video stream.

Saturday luckily went ok without any issues and we were able to go outside without any problems but Sunday the camera decided to disconnect as soon as I went outside. Luckily our intern Jill was able to keep the live going with the forecast discussion as I rushed back inside to get the camera going again. The second time was the charm and what had happened was the connection was lost in the tower. With 2 foot thick steel reinforced concrete walls it makes it difficult to get any sort of signal into the tower! I did not run fast enough up the stairs, guess I will need to get my running shoes on and practice!

The plus side is that for every one of these mistakes, something new is learned. With the sound issue from Friday, I know to test to make sure that the microphone is picking up sound. I was doing that when we first started the lives many months ago but became too overconfident. With the camera issue, I need to set up the camera outside so it is already set up and won’t lose connection. With summer this will not be too hard because it is much warmer outside and will not drain the battery of the camera. We still need to find a better winter solution though!

 

Adam Gill, Weather Observer/IT Specialist

April 2018

Satellite Imagery

Satellite Imagery

2018-04-28 09:15:46.000 – Jillian Reynolds, Summit Intern

 

One tool that meteorologists use to forecast is satellite imagery. Satellite imagery is the scanning of the earth by satellite or high-flying aircraft in order to obtain information about it (globalforestlink.com). Different sensors are used by satellites in order to collect electromagnetic radiation reflected from the Earth. Different surfaces and objects can then be identified by how much radiation it reflects.

There are three main types of satellite imagery: visible, infrared, and water vapor. Each type has a unique quality that is very useful for meteorologists.

Visible Imagery

Visible satellite imagery uses reflected sunlight (solar radiation) to see objects in the atmosphere as well as on Earth’s surface. Clouds and snow will appear white on the imagery because they are excellent reflectors. The way to tell between clouds and snow is by seeing if there is movement or not. If there is movement, then it is a cloud. If not, then it is snow. The ground and bodies of water are not great reflectors, so they will appear black on imagery. Since this imagery relies on reflected imagery, it will not be useful at nighttime.

 Figure 1. Visible image. Lighter colors represent clouds/snow. Darker colors represent the ground/bodies of water (weather.cod.edu).

Infrared Imagery

This satellite imagery senses surface and cloud top temperatures by measuring the wavelength of electromagnetic radiation emitted from these objects (called “infrared energy”). High clouds are very cold, so they will appear white. Mid-level clouds are a little warmer, so they will be light gray. Low clouds are even warmer, so they will appear as dark gray or black (sometimes it’s hard to distinguish it from the ground).

 
Figure 2. Infrared image. White represents high clouds. Light gray represents mid-level clouds. Dark gray/black represents low clouds/the ground (weather.cod.edu).

Water Vapor Imagery

Water vapor imagery depicts the amount of moisture that is present in the upper atmosphere (about 15,000–30,000 ft. above the surface). The highest humidities will be the areas with the coolest/white colors. Lower humidities will be shown with warmer colors.

 Figure 3. Water vapor image. Higher amounts of moisture are shown with cooler/white colors. Lower amounts of moisture are shown with warmer colors (weather.cod.edu).

 

Jillian Reynolds, Summit Intern

An Earth Day Poem

An Earth Day Poem

2018-04-22 09:26:19.000 – Sarah Schulte, Summit Intern

 

 

Our planet is full of so many delights

It’s a world that’s unlike any other.

For observers, it’s great fun to ride to the heights,

To experience all kinds of weather!

 

Up here, we’re our own brand of crazy,

to cheer when the winds gust with might

If our record speeds start to look hazy,

we’re crowding the Hay’s Chart all night!

 

There are snow drifts in April that tower

and rime ice that feathers the ground

You’d best not rule out a stray snow-shower;

the Rockpile gets them all year round!

 

And what of the views! When the skies are in sight,

there are so many stars you can spy

The Atlantic can shine with orange morning light

 Auroras may dance from on high

 

 Mount Washington’s truly a jaw-dropping place

There’s nowhere quite like it but here

Lovers of weather and wonder, rejoice!

 For Earth Day, we let out a cheer!

 

It isn’t just weather this planet provides

What about the Earth brings you to smile?

The fields of bright flowers, the birds in the skies,

or the thunder of waves in the isle?

 

Maybe the nighttime delights are your thing,

or the gemstones that sparkle and shine,

the plants that we grow and the food that they bring,

or the people with whom you share time.

 

Whatever you love, wherever you roam,

treat with care all the joys that abound.

