15:32 Thu Apr 23, 2015
What a Peaceful Place to Work!
My office is in the valley at the Weather Discovery Center
in North Conway. I’ve been faithfully manning my desk since I started on January 5th and decided it was time for a change! A few weeks ago I decided that I had a good understanding of staff functions in the valley so I should spend a week on the summit in order to better understand how our staff works and lives together for eight days at a time. Besides, most of the valley staff would be taking time off for school vacation week. My plan was to span both shifts so I can get to know better our entire summit staff.
On Monday Slim Bryant, our summit transportation coordinator, facilitated my trip to the office. The trip wasn’t my usual morning commute. I arrived at the garage about 8:30 AM. The weather was overcast with light wind and temps in the 30s. We were joined on the trip by Meghan Skidmore of the Mt. Washington Auto Road
who planned to film the trip and the Auto Road crew doing the spring clearing of the road. We loaded our gear into the four wheel drive pick-up for an uneventful ride up to Five Mile, near winter cut-off, where the snowcat was stored. We switched our luggage into the snowcat and after a radio check with the Auto Road Crew we were off. Five Mile grade had 10 to 15 feet of snow removed from my previous trip only a week ago. We traveled up and down over water bars through Five Mile grade where we encountered the road crew at Cragway turn. Their snowcat was carving the road out from 10 foot deep snow banks along Cragway. The weather was deteriorating and the road crew looked like they were planning a hasty descent. Slim helped out by plowing heavy wet snow off the road while we ascended Cragway. Beyond it was snowy, windy and even a whiteout for a short distance. We arrived at the summit about 10:30 AM. Just another morning commute for Slim.
After coffee and a snack (you’ve got to keep the work routine pretty standard no matter what) I set up my office, logged-in and began returning emails and phone calls to the valley. My day was uninterrupted and I accomplished quite a bit without the usual, "hey Ed, got a minute?"
, staff visits and normal coffee room chatter. As the weather continued to deteriorate I added some excitement by doing an afternoon ob with Mike Carmon and retrieved the precip can. At 6:00 PM we enjoyed a great dinner prepared by Barbara Marino, our volunteer
for the week. Everyone was excited by the increasing wind with gusts in the 75 – 85 mile per hour range. When the peak gust reached 99 mph I’d had enough of this indoor, armchair quarterback stuff and really wanted to get in the game. You know the feeling. "Hey coach, put me in!"
So off I went solo to retrieve the precip can. Returning safely, I volunteered to de-ice the tower instruments. Off again, up the tower and onto the parapet with my “scientific” crowbar. The gusts made climbing the ladder and holding on with one hand while I beat 3-4 inches of hard water ice off the pitot and wind vane pretty exciting. I’m really glad the wind was blowing the ice away from me. Being hit by one of those missiles wouldn’t have been pretty. After that the rest of the evening was pretty uneventful.
Tuesday and Wednesday consisted of more routine office work along with the usual staff meetings that accompany Wednesday’s shift change. The weather was clear for a short time surrounding shift change and I got out to do a little winter photography. Shortly after we went back into the clouds, the temperature started to drop and frozen precip started again. Of course Murphy’s Law prevailed and Mike Dorfman and I ascended the tower again to try to repair the cable connector for the radio which connects to the Wildcat cam
. We were unsuccessful and it will have to wait for better weather. Another great dinner tonight by this week’s volunteer
Joe Kayan. Last night, I retrieved the precip can and it was snowing and blowing again.
Friday will be a normal valley day in the office. It’s been an incredible experience and I’ve come to really appreciate the commitment and hard work of our staff.
With gusts of only 99 mph I didn’t make the Century Club so I’ll have to come back and try again.
Ed Bergeron, Interim Executive Director
15:52 Wed Apr 22, 2015
A Week on the Summit
Where did the week go? When I arrived the volunteers from last shift kept me company till they were ready to go down. Thanks to John Donavan and Gates Ingram for leaving the living quarters in great shape and even leaving dessert for the evening. Once they were gone it was time to figure out dinner and my shift began!
