Windthrow |
Lee
E. Frelich |
Jun
24, 2003 17:03 PDT |
ENTS:
Its been an exciting day in MN. A severe thunderstorm went
through last
night at 4:00 AM. The cottonwoods got their crown thinning that
they
needed. The street I walk down to get to campus was closed due
to a
hackberry tree (about 7' cbh) having been deposited across the
street.
All afternoon, severe weather warnings have been flying nonstop.
Some
places have had 10 inches of rain. There are four tornado
warnings are in
effect right now, including one only nine miles away from me.
Too bad I
can't see it--its raining too hard.
It has been interesting to see how each species of tree
responds. Hackberry
split at their first main fork. Bur oaks and elms give up small
branches
about an inch in diameter at the end of major limbs. Sugar maple
fold up in
the wind so they only have a small surface area, and they either
split, or
the tree uproots. Cottonwoods have branches about 10 feet long
stripped
from the tree.
A tree is essentially an a circulation system that is designed
to maximize
surface area exposed to the atmosphere, so they can
photosynthesize. But
they have to pay a price when the wind is extreme.
I had better turn off the computer now--tornado and heavy
lightning are
approaching and computer-killing power surges are likely!
Lee
|
Windthrow |
Lee
E. Frelich |
Jun
25, 2003 11:11 PDT |
ENTS:
Things are getting back to normal (except those whose houses we
levelled by
tornadoes, crushed by trees, or washed away by floods--I was
lucky I just
have mud from a minor flood in the garage) after last nights
storms.
Minneapolis had four separate warnings: tornado warnings at 6:30
and again
at 9:30, a severe thunderstorm warning at 12:00 am and a flash
flood
warning that lasted all night an extended into morning.
At 6:00 pm last night, a weather balloon released in Minneapolis
showed
winds of over 100 mph blowing straight up from the ground. With
a dewpoint
of 77 degrees, and a strong jet stream directly overhead, these
vertical
winds made for an exceptionally unstable atmosphere. What goes
up must come
down, and all the moisture those updrafts fed into the towering
thunderheads came back down in the form of a dozen tornadoes,
golf ball
sized hail, 4-10 inches of rain, and several downbursts. Once
again,
streets were closed this morning by debris (mostly trees) and
many freeways
were closed by floodwaters. The small town of Buffalo Lake just
west of
Minneapolis had the worst with a 1/2 mile wide F2-F3 tornado and
10 inches
of rain.
Four isolated super cell thunderstorms that each produced
tornadoes west of
Minneapolis converged at about midnight to form one almost
stationary
Massachusetts-sized thunderstorm that produced downbursts,
tropical storm
intensity downpours and about 50 strokes of lightning per minute
throughout
the night over Minneapolis.
We should see a lot of browning on the edge of leaves now, just
from the
physical abrasion of the wind and heavy rain. We will also get
light brown
flecks on leaves from ozone, which is created by lightning as it
heats up
the air and converts O2 to O3. This thunderstorm created a major
ozone event.
Lee
|
Windthrow |
Lee
E. Frelich |
Jun
25, 2003 11:22 PDT |
Gary:
To answer your question about tree geometry, I think it is
pretty well
fixed genetically. What throws the genetic pattern off is injury
by
drought, wind, lightning, etc. Of course, old trees accumulate
injuries
that change their growth form, so they develop a lot of
character.
There are several different growth patterns that trees can be
classified
into that relate to the frequency of buds along a stem, what
angle the new
shoots grow from the stem when the buds open, and whether the
buds are
organized in whorls, alternate or opposite, and the degree to
which apical
dominance limits the growth of side branches. In the tropics
there are
about 20 different growth forms, which are shown in the book by
Halle,
Oldeman and Tomlinson, which as I recall was published about 20
years ago.
A few simple parameters like bud placement, branching angle, and
apical
dominance can be combined in many ways to make unique and
recognizable
growth patterns for thousands of tree species around the world.