We all share Earth’s wonder; we all call it home.

And there’s only one like it around!

 
 

 

Happy Earth Day!

 

Sarah Schulte, Summit Intern

An Epic Storm Summary

An Epic Storm Summary

2018-04-19 06:14:10.000 – Caleb Meute, Weather Observer / Meteorologist

 

As this past shift elapsed, our eyes turned to an impending storm that looked to bring a mess of wintry precipitation and STRONG winds Saturday through Tuesday. We became especially excited through the weekend as the storm setup looked eerily similar to the storm that brought the summit a 231 mph wind gust in 1934. The only difference was going to be the strength of the high and low pressure systems in play, so we knew that it would not be breaking any records, BUT we had a feeling the winds were going to roar. In the days leading up to the storm, the forecast personally had me pulling my hair out (I am bald now) (but not really). The issue was a strong temperature inversion that was going to set up beneath the summit, or so I thought. The colder air at the surface was the result of high pressure to the north sending a backdoor cold front into New England. I mistakenly forecasted for the summit to remain above the inversion and in a layer of air that would be above freezing, thus expecting our dominant precipitation type to be rain during the worst of the storm. As you are likely aware of now, this was not the case…

3 foot long rime ice feather plucked off of the tower! 

Rain, freezing rain, sleet and snow fell on Friday heading into the weekend and the ice already began to accrue atop the Rockpile. Plain rain fell late Friday night, and that was the last time we would have any non-freezing precipitation through Tuesday. One inch of snow and sleet accumulated on Saturday as a warm front lifted through New England (although that warm air remained above the summits). The result was wet snow, sleet and some freezing drizzle. The front stalled out on Sunday and the day was very similar to Saturday, although precipitation fell more as freezing rain and sleet this go around. Sunday was when the hair pulling really took off as my forecast for Monday was determining just how high that temperature inversion would set up as the worst of the storm barreled through.

The wind forecast was okay! The temperature and precipitation type were not. I went to bed Monday morning, already a little exhausted from battling glaze ice that had been accruing on our instrumentation for a few days straight. My anticipation was to wake up and hear the winds roaring, and heavy rain falling, assuming the mercury had risen above freezing. I woke up to what felt like an alternate reality if I am being perfectly honest. Upon waking up in the afternoon, Adam informed me that the temperature was in the teens and VERY heavy sleet had been falling through the afternoon. When it came time for my first observation at the start of my shift, I climbed to the top of the tower where it felt as though I was under fire from an army wielding BB guns. It was not JUST heavy sleet (and I mean HEAVY), it was very large sleet, forming in a convective nature. These large balls of sleet were coming at me at category 1 hurricane strength and occasionally hitting me along a gust over 100 mph. This may “sound” awful, but it was truly remarkable to experience… After my second observation, Adam and I went to the observation deck door to film a quick video to give everyone a taste of what was going on. As we were filming the video, we opened the door and realized the heavy sleet had transitioned to very heavy freezing rain that was causing glaze ice to form at a tremendous rate. The second that my phone was exposed to the freezing rain, wind and cold, it unfortunately died so we could not get the footage we were hoping for. To give you an idea of how hard the freezing rain was coming down, after being outside for a few minutes I came back inside and was covered in glaze ice myself.

I took this right after coming inside from one of my observations. I was outside for a few minutes and became encased in glaze ice!

After filming the video, we came back down to the weather room to watch it. In the middle of it, the building began to shake amidst a loud roar as a rogue gust of wind seemed to come out of nowhere. Adam shouted “WHAT WAS THAT?!” as we both looked towards the Hays Chart and saw the needle pushing towards the outer edge of calibration. We ran over and realized that we hit 131 mph!

Hays Chart showing our peak gust of 131 mph at 8:19pm EDT.  

Adam is okay, so I figure I share this next part because looking back on it now is very funny. He ran downstairs to get our intern Jill, and summit volunteer, John. In a fit of joy and rapid motion, he slid all the way down the stairs to where John was waiting at the bottom and saw the whole thing. The stairs were actually covered in sleet that had blown through the door, so this is understandable. Full of adrenaline, he came back upstairs and we all enjoyed the loud roars of wind gusts consistently hitting 110-120 mph for the next couple of hours before they began to diminish. Freezing rain continued for several more hours before finally transitioning to snow showers by the wee hours of Tuesday morning. By daybreak, it was a fascinating sight atop the Rockpile as every surface was covered in FEET of hard rime and glaze ice. In addition to all of the ice, over 3 inches of liquid precipitation had fallen on Monday, which was composed of freezing rain and 6.7” of sleet! So much sleet was accruing and being lifted up by the winds causing us to report blowing snow, which was actually composed solely of sleet. As you walked through the drifts of sleet, each step you took resulted in a splash as the tiny beads of ice displaced outward. It was another epic storm that I will undoubtedly remember for the rest of my life!
 

