Lee,
don't forget to bundle up |
Robert
Leverett |
Jan
17, 2005 11:43 PST |
Lee:
Congratulations (???) on Embarrass Minnesota's 54 below zero
reading.
Only 11 below.
Bob
Robert T. Leverett
Cofounder, Eastern Native Tree Society
|
Re:
Lee, don't forget to bundle up |
Lee
Frelich |
Jan
17, 2005 13:57 PST |
Bob:
Temperatures in the range of -40 to -45 have been occurring
since late
December in northern MN. This morning two stations up there had
50 below or
colder and there were many reports of -45 to -50. During 1996 it
was -60,
so these temperatures don't really threaten the record low.
The red maples that have been invading the southern margin of
the boreal
forest during the mild winters of the last few decades will have
to think
twice about it now. Their deep supercooling strategy to keep
cells alive
only works to -45 or so.
They built Minneapolis were they did for a reason: we are in the
banana
belt. Big cities don't function well when its -50, so they put
Minneapolis
in southern MN. It hasn't been any colder than -15 to -20 in the
Minneapolis area in the last two weeks, and it has warmed up
very nicely
each day to 1 or 2 degrees.
Lee
|
RE:
SOOOPA! winter temps |
Lee
E. Frelich |
Jan
26, 2005 06:40 PST |
Ed C, Dale et al.:
The actual reason people move to northern MN is so they can pull
up a lawn
chair and sit outside all night to watch for the exact moment
that a tree
trunk splits open when it is -50 to -60. You have to pick the
right type
of tree--black spruce never splits due to cold.
This only half joking--some people from northern MN used to live
in the
condo above me, and they used to sit out on their balcony until
midnight,
even when it was -20. A few years ago they moved back to
Bemidji--there
just wasn't enough cold weather in Minneapolis to make them
happy.
During January 1996, the Weather Service predicted it would
reach -60 at
Embarrass and Tower MN, and reporters from every TV, Newspaper
and radio
station in the state went there--and sat outside all night in
lawn chairs
watching the thermometer. It hit -60 in Tower, but Embarrass
didn't make
it, so the party was in Tower. They threw a bucket of boiling
water in the
air and watched it turn to steam and fall to the ground as
little crystals.
I watched the festivities on TV in my +65 degree living room.
The following spring, red oak 'trees' on my nearby Hegman Lake
study site
had lots of dead spots on the bark, and got even more twisted
than they
already were. One is at least 170 years old, is 6 feet tall, and
its trunk
is a mass of scars from frost cracks. Nearby red pine, white
pine, balsam
fir, paper birch and black spruce didn't seem to have any
problems. The
170 year old white pines reach heights of 95 feet even though
they are
growing on a slab of granite.
Lee
|
RE:
SOOOPA! winter temps |
edward
coyle |
Jan
26, 2005 07:08 PST |
Lee,
I looked up Bemidji, as i had no idea where that was, and read
they have
temps of -50 with 50 mph winds. I have to think that eyes would
freeze shut
in those conditions.
Just a little inhospitable for me. Though I would like to see
those
protected valleys you spoke of, I'll wait for summer, or fall.
Ed C
|
RE:
SOOOPA! winter temps |
Ernie
Ostuno |
Jan
26, 2005 07:58 PST |
Lee,
You may be interested to read a paper titled "Recent State
Minimum
Temperature Records in the Midwest" from the Bulletin of
the American
Meteorological Society: Vol. 78, No. 1, pp. 35–40. It goes
into some
detail of the 1996 record low:
http://www.google.com/search?hl=en&q=%22recent+state+minimum+temperature
+records+in+the+midwest%22+schmidlin&btnG=Google+Search
(click on the "view as html" link in the third listing
from the top)
excerpts from section 3.e:
In anticipation of record cold, the media and other interested
persons
congregated on 1 February at the home of R. Fowler, the official
observer in Embarrass. Two persons familiar with the events, G.
Spoden
of the Minnesota State Climatologist Office, and meteorologist
B.