This is my third time as a volunteer on the mountain, and it never gets old. Baking, cooking, and planning meals is oddly satisfying for someone who never cooks at home. (Have you seen the pantry and kitchen up here? You just can’t fail!). And every day there is time to be outside to meet hikers or just enjoy the weather. Hi to Amanda and her 2 intrepid buddies who had climbed up Pinnacle Gully and then came the rest of the way to watch the sunset from the top, and recharge before heading down. Sunday was gorgeous: they couldn’t have had a better day for the adventure. They were raiding John’s supply of candy and still excited from the ice in the Gully. After visiting with me for a while, they headed down Lion’s Head for a nighttime hike out. I heard that people saw them coming down around 9pm, so they made it ok. I’ll bet they didn’t want to go to work the next day!
Right now the weather is foggy, with low visibility; and the ice that formed yesterday is breaking off the building and falling on the external part of the hood vent. Sounds like it will come right into the kitchen onto the range. Earlier this week the wind was howling out of the SSE and coming right down the hood vent. Dropped the temperature in the living quarters pretty dramatically until we blocked the vent. And we’ve had rime ice…gorgeous stuff and a treat I didn’t expect to see in April. The highlight of the weather week was the thundersnow. Pretty exciting storm to watch and to hear, snug and safe inside the observatory.
Other highlights: Kyle’s meatloaf recipe (think a loaf of ground pork, beef, cheddar crackers, hot sauce, eggs, and cheese wrapped in bacon) was weirdly colored but surprisingly good; Tom finally got up in time to get a breakfast sandwich; Adam had enough hot sauce with every meal to get an ulcer; and Mike led the shift like a pro, including making the executive decision related to spoiled sausage. Ed joined the shift late and was a trooper. Thanks guys for making me feel welcome.
So the guys just came through looking for afternoon coffee and snacks. There are dinner rolls rising, and lots of leftovers for dinner. Tomorrow we head down, and I’ll turn over the kitchen to the next lucky volunteer. Where did the week go?
Barbara Marino, Summit Volunteer
15:45 Tue Apr 21, 2015
Sleet vs. Hail
Non-meteorologist: "It’s hailing outside."
Meteorologist: "No, it’s actually sleeting."
Non-meteorologist: "What’s the difference?"
This is an exchange I've had with friends, family, and peers alike. I always wince a little when hail is mistook for sleet or vice-versa; and I really cringe when it’s assumed there is no difference at all. That's because both are very distinct precipitation types that form under very different meteorological circumstances. It's true both sleet and hail are forms of solid precipitation. But that's about the extent of their commonality.
Sleet is actually a common slang term for "ice pellets." Ice pellets form due to differences in the temperature profile of the atmosphere. The most common scenario in which a location will experience ice pellets is with the approach of a warm front in the winter months. As warm air approaches behind a front, it rides up and over the relatively cold air in place closer to the surface of the Earth. This creates a temperature inversion, or an increase of temperature with height.
With this setup in place, imagine a hypothetical snowflake falling from high up in the atmosphere. As it hits the warm layer of air incoming behind the warm front, it partially melts. Then, if there is enough cold air still in place at the surface, the partially-melted flake will re-freeze into an ice pellet. This is the process that forms sleet.
Hail, on the other hand, is a much different animal. Hail forms under convective circumstances (thunderstorms), when strong updrafts carry water droplets high into the atmosphere, where they freeze and grow into very large ice structures. The structures grow large enough to the point where their weight can no longer be supported by the updrafts, so they will subsequently plummet towards earth. The hail stones fall so fast that they literally drag the air with them, creating very strong downdrafts.
Updrafts of this strength only develop in convective situations, where the updrafts are strong enough to carry the growing-hail stones up to heights of 20,000-30,000 feet, where they’ll meet with supercooled cloud droplets and continue their growth.
Sleet with a thunderstorm is possible, as we just experienced that on the summit of Mount Washington this weekend. However, the sleet still formed under the same mechanism as described above, not as hailstones. Sleet is more of an indicator of the temperature profile of the environment (warm air above cold air), whereas hail is an indication of extreme instability in the atmosphere.
Mike Carmon, Co-Director of Summit Operations
15:41 Mon Apr 20, 2015
Gazing Into the Rockpile's Icy Past
It is late April at the end of a long cold winter and the ravines on Mount Washington are just about full to the brim with snow. More snow may be on the way this week and it’s almost hard to imagine that it will all melt before the snow flies again in the fall. That will probably seem foolish come July, but there have been times in local memories when small pockets of snow endured the summer months tucked away in hidden corners of the mountain, and a few dedicated skiers claimed streaks of 20-30 consecutive months of turns. The lore of perennial snow in the Whites is impressive, but it wasn’t long ago that winter ruled and the mountains of northern New England were saddled with the glaciers that carved the many cirques of the Presidential Range. By some estimates mean summer temperatures would have needed to be 5-9 degrees C below modern-day value to support glaciers in the White Mountains (assuming equal amounts of winter precipitation).
