What is revealed when 1913 high-water measurements are input into today’s Geographic Information System (GIS) computational tools? By guest author Barry Puskas of the Miami Conservancy District
Beginning Easter Sunday 1913, 9 to 11 inches of rain fell within three days, March 23–25, throughout the Great Miami River watershed. The massive deluge surged through downtown Dayton and a host of other cities and towns,
Dramatic digitized
map of 1913 flood depths in Dayton, Ohio, was one of nine geo-referenced maps
created by Barry Puskas and colleagues at the Miami Conservation District
(MCD) between 2008 and 2012, synthesizing data from 1915 hand-drawn maps with modern
GIS techniques. For this poster, which also paired photographs of submerged
locations in Dayton with similar views of the same locations today, Puskas was
received the Map Gallery People’s Choice Award from the Ohio GIS Conference
(OGISC) of 2013. High-res digital maps of the 1913 flood in Dayton and eight other cities are available from the MCD (more info below)
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drowning or otherwise
killing more than 360 people throughout the Miami Valley—60 percent of Ohio’s
death toll in just 10 percent of its area. In addition, property damage throughout
just that southwestern corner of Ohio exceeded $100 million in 1913 dollars, equivalent
to between $2.5 billion and $44 billion in today’s economy (see the discussion
at the end of this post on converting the value of historical dollar figures, as
well as details about fatalities in “’Death Rode Ruthless…’” and about property damage in “Like a War Zone”).
In response to the flood, the some 23,000 citizens of the
Miami Valley raised local donations of $2.2 million (in 1913 dollars) by the
end of May for a permanent flood protection system (see “Morgan’s Cowboys”). The Miami Conservancy District
(MCD) was formed as a regional agency for the entire watershed; construction was
finished in 1922 and the system completely paid for 1949 (see “Morgan’s Pyramids”). The MCD has been providing flood
protection since.
The MCD system consists of five major dry dams (slide 14)
that hold back floodwaters in excess of what can be handled by 55 miles of
levees and 35 miles of improved channel downriver. The system protects not only
Dayton but
also select areas in the cities of Franklin, Hamilton, Huber
Heights, Miamisburg, Middletown, Moraine, Piqua, Tipp City, Troy, and West
Carrollton.
The system
was designed to protect the valley from not just another 1913-scale flood but
also an additional 40% more runoff. The 1913 flood exceeded a 500-year flood
(that is, one with only 0.2 percent chance of occurring any year), and some
statistics I’ve seen indicate it even exceeded a 1000-year flood (one with less
than 0.1 percent chance of occurring any year). So the MCD system protects the
valley against a 1000-year flood plus potentially 40% more. That’s a heck of a
lot of flood protection. But after
suffering through the 1913 flood, the citizens of the Miami Valley did not and
do not want to experience such a catastrophe ever again.
Need
for maps
To design, engineer,
and construct the effective dams, levees, and improved channels, MCD engineers
needed several sets of data including: 1) detailed topographic information of
the cities and rural regions swept by the flood; 2) the actual peak heights and
extent of the floodwaters for calculating the volume and forces exerted; and 3)
some realistic sense of the probability of a future flood of the same or
greater magnitude for calculating an adequate safety margin.
But in 1913, only
1:62,500 scale U.S. Geological Survey topographic maps existed of the Miami
Valley. Those USGS maps were of only limited use, however, as the usual USGS elevation
contour interval was 20 feet, far too coarse mapping of elevations for the
MCD’s flood-protection needs.
So, to gather the additional
data, MCD chief engineer Arthur E. Morgan famously sent teams of surveyors
armed with buckets of white paint fanning out throughout the Miami Valley,
interviewing residents about flood heights and times, marking flood heights on
buildings and trees with white paint all the way from Piqua (pronounced PICK-wah) to Hamilton.
Then, using
traditional surveying tools and techniques, they meticulously measured horizontal
lines of sight and (vertical) elevations. They determined elevations to 1-foot contour intervals on
flat ground for the whole river corridor where it flooded, and 2-foot intervals
on steeper slopes up to 50 to 75 feet elevation above the flood zone.
By 1915,
they completed about 100 hand-drawn, black-and-white paper maps of the valley’s
topography and high-water marks plus property boundaries and other essential
features. The contour maps
included topographical information, 1913 flood limits, and observed high water
marks. In some areas, they even mapped river bottom elevations that would have
been below the water’s surface. The maps were so careful and precise that they
were used by the MCD for nearly a century for estimating flood depths.
Bringing the maps into the digital age
Beginning in 2008, the
MCD wanted to digitize the maps so that they could be geo-referenced to a
modern geographic coordinate system where the data could be manipulated using computerized
Geographic Information System (GIS) methods. By 2012—in time for the centennial
of the Great Easter 1913 Flood—the MCD produced dramatic new maps of the 1913
flood.