With respect to wind out analysis of MN blowdowns shows that
tree species
with narrow crowns on top of a tall trunk (forest grown aspen,
black spruce
and balsam fir) are the most susceptible. Trees that retain low
branches
(white cedar) and broad crowned species (maples and oaks) are
less
susceptible to blow down.
Lee
|
Windthrow |
Leverett,
Robert |
Jun
25, 2003 12:04 PDT |
Lee:
I read an article a number of years ago in Scientific American
that discussed the geometry of tuliptree leaves in heavy winds.
As I recall the species does a remarkable thing by curling its
leaves into cylinders that allow wind to blow past and through,
thus minimizing wind resistance. I wish I had saved the article.
It made quite an impression.
The storm system you described sounded scary if not downright
terrifying. I have been in a few of those mid-western storm
systems that produced lightening flashes saturating the
atmosphere. They are awesome and serve to remind us that natural
events still rule. Given the frequency and intensity of storms
in Minneapolis, how do they affect the awareness and feelings of
ordinary citizens toward nature/natural events relative to say
Philadelphia, Atlanta, or Los Angeles?
Bob
|
Windthrow |
Lee
E. Frelich |
Jun
25, 2003 12:45 PDT |
Bob:
A lot of trees streamline their leaves during high winds (i.e.
the blade is
parallel to the wind, presenting a tiny surface area). I have
not heard of
trees rolling up their leaves, but then there is so much to know
about
trees that I have barely started to acquire knowledge.
Regarding people's attitude towards natural events, you may have
noticed
that no one was killed, and people are seldom killed here even
though we
have violent weather. That's because people here are very aware
of weather
safety, which is taught in the schools, and are always ready.
Buildings and
infrastructure are engineered to handle extreme events, so we
have
relatively little damage, and people just sit back and enjoy the
storms.
People in Minnesota are pretty strongly connected to nature and
like to see
all the variety it produces, or they wouldn't live here.
People from the two coasts (and especially LA) don't think of
weather as
something that could kill them at any moment. My neighborhood
always has
lots of visitors from more benign climates, and it is fun to
watch them
look around and wonder why they are suddenly the only ones left
in the
middle of the park when the sky turns black, or deep luminous
green like it
was last night, or the tornado siren sounds. After a few minutes
(but just
before the tornado arrives) one of us will go out and tell any
panicking CA
residents what to do (i.e. stop gathering under large open grown
trees and
go in a building).
Lee
|
Windthrow |
Paul
Jost |
Jun
25, 2003 13:10 PDT |
Lee, Bob,
I'm just hypothesizing here, but I'll give it a try:
A "flat" leaf is never really flat which is probably a
really bad thing
when wind is concerned. Any slight curvature in the leaf while
exposed
to wind in a direction parallel to the approximate plane of the
leaf
(wind blowing at the edge of the leaf showing the smallest
possible
surface area to the wind) will cause it to act like a wing due
to the
pressure differences caused by moving air traveling different
path
lengths along the top and bottom surfaces of the leaf. Ooooh...
nasty
run-on sentence. Anyway, a slightly curved or nearly flat leaf
will
always flip around in the wind while a leaf that curls into a
tube will
align itself with the wind. The nearly flat leaf the flops
around and
periodically exposes it's surface to the full speed of the wind
will
likely get twisted or torn off while a leaf that forms a tube
might
survive by being more aerodynamically stable and properly
oriented with
minimal surface area to the wind at all times.
I'm just guessing about this but it seems to make sense to me...
Paul Jost
|
Re:
Snowfalls capture the record hunter's imagination |
Lee
E. Frelich |
Jun
11, 2004 10:30 PDT |
Bob:
Our thunderstorms can produce derechos (clusters of several
downbursts)
with gusts of 150 mph and sustained winds of 120 mph. They can
cover an
area 10-15 miles wide and 150-200 miles in length. They reach
the size and
intensity of a category 3 or 4 hurricane, and cause comparable
damage,
although the spatial pattern of damage is different. It is
probably several
hundred years between such events at any one spot on the ground.
A more typical severe thunderstorm that most places experience
once a
decade has winds 70-80 mph.
Lee
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