Drawn in by the spectacular cirques of Tuckerman and Huntington Ravines, geologists have been contemplating the glacial history of the range for almost 200 years, although they weren’t always aware of the glacial origins of the ravines. A popular idea of the early 19th century was the “drift theory”, which attributed glacially-derived sediments and striae (grooves on rocks) to a marine flood throwing icebergs against the mountainsides. The conclusion may have been a bit off-point, but the observations and measurements on which it was founded were the initial steps in a lengthy collaboration that has, in today’s understanding, identified no less than 17 glacial cirques on the Presidentials. Some, like the Upper Great Gulf, are classic examples of alpine cirques, with steep headwalls and broad flat floors. Others, like the Ammonoosuc Ravine, are a little less convincing, perhaps due to fluvial erosion that has occurred since the glaciers retreated. All together these cirques have an average height of 452 meters and a total collective volume of 4.21 billion cubic meters!
Aside from identifying the many cirques, there have been a few large-scale questions about the glaciation of the White Mountains, and other ranges in northern New England, that have puzzled those who study it. The morphometry, or shape, of the most pronounced cirques, with defined lips at the upper edge and a high headwall-floor slope ratio, is suggestive that independent alpine glaciers carved the cirques, and that they were not formed by a continental ice sheet or tongues of ice extending down from an icecap centered on Mount Washington and the rest of the range. Continental glaciation has, however, been an active part of forming the landscapes of New England, and the question arose of whether the cirque glaciers outlasted the Laurentide Ice Sheet, which left the moraine of Long Island as it began its recession 15,000 years ago.
Dating the recession of cirque glaciers in the Whites is a difficult proposition due to the limited number of tarns (small lakes that sit at the base of a cirque in the depression formed by the weight of the ice). While the two tarns of the Presidential Range (Spaulding Pond and Hermit Lake) have not been cored for organic material to date, minimum radiocarbon ages for retreat have been determined from cores of Lost Pond in Pinkham Notch (12,870 +/- 370 years) and the lower of the Lakes of the Clouds (11,530 +/- 420 years). These dates are the ages of the first organic material that collected in the bottom of the ponds, and indicate that deglaciation occurred at least that long ago. The question of whether cirque glaciers survived beyond the recession of continental ice is still a debated topic, due in part to complex glacial features (debated provenance of till in cirque floors, presence or absence of terminal moraines on cirque floors) and the lack of high resolution dates for the local recession of the ice sheet. It is still fascinating, however, to look out our windows and imagine the glaciers draped on the sides of the surrounding ridges (and how much fun they be to ski!).
Mount Washington Summit and the Great Gulf Headwall from near Clay col.
PT Davis, Cirques of the Presidential Range, New Hampshire, and surrounding alpine areas in the northeastern United States, Geographie Physique et Quaternaire, Vol. 53, No. 1 (Image Source)
WB Thompson, History of research on glaciation in the White Mountains, New Hampshire, Geographie Physique et Quaternaire, Vol. 53, No. 1
Adam Freierman, Summit Intern
16:04 Sat Apr 18, 2015
From Great To Awesome
As the sun began to rise over the horizon the skies were mostly clear of clouds. Temperatures were slightly above average. The winds were light, at least they were by summit standards. The lovely start to the day was greatly appreciated since it took a while to get the wet bulb reading off the sling. As the morning transitioned into the afternoon the weather turned from mostly sunny to mostly cloudy, and then conditions just continued to worsen.
Just like the forecast was calling for a, weak area of low pressure was beginning to push south from Canada and into New Hampshire. By the middle of the afternoon the outer bands of precipitation started to be seen on the horizon, but it was all falling as virga. With so much dry air in place at the surface the precipitation was evaporating before reaching the ground. As the low pressure continued to push south, enough moisture finally moved in sending the summit into the clouds and bringing showers of snow pellets. More interestingly are the convective aspects that are currently moving through the White Mount Mountains.