 

 

Caleb Meute, Weather Observer / Meteorologist

Spring Around the Corner?

Spring Around the Corner?

2018-04-17 20:08:15.000 – Adam Gill, Weather Observer/IT Specialist

 

With how cool the weather has been across much of the country, many are looking ahead to see when more spring like conditions will begin.  First, why has much of the eastern United States been seeing such cool weather when we had such warm conditions in February and early March? Well in the overall synoptic flow (Large scale weather patterns larger than 1000km across) there has had consistent blocking high pressure over Greenland, which creates a deep trough (Dip in the jet stream) resulting in cooler than average temperatures. Figure 1 below is a plot of the 500 millibar height anomalies for the northern hemisphere over the past month. The warm colors over Greenland and the colder colors over Canada are a good indicator of the persistent blocking that we have been seeing over the last month.

 

Figure 1: 500 mb height anomalies in the northern hemisphere over the last month.

Higher than average snowfall in March and early April has recovered the snowpack lost in the February melt and then some. In Figure 2 and 3 below, snow covers much of the interior North East as well as the Great Lakes region to the Hudson Bay. With northwest flow due to the persistent blocking pattern, air masses are originating from over the deep snow pack. The snow helps insulate cold air as it moves south by both reflecting incoming solar radiation with any heating from the sun going into melting the snow, keeping temperatures near freezing. If there was bare ground, the air mass would heat up during the day as the sun warms the ground and transfers that heat to the atmosphere above it. With how strong the sun is at this time of year, any snow free ground would quickly warm a polar air mass and take away its chill.

 

Figure 2: Current snow depth across the United States

 

Figure 3: Current snow depth across the North East

The good news about this map is that there is not much snow to the south and southwest of New England. Once the weather pattern changes and we get a few days of southerly or southwesterly flow, the snow in the North East will quickly melt, exposing the bare ground to the sun to really start our spring season. We would need a weather pattern with southerly flow to bring in the warm air with sunny skies to last long enough to melt a vast majority of the snow in the Great Lakes region and southern Canada. This will give us a good buffer from the colder air masses as they travel out of the Polar Regions. Losing all that snow won’t necessarily mean that we will be free from the cold weather but the amount of time that it will stick around will be greatly reduced.

Looking ahead in the short term, we will have another colder storm coming in keeping below normal temperatures into the weekend, but beyond that is much more promising for warmer weather. In Figure 4, I have a plot of the 500 mb height anomalies expected early next week. It is a long way out so I am using an ensemble of model to get more of a mean out of a bunch of different model runs with different parameterization to help reduce error in the long range. Looking at anomalies also gives a better idea on if we are going to see a better chance of warmer or colder weather rather than looking at specifics like precipitation or expected high temperatures.

 

Figure 4: Forecasted 500 mb height anomalies for early next week

With those darker oranges over New England, there is good agreement that a warm up is on its way. We will have to see how much snow and ice this warm up will melt! This late into spring, it is possible that after this weekend southern and coastal regions of New England will have seen the last of below freezing temperatures until fall! Up here on the Rockpile, we are prepared to see winter for another few months of winter! We can see snowfall up here in any month of the year!

 

Adam Gill, Weather Observer/IT Specialist

Big Wind Day

Big Wind Day

2018-04-12 13:02:11.000 – Taylor Regan, Weather Observer

 

It’s hard to believe, sitting here amidst the hum of computers, the whir of a humidifier running continuously, and the occasional phone call that 84 years ago to the day, in a one-room wooden cabin chained to the mountaintop where cats outnumbered people, a group of intrepid explorers and scientists experienced, observed, and recorded a humbling wind gust of 231 mph… surviving not only to tell of their experience, but also to verify the accuracy of their measurement. A measurement which stood as the fastest surface wind speed recorded for nearly 62 years, and remains to-date the fastest surface wind speed experienced by man.

In reflecting on the event, and its significance to the Observatory, I thought it would be fun to look at the historical weather maps as well as a few snippets of documentation from the observer log books.

