Town Indexes
At 11:25 AM 6/2/03
-0400, you wrote:
Jess, Colby, Will,
Dale, Lee, Tom, et al:
I would expect southern towns to commonly exceed their northern
counterparts with respect to the Rucker Index. I just don t have a feel
for how much. For Massachusetts the following tall tree relationships
currently exist.
Entity Rucker
Index %
of Mass Index Location
State
137.2 100
Max
site
133.95 98
MTSF
Max
township
117.5 86
Northampton
Typical Tall tree
site 110 80
Average mature site 92
67
The above table
shows the relationships between the state as a whole and the maximum
index for a town, max for a single site, a typical site with tall trees,
and a typical mature forest site. The last number is a little shaky. It
may be high. I m curious how a state like South Carolina compares. I
suspect that sites like Congaree and Station Cove will score above 95%
of the state maximum. The ratio of site index to the state index could
be used to identify sites worthy of special protection.
Bob
From: Lee
E. Frelich
Sent: Monday, June 02, 2003 4:38 PM
Subject: Re: Town Indexes
Bob:
I expect a latitudinal gradient in urban Rucker
index. I wouldn't be
surprised if it varied by 30-40 feet from South
to North.
We can probably break 90 feet for the Rucker
Index in the Minneapolis Metro
area, although that's higher than it would have
been 10 or 20 years ago. It
seems that trees are growing taller now than in
the past. Maybe that's an
early sign of global warming.
Lee
From: Robert Leverett
Sent: Monday, June 02, 2003 8:49 PM
Lee:
The
plan I've established for myself is to sample
spots along the
Massachusetts river systems, using the top down
approach in selecting
trees. I think I can cover the region from 41 to
43 degrees latitude
north and 71 to 74 degrees longitude west.
That's about as big of a slice
as I can hope to cover with any degree of
thoroughness. Hopefully Howard
Stoner can pick up and extend westward toward
Dale's territory, and Dale
to Tom's territory, which would give us a pretty
good picture of the
species from New England to Ohio. If you and
Paul pick up from there
(with a zigzag northward), we can take the
species quite a bit farther west.
Since
stream corridors are almost certain to give us
long swaths
of good cottonwood habitat, we never have to
worry about where to look. In addition, since the species isn't used for
lumber and does fit in with
wetland conservation, we have plenty of mature
trees to sample. I'm
simply amazed at what I've been overlooking.
Talk about having blinders
on. I could never fairly point the finger at
anyone else for tuning
something out.
Bob
From: Gary
A. Beluzo
Sent: Monday, June 02, 2003 10:24 PM
Subject: RE: Town Indexes
Bob and Lee:
Exciting! Are there other species you can think
of that would fit in the
same category as the cottonwoods (i.e. large
mature trees that have been
left because they have little commercial value
and their habitat is for
the most part protected)? I am thinking that
many of the riparian trees
might fit into that category and hence be good
measures of the Rucker
Index and portend the effects of global warming?
Gary
At 06:54 AM 6/3/03 -0400, you wrote
Gary:
Silver
maple fits the requirement. Maybe green ash and
sycamore to
a degree. I can't believe how blind I've been to
the riparian habitat. The large cottonwoods near the Connecticut River
that I measured on
Sunday are spectacular trees. If we encountered
maples or oaks of the
size of the cottonwoods in our mountain forests,
we would be hooting and
hollering for days. We've got lots of great
territory to cover, partner.
Bob
From: Lee E. Frelich
Sent: Tuesday, June 03, 2003 9:13 AM
Subject: Re:
Town Indexes
Bob and Gary:
We also have green ash and silver maple in riparian
habitats, as well as
bur oak, swamp white oak, black willow, and basswood.
The southern part of
MN and WI also have honey locust, Kentucky coffee tree,
and sycamore,
especially along the Mississippi, Wisconsin, and Rock
Rivers.
The upper Mississippi in MN, WI, IA and IL probably has
an area of riparian
habitat the size of one of those little states out east.
The bottomland is
several miles in width by 400 miles long and lined with
500 foot bluffs on
either side.
There are also interesting seepages in the coulees
(valleys that are
perpendicular to the river with small streams that empty
into it). The
coulees have forests of sugar maple, white oak, red oak,
walnut, black ash
and yellow birch in coves enclosed by steep rocky walls.
Great potential
for unusually tall trees there. They are a lot like Ice
Glen, and there are
dozens of them. The best of them are in state parks.
The final odd feature are algific slopes. They have
caves that fill with
ice from seepage during the winter, and they take all
summer to melt, so
the caves give off cold air, which percolates out
through talus slopes,
which support really bizarre features like a balsam fir
stand in Iowa a few
hundred feet from bur oak savanna, and 250 miles south
of the southern edge
of the main range of balsam fir.
Lee
At 10:48 AM 6/3/03 -0400, you wrote:
Lee:
Very interesting descriptions. I'm amazed at the habitat
diversity of the
upper Mid-west. So many jewels that hardly get noticed.
For our study purposes, how do you see the roles of the
different habitats
for the study of the maximum growth potential models
we've been
contemplating? Which habitats do you see as providing
the greatest returns
for us? My approach so far has been to look for the
absolute richest sites
and work downward from that, since the absolute species
maximums will
occur on the good sites. So far in Massachusetts, lower
elevation mountain
cove and ravine sites produce the tallest members of the
representative
species. The riverine habitats produce the largest trees
and fastest
growth rates. The larger the river system, the deeper
the soil deposits.