While I have been writing this thunder and lightning has been flashing and crashing all around, with several direct strikes hitting to summit. The winds jumped up from about 30 mph to 45 mph with gusts up to 60 mph. As a weather nerd, today was truly an awesome day. It started off beautiful and ended with a bang, literally! Days like this are why I love to work at the Mount Washington Observatory!
Michael Kyle, Weather Observer/IT Specialist
16:54 Fri Apr 17, 2015
Spring Snowstorm On The Horizon?
As our Co-Director of Summit Operations Mike Carmon mentioned yesterday, signs of spring abound across the higher elevations of New Hampshire. Our snow depth is at its lowest point in nearly 3 months, and temperatures have been climbing above freezing on the summit much more frequently the past few weeks. Does this mean we’re done with snow and wintry weather across the higher summits? No way!
Looking ahead at the weather over the next several days, a very active storm pattern will lead to plenty of precipitation across New England through the middle of next week. While the lower elevations will likely see heavy rain and even have concerns for flooding, the very highest elevations of New Hampshire will likely see several inches of heavy wet snow. Tomorrow a quick moving system will dive south out of Canada, with enough cold air in place for mostly snow beginning around noon and lasting into the evening. While this will be a short lived event, precipitation may fall heavily, with isolated thunder not out of the question especially further south and east.
The more interesting storm system will approach the area by Monday, with slow moving low pressure moving into the Great Lakes pulling up plenty of moisture from the Gulf of Mexico and Atlantic. Typically this type of scenario, with low pressure passing to our west, would result in a surge of warm air and likely rain this time of year for the summit. At this time, it appears enough cold air will remain in place ahead of the storm to keep precipitation all snow into early Tuesday morning. This will be followed by only a few hours of rain or freezing rain before more snow arrives on the tail end of precipitation Tuesday night and possibly into Wednesday morning. With such a slow moving system, snowfall amounts could be impressive for this time of year, possibly exceeding a foot if enough cold air remains in place throughout the storm. This serves as a reminder that although spring seems to be here in the surrounding valleys, winter conditions can be seen at any time of year on Mount Washington.
Tom Padham, Weather Observer/Meteorologist
15:07 Thu Apr 16, 2015
I stepped outside for an observation earlier today. After utilizing the sling psychrometer, the temperature read 37°F, with plenty of sunshine overhead, and a warm 25 mph breeze. I remarked to no one in particular, "wow, it's really warm out here." And then I thought twice and chuckled to myself.
Where does 37°F feel "really warm"? The summit of Mount Washington, that's where.
After an impressively cold winter season in which we've seen over 300 inches of snowfall (so far), temperatures struggling to rise above zero degrees for days on end, and winds gusting to some of their highest levels in the last decade, 37 degrees and sunshine in fact feels like a mild spring day for us summit folks. I'm not quite ready to bust out the shorts, but add another 10 degrees and reduce the winds to near-calm, and you'll be left with Mt. Washington t-shirt weather.
The landscape reflects the spring fever as well. Patches of bare sedge and rocks are now much more ubiquitous around the summit cone, and the large snow drifts are steadily succumbing to the increased solar radiation.
This time of year also means more complicated transportation up and down the Auto Road for our shift changes. Yesterday, we ascended up a little more than half of the road in a truck and van, and then hopped in the Snow Cat (after transferring all gear and personnel) for the notoriously snow-laden 5-mile and Cragway sections to the summit.
Summer is coming, though, and we'll be ready and waiting for it!
Mike Carmon, Co-Director of Summit Operations
08:21 Wed Apr 15, 2015
SO MUCH TO EXPERIENCE!