 

Figure 1. Daily Weather Map for Tuesday, April 10th, 1934

Washington, D.C., Tuesday April 10, 1934 – 8 A.M. (E.S.T.)
“A disturbance that was central over Minnesota Monday morning has moved eastward to Lake Huron, Alpena, Mich., 29.40 inches. Another disturbance is central about 300 miles east of Cape Hatteras, Hatteras, N. C., 29.62 inches.”

 

Figure 2. Daily Weather Map for Wednesday, April 11th, 1934

Washington, D.C., Wednesday April 11, 1934 – 8 A.M. (E.S.T.)

“A disturbance of considerable intensity is central over the lower Lake region, Erie, Pa., 29.22 inches.”
 

Figure 3. Daily Weather Map for Thursday, April 12th, 1934

Washington, D.C., Thursday, April 12, 1934 – 8 A.M. (E.S.T.)
“A disturbance of great intensity is central this morning over Connecticut, New Haven, 29.26 inches. Pressure is high from the Rocky Mountain region eastward to the Mississippi Valley, Rapid City, S. Dak., 30.54 inches.”

 

Note how in each of the weather summaries, the verbiage describing the system increases in severity, from simply a disturbance, to one of considerable, and then great intensity. Even with the lack of operating weather stations at the time, enough data was available to discern that a very strong system was set to impact the area.

The following paragraph is a snippet from the observer log books:

“I dropped all other activities and concentrated on observations. Everyone in the house was ‘mobilized’ as during a war attack and assigned a job. The instruments were watched continuously so that they may give a continuous and accurate record of the various meteorological elements at work. The anemometer was particularly watched. A full tank of gasoline made us feel good.-Log Book entry, Sal Pagaliuca

 

Figure 4. Observers Alex McKenzie, Bob Monahan, Joe Dodge, and Sal Pagliuca

One of the most remarkable aspects of this storm was that the gust to 231 mph wasn’t an isolated event. As the afternoon wore on, frequent values of 220 mph were recorded, including several gusts to 229 mph. For reference, a Category 5 hurricane has wind speeds of greater than 156 mph.

The observers at the time captured just how unbelievable this event was in their log book:

“‘Will they believe it?’ was our first thought. I felt then the full responsibility of that startling measurement. Was my timing correct? Was the method OK? Was the calibration curve right? Was the stopwatch accurate?” -Log Book entry, Sal Pagliuca

As we now know, the measurement was in fact accurate, with the anemometer being sent down for confirmation of its accuracy and repeatability after the event. That astonishing value, 231 mph, became the highest surface wind speed ever observed by man, and solidified the importance and value of having a manned weather station atop the summit, a feature which continues to this day.

 

Taylor Regan, Weather Observer

Vernacular Confusion (The Sequel!)

Vernacular Confusion (The Sequel!)

2018-04-06 10:42:31.000 – Sarah Schulte, Summit Intern

 

“We’ll never survive!”

“Nonsense! You’re only saying that because no one ever has!”

Wesley and Buttercup, The Princess Bride

It’s time for more Vernacular Confusion! Don’t worry; it’s not going to be as scary as it sounds. Maybe I should have led with a different quote…

Vernacular Confusion is where I go over meteorological terms that might be misunderstood or misused. Part 1 of Vernacular Confusion had a definite winter vibe to it, so this time I’m going to go over some warmer terms. It is Spring, after all (whether or not it feels that way up here at the Rockpile is unimportant). Let’s get to it!

Pineapple Express/Atmospheric Rivers

Just to start things off, I want to clarify that Seth Rogen and James Franco have nothing to do with this. In meteorological terms, the Pineapple Express is an example of a strong atmospheric river. According to NOAA, atmospheric rivers are “narrow regions in the atmosphere that transport much of the moisture from the tropics to the northern latitudes”.

The Pineapple Express is an atmospheric river that transports moisture from the tropical Pacific (near Hawaii) to the West Coasts of Canada and the United States. The Pineapple Express can drop up to five inches of rain on California in a single day. Not all atmospheric rivers are strong, and their precipitation can prove beneficial to water supplies, but those with the strongest winds and largest moisture contents can cause severe flooding due to extreme rainfall.

 

Diagram of the Pineapple Express from WeatherNation.