One puzzle to me at this point is exactly what
determines where the
cottonwoods dominate? More to the point, where do they
cease to dominate,
i.e. the interface zone? Of course flood plains and
river corridors are
where I find the species in abundance, but as I follow a
feeder stream
into the uplands, cottonwood abundance and individual
tree size drops
dramatically. Quicker than I can presently account for.
Why don't I see at
least a few whoppers on the upper Deerfield? The other
species there are
doing just fine, but so far I haven't found a single
really huge
cottonwood. Perhaps cottonwoods need much deeper soils.
What conditions
would support silver maple dominance over cottonwood and
vice versa? My
belief has been that every year is a good year for
cottonwood seed
production. Am I wrong?
Dang it, Lee, I've gone cottonwood crazy.
Bob
Bob:
Starting at the maximums and working down (which means working
up in
latitude and elevation) is a good strategy. It seems to be
easier to
characterize maximum tree height than the pattern of tree height
among
habitats.
Cottonwood only grows into a big tree (15' cbh) on deep soils,
and also it
is extremely intolerant of shade and cannot compete (especially
at the
seedling stage) with other species that are more shade-tolerant
once you
get far from the river. Cottonwood can function as an early
successional
species after a major disturbance (tornado, flood, fire,
clearcutting),
regardless of distance from the river. But it cannot grow in its
own shade,
and it only dominates for long time periods in areas where there
is
frequent flooding, since it can better survive the period of
root
saturation and lack of oxygen than other species, and it is even
a little
better at that than silver maple. The seedlings can grow to
heights of 10
or 20 feet in a year or two, thus getting above the flood levels
of all but
the greatest floods (we have 40 foot floods in the Midwest, but
only every
10 or 20 years, a typical spring flood is only 10-15 feet). Any
seedling
that is totally submerged for more than a few hours will die.
I suspect that the flooding history of a site determines the
difference
between dominance by silver maple and cottonwood, but don't
really know the
details. There are always plenty of seeds for both species, so
that doesn't
explain the differences.
Cottonwood, silver maple, swamp white oak, green ash and other
flood plain
tree species do well in big cities, especially commercial areas
with lots
of pavement, because their roots are adapted to floods and can
tolerate the
lack of oxygen underneath sidewalks. We use cottonwood in
Minneapolis,
where they grow to about 40 feet in height in 5 years, even when
planted in
concrete, but then they die from ground frost. Black ash is
another wetland
tree that has recently gained attention as an urban tree. They
can survive
in sidewalk planting pits, including lack of oxygen, tons of
salt which is
used in commercial areas to keep sidewalks from becoming skating
rinks
(which is fine with me but dangerous for old fogies), and
extreme ground
frost to depths of 7 feet, like we had this past winter.
Lee
At 02:00 PM 6/3/03 -0400, you wrote:
Lee:
There's always a reason. Thriving in paved-over areas
due to the species
adaptation to oxygen-deprived environments made
immediate sense - once you
said it. I'm now thinking of the cottonwood corridors I
regularly pass
that have developed adjacent to paved areas. Of course!
Do you see any
east to west developmental factors for the species such
as appears to be
the case for tuliptree?
Tulips seem to gain in stature going westward at the
same latitude and
elevation. Little River Gorge, just west of springfield
has old tuliptrees
as do a few spots in the southwestern part of Mass, but
they are puny
compared to Green Lakes and Zoar Valley. Going southward
into
Connecticut, tuliptrees quickly become abundant and
start to appear taller (gotta get down there more). At first I thought the
species was highly
sensitive to a slight drop in average temperature, but
Green Lake State
Park blows that theory, as does Zoar Valley.
Understanding the adaptations of species to their
environments is what
fascinates me most. Your statement about cottonwoods:
"since it can better
survive the period of root saturation and lack of oxygen
than other
species, and it is even a little better at that than
silver maple", was of
particular interest. Who is presently studying these
adaptive traits and
have there been any recent revelations of which you are
aware?
Bob
Bob:
There is a strong east-west gradient in drought and severe storm
frequency
(and variability in general, with more extremes towards the
west) in the
Midwest. This means that trees get taller as one goes east at
the same
latitude from the prairie-forest border to Lake Michigan,
although the
coves in southwestern WI may be an exception.
The major problem with comparing trees across a large region is
the
variability in soils. One should only compare tree heights
across lat and
lon gradients on similar soils. However, I doubt that we will
ever be able
to describe soil adequately enough to say how similar they are
over large
areas. We will have to settle for getting a lot of sites where
trees are
measured and dividing the whole cluster into high, medium and
low heights,
and assume that these represent very good, good and poor soils
for each
region, even if very good doesn't mean the same thing in MA and
GSMNP.
I know a few people who have studied floodplain forests,
including Paul
Harcombe at Rice University in Houston, Rebecca Sharitz at
Savanna River
Ecology lab, and Kurt Shulz at Southern IL University. Most of
what little
I know comes from seeing their presentations at meetings and
reading their
papers.
Lee
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