When you step out of the Snow Cat upon arrival at Mount Washington Observatory the experiences start piling up. Driving almost vertically up a 20 foot snow pile to clear the entrance for unloading, we've arrived. A well organized fire line of Observers and Volunteers
pass along the many backpacks, food and gear that is arriving, then pass along the many backpacks, trash and gear that is departing. Now to unpack, organize the kitchen and plan the night's first meal. Done! Let's get in our mountaineering gear and go outside and see what the weather is doing. All righty then. we have rain, freezing rain, freezing fog, ice pellets, snow and LOTS of wind. I experienced a105 mph sustained wind and a 117 mph gust that taught me how to fly. What an experience THAT was! I went hiking to a nearby Crag and enjoyed a lunch in a Snow Cave protected from the wind and listened to melting streams of snow and ice crackling underfoot. I did laps in wet snow on the Summit Cone as continued training for Seek The Peak 2015
. When you Volunteer at Mount Washington Observatory, you also get to interact, host, as I call it, with Edu-trip overnight guests. We hosted a very interesting three day visit from an AIARE
course, held by Eastern Mountain Sports Climbing School
. A wonderful, hearty group of outdoor adventurers willing to brave The Home of The World's Worst Weather to learn about avalanche protocol. We made sure they were well fed so they would have the energy they needed to brave the elements. After dinner, conversations at our community dinner table featured talk about their days' adventures, personal backgrounds and the world in general. You meet so many interesting people while Volunteering at MWOBS
. The groups are now gone and the population goes from 16 to 6. It's much quieter, except for the 100 mph Winds howling along the outside wall of the Obs Tower, and life slows down. We are here during the 81st anniversary of BIG WIND DAY
and we baked a cake to commemorate the occasion and had a chance to bond more with the Obs crew. What a GREAT group of dedicated people! Now the HARD part, time to start thinking about packing up and going home. I'm already thinking about my next chance to Volunteer in the Fall. You know, you can Volunteer
also! Go to www.mountwashington.org
to check out how to Volunteer. All these experiences and more could be yours!
John Donovan, Summit Volunteer
20:23 Tue Apr 14, 2015
Ramblings from a Volunteer
As a Boy Scout it was my first time up Mount Washington with a troop from Dover, NH. I learned very quickly that you don’t take this mountain for granted. While ascending Tuckerman Ravine trail I witnessed a body in a stretcher being brought down from Lunch Rocks. It was death #38 as noted in Not Without Peril
by Nicholas Howe. That number has now been exceeded by over 100. You can find the book
at the Weather Discovery Center
gift shop in North Conway and read about it on page 182.
As a volunteer cook, this is my 10th time serving crews that record weather conditions found nowhere else in the world 24/7/365. This information is needed by scientists, government agencies, universities, media, military, right down to hikers, skiers and recreational enthusiasts. I believe Mount Washington and its environs have one of the highest number of recordable deaths in the world; this on a mountain that is just over 6200’ and has made information available to warn and prevent further incidents.
Walking about the buildings on the Rockpile in the quiet, the history and questions about that history are ever present. What signals and information are passed up and down the antennas of Yankee Building? Who of importance stayed in the Tip Top house? What about the former summit hotels, now replaced by the Sherman Adams Building? I’ve seen folks lounging near the Cog tracks opposite the entryway to State Park’s Gift Shop and the Observatory’s Extreme Mount Washington Exhibit
; but I’m still waiting for the moose to show up.
Gates Ingram, Summit Volunteer
06:28 Mon Apr 13, 2015
Sunny and Mild
If one had to summarize Monday in three words it would be “sunny and mild.” While these three words will be departing our vocabulary a bit Monday night into Tuesday, they will be returning to the region for the midweek. High pressure, which will be providing the fair weather on Monday, will be sliding offshore heading into Monday night as a low approaches to our northwest. As the low passes to our north, it will be dragging a trailing weak cold front with it, which will approach from the west. As this front passes, it will bring some light rain showers to the lower elevations Monday night into Tuesday. For higher elevations, rain will be seen at the start, however some peaks may see a wintry mix on Tuesday as a secondary cold front swings through. As the front exits, high pressure will be rebuilding from the west for Wednesday and Thursday bringing a return of spring-like conditions and those three magical words - sunny and mild. Looking further ahead though, unsettled weather will then be returning as we head into the weekend.
The view at the start of the sunny and mild Monday.
Monday - High pressure exiting and a cold front approaching from the west.
Tuesday - A cold front and associated rain showers sweep through the East.
Wednesday - High pressure returns and with it, sunny and mild conditions.
Ryan Knapp, Weather Observer/Staff Meteorologist
14:38 Sat Apr 11, 2015
Glaze Ice Galore
It’s crazy to think that since I started interning in mid-January, I had yet to see temperatures above freezing on the summit until just yesterday, when we peaked at 44˚F in the afternoon.
These temperatures brought about a slew of different weather phenomena as we transitioned through the freezing line. I found the abundance of glaze ice yesterday morning to be particularly interesting, so I figured I would talk about it a little bit.