Watson, reported the minimum thermometer in the shelter had been
broken
for some time at Embarrass but an electronic thermometer had
been used
in its place. As the temperature descended overnight at
Embarrass, the
electronic thermometer failed, some said due to all the
television
cameras and lights plugged into Mr. Fowler’s home, and the
temperature
record was lost. The media then traveled the short distance to
the home
of K. Hoppa, observer at Tower 3S. Mrs. Hoppa observed a
temperature of
−59.5°F (−50.8°C) at 0910 LST, which was rounded
to
−60°F (−51.1°C) (U.S. temperatures are recorded in
whole
Fahrenheit degrees). A thermometer in the shelter used for media
display
purposes by Mrs. Hoppa was then taken from the shelter by a
reporter and
placed in the nearby swamp where it reportedly read −74°F
(−58.9°C).With the failure of electricity at the
Embarrass
station, tourists visiting there overnight to experience the
cold placed
two liquid-in-glass thermometers in the shelter and recorded
lows of
−60°F (−51.1°C) and −61°F(−51.7°C).
The reported
−74°F in the swamp near Tower 3S cannot be compared to
official
shelter temperatures since thermometers exposed to the sky will
cool far
below the shelter air temperature on a clear calm night.
...
Mrs. Hoppa reported that −60°F was a more penetrating
cold than
−40°F, people wore more clothes, cars started poorly,
some fuel
congealed, there was hardly any traffic, and the governor
canceled
school throughout Minnesota. Schools were closed for 2 days at
Tower.
...
As media stunts, one person camped in her lawn overnight,
another
pounded a nail into wood with a banana left outside in the
−60°F
cold, soap bubbles were blown to be seen freezing in mid-air,
and water
was tossed into the air to crackle and freeze before falling to
the
ground. Birds were reported active around feeders at Tower 3S as
the
sun rose, in spite of the temperature.
Ernie
|
RE:
SOOOPA! winter temps |
Lee
E. Frelich |
Jan
26, 2005 13:09 PST |
Ernie:
Thanks for the article.
I wonder if the -74 is real? If swamps really do get that much
colder than
weather stations, that could easily explain the absence of
certain tree
species in parts of northern MN. Even if it wasn't -74, but it
regularly
gets down to -60 in swamps when its -45 or -50 at the weather
station, that
would exclude several species of trees that I thought should
otherwise be
able to grow in swamps around Tower, such as red maple, silver
maple,
yellow birch, basswood, and bur oak.
Lee
|
Re:
SOOOPA! winter temps |
Michele
Wilson |
Jan
26, 2005 20:21 PST |
and I wonder about the lady who slept out on her lawn...did she
cheat, use
an electric blanket, a sooopa sleeping bag, crawl inside a cow,
or brave it
and die...
|
Re:
cold temps and warm trees |
Lee
E. Frelich |
Jan
27, 2005 06:39 PST |
Michele:
I think the woman survived, although the lawn is not the best
place to
spend the night. This type of weather is where certain trees are
really
handy. White cedar clumps, and black spruce clones (where the
branch tips
have bent down to the ground and rooted), have relatively little
snow under
them, which means that heat from the earth rises from the soil,
and it is
trapped by the dense foliage with snow sitting on top of the
crown. You can
see dense conifer clumps on infrared aerial photos taken at
night--they
show up as hot spots. You can crawl in one of those and sleep
all night in
a toasty -30 degree environment. You might even be joined by
chickadees
and other wildlife that know where these warm spots are.
A friend of mine was camping near Embarrass two weeks ago when
it was -54,
but on the second night he decided to leave the woods and go
into town when
his thermometer reached the bottom mark (-45 on his particular
model) by
7:00 pm. He didn't know how cold it was, he just knew it was
colder than
-45, and he had -40 rated equipment.
Lee
|
Re:
Neil's hypothesis |
Lee
E. Frelich |
Jan
27, 2005 08:04 PST |
Bob and Neil:
I think you are right about soil freezing impacts on trees. we
have a large
die off in oaks in central Minnesota in the last two years, and
we also had
periods of below zero weather with no snow in the last two
winters. Frost
depths reached 8 feet in some places, and 10 cm soil
temperatures reached
as low as 7 degrees.