Gulf Stream

Let’s move to the East Coast and talk about the Gulf Stream. The Gulf Stream is a current of tropical water that starts in the Caribbean and flows up along the Atlantic Coast. It wraps around Florida and follows the coastline up to the North Carolina Outer Banks, where it takes a more eastward path farther out to sea.

 

NASA image of Sea Surface Temperatures in the Atlantic Ocean. The Gulf Stream is the curl of warmer temperatures along the East Coast.

Ocean-air interactions are a vital area of the study of weather. As stated by LiveScience, “the Gulf Stream affects the climate of the areas closest to the current by transferring tropical heat towards the northern latitudes”. Just as atmospheric rivers transport moisture from the ocean, the Gulf Stream transports heat. This keeps the coastline waters of the southeastern states much warmer than those of the West Coast.

Heat Lightning

Sometimes, particularly in the summer, you might see lightning without hearing the accompanying boom of thunder afterwards, or notice a flash without seeing a cloud-to-ground bolt. The term ‘heat lightning’ is often attributed to this phenomenon. NOAA posits that the term arose because this phenomenon happens most often on warm summer days.

In actuality, ‘heat lightning’ is no different than the lightning from any other storm. As stated by NOAA, “it is possible that you might see lightning and not hear the thunder because it was too far away”. The sound of thunder can only be heard at a distance of about 10 miles from the flash. Seeing a muted flash instead of a lightning bolt is due to interference from ground features or the curvature of the earth. Instead of seeing the bolt, you merely see the bolt’s reflection off the clouds.

 

Distant lightning captured by FOX 25 Storm Tracker Bobby Hines from okcfox.com.

A rose by any other name would still smell sweet, however, so a lightning show by any other name will still be pretty! Just take care to watch these natural shows from the safety of a secure building.

 

Sarah Schulte, Summit Intern

One Windy Day

One Windy Day

2018-04-05 14:20:11.000 – Tom Padham, Weather Observer/Education Specialist

 

Although not quite the storm I was hoping for, the storm that has affected the summit over the past 24 hours has still been very impressive due to the duration of our high winds. For 10 hours straight we observed winds equivalent to a category 3 hurricane (111 mph or greater), with 16 consecutive hours of 100 mph or greater winds. Despite the long duration of winds of this magnitude, our peak gust from the storm was “only” 120 mph, meaning these were extremely steady, but very strong winds. We’ll take a look below at the overall set up for this storm, why we were so excited for high wind potential, and one theory as to why the summit did not see higher winds.

It was anticipated that the highest winds with this storm would occur on the tail end of the system, as high pressure situated over the Southern Appalachians began building into New England from the southwest.

GFS Lamp model numbers for Mount Washington roughly 18 hours ahead of the highest expected winds. Highlighted are gusts that were expected to reach or exceed 112 mph for 7 consecutive hours!
 
 
GFS Model showing the expected surface features across the U.S. Note strong low pressure (974 mb) over eastern Canada and a 1024 mb high pressure system. Image courtesy of Tropical Tidbits.

A very tight pressure gradient between the strong storm system that tracked through the Saint Lawrence Valley and this high pressure set the stage for widespread high winds across New England. This type of set up has resulted in some of the highest wind events ever recorded on the summit (gusts of 154 mph in 1996 and 175 mph in 1942 come to mind, to name a few), but for a system to produce winds of that caliber, a few other factors need to align. Firstly, the location of the high pressure is extremely critical to the strength of the winds (by setting up the steep pressure gradient between the passing Low and the building High pressure systems). Additionally, the atmospheric profile must show a few key elements as well.

Surface weather features for Dec 3rd, 1942. Note the similarities in the location of high and low pressure to our most recent storm. Low pressure on this date was significantly stronger than the more recent storm, however, and resulted in a peak gust of 175 mph!
 
Forecast sounding around the time of highest winds on the summit. The red line (temperature) shows a sharp increase starting near 800 mb. Mount Washington was at about 785 mb during this time, or within this temperature inversion, likely contributing to a more steady, less gusty wind. 
 
These factors are where our current passing system met its downfall, in terms of generating impressive wind gust values. The summit was situated in a very strong and relatively deep temperature inversion, which likely dampened our gust potential. This inversion, or increase in temperature with height seen in the forecast sounding above diminished the air turbulence within that layer and resulted in a very steady wind. This is at least my leading theory on why we did not see higher gusts as one would typically expect with winds of this strength. Still, this was one of the more impressive storms of the winter season, and one I won’t soon forget!

 

Tom Padham, Weather Observer/Education Specialist

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