So what is glaze ice?
Back in February, I explained the formation of rime ice, and discussed how water can exist in a supercooled state, which means that it stays as liquid water below 0˚C or 32˚F. The water forms rime ice when it freezes after coming into contact with a surface.
Going off of this basic definition, glaze ice is essentially the same thing as rime, but with some differences.
To start, we’ll talk about the difference between freezing fog and freezing rain. Freezing fog leads to rime and freezing rain leads to glaze, so there’s a big connection here.
First, let’s take a look at the difference between a cloud droplet and a rain droplet. The cloud droplet exists as a liquid in a supercooled (below freezing yet still liquid) state whenever we experience freezing fog, and the rain droplet also exists in a supercooled state, except during a freezing rain event.
For our purposes, the primary difference between a rain droplet and a cloud droplet is the size. Rain droplets are much larger than cloud droplets. Take a look…
Image Courtesy of Dr. Robert Houze, University of Washington Dept. of Atmospheric Sciences
Nate Iannuccillo, Summit Intern
The smaller cloud droplets freeze more quickly than the much larger raindrops, and air gets trapped during the rapid freezing that occurs. This makes rime ice far less dense than glaze ice, and produces its white coloring. Conversely, glaze ice is relatively clear, and much denser and heavier than rime ice. This makes glaze much more dangerous when it accumulates on overhead objects.
With significant glaze accumulating yesterday morning, it felt quite necessary to wear a helmet going outside to de-ice with these heavy blocks of ice flying around.
Later last night, as we returned to sub-freezing temperatures, rime became the dominant form of ice once again.
Here’s a picture of a large chunk of glaze ice that I pulled off of the A-frame yesterday. You can see the contrast between glaze and rime quite well here. As the block of ice sat outside overnight, rime ice began to accumulate on top of the glaze ice. The color difference is quite noticeable. Check it out!
16:47 Fri Apr 10, 2015
Spring is Coming!
While the valleys have been experiencing on-again, off-again spring weather for the last few weeks, the summit has generally still been in full-on winter mode. We only recently broke our streak of below-freezing temperatures a few days ago on April 3rd! But in the weeks ahead we will be slowly transitioning into summer "warmth" (think 40-60 degrees) and seasonal risk of thunderstorms!
The front that brought severe storms to the Midwest yesterday is passing over us this afternoon and is resulting in some lightning strikes to our north and south. One of the most exciting but dangerous weather phenomena that we experience during the summer are convective storms that often roll over the summits. We get direct lightning strikes to the summit on a regular basis, so we must be extremely careful about our safety. The only times we don’t go outside for our observations are during these lightning events.
As the summits slowly transition from winter to summer, hikers who wander above tree line may encounter the dangers of cold weather risks (hypothermia, frostbite, etc) as well as potentially deadly warm weather risks such as thunderstorms or sudden downdrafts! Before wandering above tree line, be sure to check out our Higher Summits Weather Outlook
. Additionally, while it may seem safe by this late in the season, snow in the mountains continues to remain unstable (for example, there were three human triggered avalanches reported Thursday alone). To better understand what you're heading into when heading onto steep snow, be sure to visit the Mount Washington Avalanche Center's page to see their latest forecast
Michael Dorfman, Weather Observer/IT Specialist
17:34 Thu Apr 09, 2015
Do April Showers Really Bring May Flowers?
We have all heard that April showers bring May flowers! But do you think the flowers will be extra pretty in May because the April showers seem to be of the snowy consistency?
That's the story again for this weekend, which currently looks to be quite the mix. Friday will see an area of low pressure moving over the Great Lakes region, ushering plenty of moisture into the Northeast. Ahead of the low, a warm front will pass, allowing temperatures to rise. However, as the low passes, a cold front will move through and send temperatures plummeting once again. So what's the result? Rain to start, then a transition to sleet, and finally snow will likely follow overnight into Saturday morning. Any remaining precipitation should move out by Saturday afternoon.
Friday 8AM: An area of low pressure situated over the Great Lakes region brings a surplus of moisture into the Northeast. Image courtesy of The Weather Gun
Friday 2PM: The low slowly progresses, bringing a steady amount of precipitation to the state. Image courtesy of The Weather Gun
Saturday 8AM: A cold front follows, allowing any lingering precipitation to transition back to snow. Image courtesy of The Weather Gun
Kaitlyn O'Brien, Weather Observer/Education Specialist
Well, this certainly not the best news around, but who knows, maybe those flowers in May will be worth it!
