Friday, March 25, 2016

icy morning...

wet afternoon! i slipped off the steps going out to scrape the ice off vehicles...ouch. somehow i managed to not do too much damage and got the truck and car scraped but went back in to warn pam and get ashes to spread on the granite. while i was in i thought i better check to see if there was a delayed opening at the schools--the ice was pretty thick. nothing listed. when i got to the high school i found people shaking their heads a bit but doing school things.

ms doody and i got the ap chem lab ready and i grabbed some supplies to use with the third graders. on the way from the high school to the grade school i passed through a couple of silvery tunnels. tree limbs were covered with a heavy coat of ice. in one of the third grades we did an exciting demo on air pressure, crushing aluminum cans by heating and rapidly cooling the air inside them. amid the bubble of excitement watching such instant, dramatic change, there were all sorts of observations offered as to why and i left everybody thinking. on the way back home, the ice was starting to melt and fall like hail. i thought, wow, what a good time to go up and catch the action on cardigan.






i packed a quick bag and headed out. no cars were in the winter parking lot, but as i started up the gated road, i noticed boot tracks in the half inch of very wet snow--two sets going up and two coming down. i wished i had been up here earlier--maybe even as the wintery mix (this is the second time i have linked this site--it is that good!) was falling. rounding the first corner and heading up the second steep section the ice in the trees grew thicker, cool, things had not started falling yet. i was pumped with the possibility of what i would see up higher and even imagined the sun coming out and sparkling things up! what i was to find was much less dramatic, and definitely more mysterious. like the third graders this morning i was left wondering what was going on...and why?






basically, what i was seeing was a ton of the ice load--all on the ground now--but only in certain sections. where i saw the majority of ice was on the steeper sections of trail. on the flatter areas, there was nearly no fallen ice. crazily, this transition could be within yards of each other. the following four pictures are within a hundred yard section, alternating between flatter and steeper, and again flatter and steeper. weird stuff.



was there some kind of air current factor? did elevation play any part? did the increasing pools of melt indicate that there was ice but now it was gone? i had plenty of time to think about it as i hiked--the problem was as i got higher and higher, the changes kept adding new questions. it seemed like it was getting warmer and the evidence of ice was definitely disappearing. i was enjoying trying to figure out what was going on and before i knew it i was up on the slabs.

once at tree line, the only ice left was tucked deep into the thick, dark sections of the dense scrubby spruce off the trail. as those 'forested' bits gave way to nearly all rock, the wind swirled the cloud covering the mtn., lifting and dropping it, like shaking out a blanket atop a bed.  up at the top, the sun seemed to be right behind that cloud, at times so bright i wondered why i left my darkglasses at home. i stopped at the trail marker right below the summit, braced myself against a steady wind--my guess was 20mph with gusts to 30--and took a series of pictures, counting to twenty between each one. the clouds whipped around me and the tower came into and out of view.



i suppose it doesn't look like much changes in the pictures, but i was fascinated by what i could see and what i couldn't. hannah, sawyer, colin roebuck, and i have talked about 'series photos'--over both space and time--for a while now. when i started today's hike i revisited the notion of pictures going up the mountain and then coming back down spread out over a year. these four, out of eight total, or about three minutes worth of trying to hold things steady, connected me back to that idea. as my hands got colder and colder, i finally tucked the camera away and went up and stood out of the wind on the lee side of the actually solid tower.

when i headed down i could feel it getting colder. that was a bit odd as most of the snow and ice i had seen going up, had melted. i started to think that the ice that was more present at lower elevations was due to the inversion that brought the freezing rain in the first place. cold sinks and pools which helped me make some sense of the conditions i was seeing today. like my last post noted, it is always interesting, weather-wise, to live in new england.

Wednesday, March 23, 2016

"if you don't like the weather in new england now...

just wait a few minutes." so spoke mark twain, or samuel clemens if you prefer, and as true now as it was back then. i have been riding to the grade school this week and last. while i am pretty bundled up to get there by 9:00, i have been coming home at 3:00-ish with no hat or gloves. a couple of trips last week, even my jacket was too warm and once the legs got working hard, it was practically shorts weather.



jacket, hat, and gloves were welcome up on the top of cardigan for the moonrise-sunset hike yesterday. the temperature was low twenties and the wind was fairly stiff between 10 and 20mph. i noticed that every one of the windmills over toward plymouth were spinning. that seems rare. moc goes up every month give or take one day around the full moon. most of the winter i am the only one who shows, but tonight five students, one mother, two boisterous and energetic black labs, and sawyer--an alum--made the trek.






my ski buddy skip and his best friend (and wife) linda were coming down as we went up. we passed just above lunch rock. they had watched the moon rise and were heading down before the sun actually set, considering the huge cloud bank to the west, that would not take too long. we continued on and took some pictures, measured the wind speed, and hung out a bit before following.

it struck soy and i that cardigan mountain is about as wonderful a mtn to have in your back yard as could be. the top few hundred feet are above tree line--a fire scorched the top back in 1855--allowing for a 360 view to write home about. at least that is the case when it is not in the clouds and snowing or raining. while it can look and feel like the sub-alpine zone up in the whites, it has very few of the typical species in a krummholz. true or not, you get a big bang for you buck when you summit. having spent a good amount of time on summits both in the whites and on cardigan, conditions can be remarkably similar. while i have never measured winds higher than 50-60mph up top cardigan, speeds that high on a 'little mtn.' can play big.

speaking of playing big, or maybe i should say wet, the two labs had a heck of a hike, hitting every puddle--iced or melted--and stream within a hundred yards of the trail. sliding and splashing around like otters, they entertained each other as well as us--both up and down.