Of course we also had a fall drought during 2003, and that
probably added
to the impact.
Lee
|
RE:
SOOOPA! winter temps |
Ernie
Ostuno |
Jan
27, 2005 07:24 PST |
Lee,
The -74 was real only in the sense that the thermometer itself
cooled a
lot lower than it would have if it were in a shelter. As the
article
stated:
"The reported −74°F in the swamp near Tower 3S
cannot be compared
to official shelter temperatures since thermometers exposed to
the sky
will cool far below the shelter air temperature on a clear calm
night."
Any glass or metallic surface will lose heat faster through
radiative
processes if it is in the open rather than inside the
standardized
wooden box used for official temperature recordings. Now having
said
that, it is likely that any area of lower topography such as a
swamp
could well be colder than surrounding sites, thanks to
"frost hollow"
effect. It would have been interesting to have put a sheltered
thermometer in that swamp to see how much colder it was than at
the
observation site.
Ernie
|
RE:
SOOOPA! winter temps |
Robert
Leverett |
Jan
27, 2005 08:03 PST |
Ernie:
I'm confused. Are we saying that the -74
degrees IS the actual air
temperature at the point where the thermometer is placed, but
that the
process of recording temperatures officially shelters
thermometers and
that leads to warmer temperatures? If so, what is the reason for
sheltering other than to get them out of the sun?
Bob
|
RE:
SOOOPA! winter temps |
Ernie
Ostuno |
Jan
27, 2005 12:50 PST |
Bob,
I guess you can think of it this way...if you leave a
thermometer out in
full sunlight, it will heat up above the temperature of a
thermometer in
a shelter. Similarly, if you leave a thermometer outside on a
clear
night, it will cool off below the temperature in a shelter. This
is
because the thermometer is made of materials (glass and metal),
which
have different radiative properties than wood. This allows those
surfaces to cool off faster than wood if they are not sheltered
and also
to heat up faster if they are exposed to sunlight. You probably
have
noticed that the windsheild and hood of your car will frost over
long
before frost forms on most other objects that are not made of
metal or
glass. The purpose of the shelter is to avoid these temperature
extremes
caused by the direct radiative heating and cooling of the
thermometer
itself.
Ernie
|
Re:
SOOOPA! winter temps |
John
Eichholz |
Jan
28, 2005 04:18 PST |
Ed, Bob:
As I understand it, the basic process of radiational cooling is
the
radiation of heat to deep space at night. The clear winter
nighttime
sky exposes objects to the deep darkness of space, which is very
cold.
The rate of transfer of heat is always proportional to the
temperature
difference and the insulation value of the air, thus the rapid
rate of
cooling experienced by the bulb on very clear nights. Deserts
also have
that large day/night difference, because the air is so dry (like
it is
in winter here). In some circumstances, the air just doesn't
hold
enough ready heat to reintroduce into the bulb of the
thermometer by
convection, so there occurs a temperature difference. When the
sky is
cloudy, radiation to (or from) deep space cannot occur as
readily, so
this effect is absent. Why doesn't the air also cool? Probably
because
air is a poor radiator compared to glass or metal, and cools,
but not as
fast.
The shelter contains many surfaces not exposed to this cooling
process,
and is perhaps made of wood ( a better insulator than glass) and
is
therefore more in equilibrium with the air temperature. Too,
radiational cooling is only one reason for a cold night, the
other being
the introduction of cold air from elsewhere via atmospheric
circulation. This air finds its way into the shelter easily
keeping it
cool.
Eventually, the object cools the air, or stops radiating so fast
and the
air warms the object, and equilibrium is reached. It is perhaps
a
philosophical point, but all objects are always at different
temperatures, since their temperature is always changing in
response to
the temperature of bodies around them. Even a bowl of soup will
always
have hotter parts and cooler parts. I think when this stops
we'll all
be dead -- complete entropy.