20:10 Wed Apr 08, 2015
Observing the Observers
Our shift ran Wednesday to Wednesday, April 1-8. The Bombardier Sno-Cat brought us up the Auto Road
bumping and shimmying, often times pushing drifted snow as we proceeded by birch poles marking the edge of the road. Some stuck up only inches from the snow road's surface, even though some of the markers are over 10 feet high. Occasionally pavement was bare due to the windblown conditions, especially near the top.
The Observatory staff was generous to let us ride up front. Our driver, John, offered interesting commentary and answered questions. We lucked out with spectacular weather. We could see all the way to the Atlantic Ocean, which appeared as a shiny band of silver in the distance.
The week brought interns interviewing for summer positions, a Plymouth State University presentation about the effect of the boundary layer's elevation on weather data at the summit; and two groups who had hiked up, led by guides from Eastern Mountain Sports
and International Mountain Equipment
. We were happy to share the newly remodeled bunk rooms with very appreciative overnight guests.
We enjoyed seeing Observatory website acronyms: SN BLSN FZFG for Snow, Blowing Snow, and Freezing Fog. The weather we experienced this past week included temperatures ranging from -3 F to +35 F, a peak wind gust of 98 mph, and an average wind speed of 47 mph. The Rockpile received its first rain showers of the year, but also saw an impressive snowfall of 22.6" for the week. Visibility ranged from 0 to 120 miles.
We were treated to two red-sky sunsets with clear evening lights of distant towns and ski areas. It was equally impressive to stand at the Observatory windows seeing clouds, fog and snow fly by. Thank you Mt Washington Obs staff for being so polite, informative, and hungry for the food we prepared. Being with you for the week has been a total pleasure.
Brenda and Preston Conklin, Summit Volunteers
21:17 Tue Apr 07, 2015
Interesting Snow (And Lots Of It!)
What a weekend! Above freezing temperatures and warm wet fog really decimated our snowpack on Friday. The summit cone was showing more sedge than snow and the cols and peaks along the ridgeline were looking pretty rocky. Things quickly got wintery again on the rockpile, however, as we’ve picked up 22“ of snow since Saturday and our snowpack is now deeper than it been for most of the winter. This snowfall has been a bit different than most we have seen this winter as well. Slightly warmer temperatures and relatively light winds mean that instead of watching this snow blow away in giant plumes, it has drifted considerably on the summit. Of course this made for quite a day of shoveling…but what better way to enjoy the sunshine.
With varying temperatures throughout the weekend we also saw a great variety of snowflake types. Along with the dendrites and needles we collected rimed crystals, spatial dendrites, and these beautiful capped columns that Kyle caught yesterday afternoon.
These crystals start by forming as hexagonal columns or prisms, which is a simple and common snowflake geometry. They are then blown into a part of the cloud which is at a different temperature and crystal growth transitions to plates, which grow on each end of the column resulting in a spool-like capped column.
Adam Freierman, Summit Intern
17:05 Mon Apr 06, 2015
Chocolate, Snow, and King Marty
Easter has come and gone on the summit, and most of the staff up here won’t be able to look at chocolate for quite a while. I may have gone a little overboard with the amount of candy I brought up for the holiday. But I can safely say it was enjoyed by all yesterday! Between the candy, snacks, appetizers, the awesome meal cooked by our volunteers, and the inevitable dessert, it was surely a holiday fit for a king!
King Marty, on the other hand, hasn’t seemed to have had his fill at all. I caught him snooping through our leftovers this afternoon. Who knew his sweet tooth was so unrelenting?
With the amount of snow we’ve seen up here since Saturday (we’re up to 12.6 inches, and still counting!), it felt like we should be celebrating Christmas instead of Easter. But as always, the weather always has its own plans, and runs on its own schedule. One of my favorite sayings is “the mountain does what it wants.” This week has certainly been no exception!
So, until the skies clear and the summit begins to thaw, we’ll rely on our chocolates to boost our mood in lieu of the sunlight we crave.