The new digital maps
are scientifically important, because much topography today has been altered
from what it was in 1913 as a result of major changes—including construction of
the MCD flood protection works themselves. The new maps would allow us to overlay
the current MCD levees and channel improvements. Making the maps digitally
accessible also would allow us to understand some of the dynamics of the 1913
flood in greater detail as described by observers or survivors.
The new digital maps
are also historically and culturally important. Mapping the 1913 flood over
today’s geography brings home to current residents the phenomenal extent and
power of the natural disaster against modern landmarks. Thus, the maps may be
freely used by historical societies and other groups throughout the Miami
Valley. A few communities—notably
Dayton, and Franklin, Hamilton, and Troy—have
chosen to use the maps to guide them in prominently marking the peak flood
heights of the 1913 flood along downtown streets to encourage walking tours of
local history. To that end, the MCD also produced utility-grade stickers that
can be affixed to light poles and other smooth surfaces to mark 1913 high
water.
Converting
from then to now
In a nutshell, the
MCD generated the new digital maps from the century-old paper maps. As just one
example, I’ve zoomed
into one area in Piqua: a peninsula jutting into the Great Miami River that we
dubbed the Piqua nose, which shows the hand-drawn streets as they existed in
1913.
First, we
took the black-and-white maps and raster-scanned them to
convert them into digital form. Then we digitally stitched them together to
give us one gigantic map of the entire Miami Valley, through all five counties
along the Miami River corridor. To tie them to modern geographic reference
systems—specifically to the Ohio State Plane coordinates—we needed features that have not
changed since 1913. Streets are sometimes dug up and moved, buildings razed,
canals filled in or otherwise destroyed, bridges replaced, etc. But in general,
railroad tracks don’t shift much. So the railroad tracks were essential in
allowing us to carefully tie the century-old maps to today’s widely used
coordinate system.
We also
wanted to separate out the topographic contour intervals along with their
associated elevation information. We did that through what is known as a
raster-to-vector conversion, which simply means converting a hand drawn line
from an image to a digital (or computerized) line object.
That allowed
us to create a digital elevation model (DEM) of the region’s topography in
1913, extracting three-dimensional information from the two-dimensional maps.
That’s important because water runs downhill—river hydraulics is all about
topography and gravity—and features obstructing floodwater flow that can change
or alter flow patterns and flood depths.
On that 1913
digital elevation model, we were then able to plot all the high water marks
that Morgan’s surveyors had painted and measured—shown as red dots. They plotted
and recorded some 1,900 high water marks along the river corridor.
Then, from
those high-water marks, I made some flood water surface lines, that is, making
lines that would represent the maximum or peak surface of the 1913 floodwater
from one side of the river valley to the other.
Now here
comes the power of digital manipulation. The digital 1913 flood water surface was
interpolated to map the edge of the flood boundary.In addition, the data were used to
calculate flood depth for every 10 foot by 10 foot area on the ground. The
detailed depth mapping was a new look of the flood that depicted much more
detail than the 1915 maps. The newly created flood boundary from GIS matched very well to the 100-year-old paper maps; even the dry areas, or as I call them "islands," complemented the original maps.
From this
stage, we can now display today’s aerial imagery view of Piqua’s city streets
to create a flood depth map for the city and whole region. Once again picking
on Piqua, this view reveals how the 1913 floodwaters—which were up to 20 feet
deep in this region—would have inundated the streets of Piqua as they exist
today. This, of course, is what happened before the MCD flood protection system
was built.
Equally
dramatically, now that everything is georeferenced, we can digitally
superimpose other layers from current aerial photography or any other digital information.
For example, we can overlay the MCD’s current flood protection measures: the
long orange line around the Piqua nose marks the MCD levees, and the little
green squares mark some floodgates on storm sewer outlets so water can’t get
back underneath the levees and inundate the city.
Finally, we
can map the area of Piqua—or elsewhere along the Great Miami or other
rivers—now protected by the MCD system today.
Sidebar: Gallery of digitized maps
Below are
thumbnail images of the digitized maps of the 1913 flood depths in eight cities
along the Great Miami River corridor, in addition to the map of Dayton shown as
the lead (top) photo in this article. High-resolution versions of the maps are
available from the Miami Conservancy District, especially for those communities
that wish to create exhibits or otherwise commemorate the 1913 flood as part of
their local history. For more information about the digitized maps and
high-water stickers, contact the author Barry Puskas c/o t.e.bell@ieee.org.