John
|
Re:
SOOOPA! winter temps |
John
Eichholz |
Jan
28, 2005 18:26 PST |
Bob:
I found a neat NOAA website where they go into the equipment
used at a
"cooperative weather station", including a picture of
a temperature
shelter. It is at: http://www.srh.noaa.gov/bro/coopsite.htm
John
|
RE:
SOOOPA! winter temps/question for Lee |
Ernie
Ostuno |
Jan
30, 2005 17:14 PST |
Ed,
In this case I think that the surrounding air is actually cooled
by
being in contact with the metal surface (or glass, or snow for
that
matter). Think about a surface that is losing heat to space. The
temperature will cool due to radiative heat loss and that
cooling can be
at a much greater rate than the rate the surrounding air is
cooling.
A case in point...clear, calm nights right after a fresh
snowfall are
often the coldest of the year. Why? Because snow does two
things. First,
it reduces the warming effect of terrestial longwave radiation
from the
ground and second and most importantly, it is very efficient at
radiating heat energy to space. The surface of the snow will
actually
cool the air quite a bit colder than it would get if the snow
wasn't
there. This effect is not as pronounced on windy nights (unless
colder
air is being advected in) because the wind mixes the air near
the ground
with warmer air from above (which hasn't been cooled by being in
contact
with the snow surface). Conversely, snow is a great insulator.
There can
be a tremendous temperature gradient from the surface of the
snow, where
temperatures can be far below zero, to just a few inches below
the
surface, where temperatures are usually not far below freezing.
It is
for this reason that I can tell how deep the snow cover was on
the side
of my house during the winter by the level that my rose bushes
sprout
back in the spring.
Lee,
As for radiative properties of different materials...you brought
up an
interesting point. It would appear that the more cold-adapted
tree
species such as spruce are less efficient at losing heat through
radiation from their surfaces as other trees are. Has anyone
looked at
the radiative "energy budgets" of different tree
species? For instance,
I wonder if a tree with smooth bark such as beech would lose
heat
quicker than a rougher barked oak or hickory. I suppose an
infrared
sensor could be used to "see" which trees are warmer
than others on a
cold winter night...
Ernie
|
winter
temps/question for Lee |
Lee
E. Frelich |
Jan
31, 2005 06:08 PST |
Ernie:
I have not heard of anyone looking at radiative properties of
different
tree surfaces for cold tolerances.
We have studied insulating properties of bark, and pines have
the best
insulating capacity because their bark is thickest, and it is a
slightly
better insulator than bark of other species at the same
thickness.
However, I think this is probably more applicable to fire
survival.
Basically, 2.9 times the square of bark thickness in cm predicts
the number
of minutes that a tree trunk can be exposed to a 500 degree C
flame before
the cambium underneath will be killed, which in turn requires
exposure of
living cells to temperatures of 60 degrees C for about 1 minute.
For example, of two white pine trees are exposed to flames for 5
minutes
during a surface fire, and one tree has 1 cm thick bark and the
other 2 cm
thick bark, then tree #1 will be girdled by the fire and killed
(it can
only tolerate about 3 minutes of flame exposure), whereas tree
#2 will
survive with little damage, since it can tolerate 2x2x2.9
minutes or about
12 minutes of exposure.
Bark thickness is greatest at the base of a tree where it is
exposed to
fire, and it is very thin on the twigs, yet we don't see pines
and spruces
along the northern edge of their range with dead twigs each
spring after an
episode of -60 temperatures, which is why I conclude that bark
insulation
is more important for fire survival than for surviving winter
cold. We do
see dieback of red maple and red oak after an extreme winter
cold spell,
but that is known to be due to their deep supercooling mechanism
that can
only possibly work down to about -47 F. Still, it would be nice
to know
whether tree surfaces (especially conifer needles) cool down to
temperatures above, at, or below the air temperature on calm
nights, and
whether these effects vary among species and help explain the
presence or
absence of certain tree species which have very patchy
distributions in
northern MN.
Lee
|
RE:
winter temps/question for Lee |
Robert
Leverett |
Jan
31, 2005 07:09 PST |
Lee:
This is absolutely fascinating stuff. I image
that you all paint of
the constant heat exchange that is going on between surfaces
that are
out in the open makes it seem very strange to me that I ever put
so much
stock in the "official" temperatures reported from
regional airports.
Bob
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