Mike Carmon, Interim Director of Summit Operations
17:36 Sun Apr 05, 2015
We’ve seen a large variety of weather this week, with signs of spring on the horizon across the high peaks of New England but plenty of wintry weather as well. The summit broke above freezing for the first time in over 80 days, with our first liquid precipitation of the year the overnight of the 2nd into the 3rd. Winter came rushing back in not long after this, however, with the summit picking up nearly 8 inches (or roughly 4 marshmallow peeps) of snow yesterday along with temperatures bottoming out around 0 along with hurricane force winds.
Looking ahead, winter still doesn’t plan on giving up its grip just yet across the higher elevations. A series of mostly weak low pressure systems look to bring frequent snow showers to the higher summits through most of the week. It seems likely that over several days the summit may see in excess of 6 inches of snow, only adding to the snow pack in place. Still, eventually the longer days and stronger April sun will begin to win out, and before long the snow will melt in time for many summer visitors to begin enjoying the views from atop the Rockpile. Until then, I’m personally looking forward to the small steps towards summer, like the first day I’ll be able go outside without a heavy jacket and gloves!
Tom Padham, Weather Observer/Meteorologist
19:58 Sat Apr 04, 2015
A Great End To Winter Trip Season!
Last night at the Observatory our shift hosted our final climbing trip of the season. Throughout the winter it has been a pleasure welcoming climbing trips and educational overnight trips into our home on the summit. These folks always arrive at the Observatory with enthusiasm to get an extended peek at life on top, and usually a bit of gratefulness to have a refuge from the wild weather outside. Eight days on top of a mountain in winter can feel like a lot longer, and it is nice to have these guests to break up the week and to share our excitement with. It is a rewarding experience to take guests up into the tower and have the fog break at just the right moment for them to catch a glimpse of what lies beyond.
The climbing trip yesterday arrived a little later than normal, as they took their time enjoying the nice soft snow and views in the warm spring sunshine. They were sure to make an early start of it this morning however. When I went out to retrieve the precipitation can at 7:30 there was a fresh and fluffy couple inches blanketing everything underfoot, and snow was falling vertically making for the most tranquil morning I’ve experienced here. It wasn’t long though before we were right back in full-blown and full-blowing winter conditions, with winds gusting to almost 100 mph by lunchtime and snow blasting our windows. While we now have a stretch of quieter shifts before the Cog and Auto Road open to mark the beginning of the summer season, I’m sure the weather will keep things plenty interesting.
Adam Freierman, Summit Intern
19:39 Fri Apr 03, 2015
The Streak Has Ended
Yesterday at around 7:30 PM the summit’s temperature reached a reading greater than 32°F for the first time in 87 days. That 87 day stretch of below-freezing temperatures is tied for the 5th longest, for days with temperatures below freezing since 1935. This was the first time in 37 years that the summit saw more than 80 consecutive days with temperatures not exceeding the freezing point! For many reasons, this has been an impressive winter across New England. While it was fun seeing how long this streak was going to last, now that it is over, it’s nice to see warmer temperatures making their way back into the forecast. Although this weekend’s forecast might be calling for another late-season storm in the higher elevations of the White Mountains, the long range forecast is showing the return of above-average temperatures for the end of the next work week.
Michael Kyle, Weather Observer/IT Specialist
16:59 Thu Apr 02, 2015
Summer, Then Back to Winter
With the spring season in full swing, those infamous April showers are to be expected, and the next few days will be no exception to that. However, glimpses of winter will continue to nose their way into the forecast from time to time.
A strong warm front will approach the region tonight, ushering in some of the mildest air the region has experienced since the turn of the new year! High temperatures soaring into the upper 50s are likely as far north as the Berlin/Gorham area on Friday, with readings well into the 60s throughout southern New Hampshire. Along with these warmer temperatures, rain will overspread the area, lasting through the early part of Friday, with even the summit of Mt. Washington experiencing plain rain for a time!
In fact, the above-freezing temperatures we're expecting overnight tonight on the summit will be the first since early January!
Mike Carmon, Interim Director of Summit Operations
However, this summer preview will not last long, as an area of low pressure off the coast rapidly deepens and pushes a strong cold front through New England. This will bring an abrupt end to those relatively-balmy temperatures, prompting precipitation to change back to snow on the summit as the mercury tumbles back into the sub-zero realm. If the low sets up just right, a significant amount of snow could be seen on the higher summits by late Saturday.
Even though summer keeps assuring us that it's on the way, winter just won't let go!