Digital map of 1913 flood in Franklin, Ohio. Credit: Miami Conservancy District |
Digital map of 1913 flood in Hamilton, Ohio. Credit: Miami Conservancy District |
Digital map of 1913 flood in Miamisburg, Ohio. Credit: Miami Conservancy District |
Digital map of 1913 flood in Middletown, Ohio. Credit: Miami Conservancy District |
Digital map of 1913 flood in Moraine and West Carrollton, Ohio. Credit: Miami Conservancy District |
Digital map of 1913 flood in Piqua, Ohio. Credit: Miami Conservancy District |
Digital map of 1913 flood in Troy, Ohio. Credit: Miami Conservancy District |
Digital map of 1913 flood north of Troy, Ohio. Credit: Miami Conservancy District |
Barry Puskas, P.E.,
G.I.S.P.—shown here with the Map Gallery People’s Choice Award he received at OGISC 2013—has been manager of technical services for
the Miami Conservation District in Dayton, Ohio, since 2007. Before that, he
was a hydrologist for the U.S. Geological Survey. Mr. Puskas has professional
experience in civil engineering projects such as land development design,
hydraulic and hydrologic studies, and dam/levee safety engineering. A graduate of
The Ohio State University, he is a registered professional engineer (PE) and
geographic information system professional (GISP). His technical expertise is
in hydrologic and hydraulic modeling; FEMA flood studies; geographic
information systems; flood forecast modeling; flood protection system
operations; and engineering design and analysis of dam safety and levee safety
projects. Mr. Puskas also has experience in management of information
technology (IT) including servers, virtual servers, network systems, work
stations, laptops, and mobile devices. He may be reached c/o t.e.bell@ieee.org.
©2016 Barry
Puskas
Next time: Racing Against Epidemic
Selected references
The text and most of the illustrations in this guest post are
based on half the conference presentation by Barry Puskas supplemented with
information gathered during a telephone interview with him on June 24, 2016.
Listening to his full 45-minute presentation online
while watching his full slide presentation is highly recommended for his additional
discussion comparing photographs taken during the 1913 flood in half a dozen
cities with photos of the same locations today.
There are at least seven separate methods for assessing the present
value of historical money (all seven are discussed at the excellent site
MeasuringWorth.com by two economics professors at the University of Illinois).
They are all correct in different contexts, yet they all yield answers that
differ widely. Since natural disaster losses pertain to damage to and
rebuilding major projects such as bridges and railways, the most relevant
method for this purpose seems to be the “relative share of the GDP,” which
allows comparison of the cost of construction of a major project in historical
times to the value in the economy at the time as a percentage of the GDP. To
compare capital losses in 1913 dollars with 2014 dollars (the latest given on
Measuring Worth.com), the “relative share of the GDP” calculator multiplies
1913 dollars by a factor of 439 to reach today’s value. So $100 million in 1913 would translate to about $44 billion today.
For more information, see Officer, Lawrence H. and Samuel H.
Williamson, “Measuring Worth is a Complicated Question”; for the actual calculator, see “Seven Ways to Compute the Relative Value of a
U.S. Dollar Amount, 1774 to Present.”
See also their discussion “Choosing the Best Indicator to Measure Relative
Worth,” using the cost of constructing the Empire State Building as an example.
Miami Conservancy District, The. A Flood of Memories. One Hundred Years After the Flood: Images from
1913 and Today. The Miami Conservancy District. 2013. ISBN
978-0-615-75860-2. 128 pages. Hardbound. Colorful coffee-table book depicts the
dramatic 1913 flood side-by-side with images of the same areas today captured
by photographer Andy Snow. Dayton, Franklin, Hamilton, Miamisburg, Middletown, Piqua,
Troy, and West Carrollton are all included. Each pair of images has brief
descriptive text, but the bulk of every page is reserved for the striking
contrasts between devastation in 1913 and the safety and vibrancy these
communities enjoy now.
Some two dozen more books plus several
documentary films have been published about the 1913
flood in various cities in the Miami Valley, including many for the 2013
centennial commemoration. For detailed listings and descriptions of them, see
“Book Report!”, “Centennial Highlights—and Legacy”, “Centennial Year + 2”, and “1913 Flood + 3”.
Bell, Trudy E., The Great Dayton Flood of 1913, Arcadia Publishing, 2008. Picture
book of nearly 200 images of the flood in Dayton, rescue efforts, recovery, and
the construction of the Miami Conservancy District dry dams for flood control,
including several pictures of Cox. (Author’s shameless marketing plug: Copies
are available directly from me for the cover price of $21.99 plus shipping,
complete with inscription of your choice; for details, e-mail me.)
Thank you for the fantastic article.
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ReplyDeleteJourney back in time with us to an event etched in history, an unprecedented disaster that reshaped landscapes and communities—the Great Easter 1913 Flood. Through this blog, we pay homage to this monumental calamity, delving into its impact, stories of resilience, and its lasting legacy.
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