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Ruidoso's
Flood History Analysis
By
Frank Potter
Floods:
Recurrence intervals and
100-year floods
When
flood conditions occur, you
might hear reports on the
radio or TV say something
like, “This storm has
resulted in a 100-year flood
on the Rio Ruidoso, which
crested at a stage of 12
feet.” This means that the
river reached a peak stage
height that happens only
once every 100 years, right?
Well, not exactly.
Hydrologist don't
like to hear a term like
“100-year flood”
because, scientifically, it
is a misrepresentation of
terminology that leads to a
misconception of what a 100
year flood really is.
Instead
of the term “100-year
flood”, a hydrologist
would rather describe this
extreme hydrologic event as
a flood having a 100-year
recurrence interval.
According to historical
rainfall and stream stage
data, the probability of the
Rio Ruidoso reaching a stage
of 12 feet is once in 100
years.
In other words, a
flood of that magnitude has
a 1 percent chance of
happening in any year.
What
is a recurrence interval?
Statistical
techniques, through a
process called frequency
analysis, are used to
estimate the probability of
the occurrence of a given
precipitation event. The
recurrence interval is based
on the probability that the
given event will be equaled
or exceeded in any given
year. For example, there is
a 1 in 50 chance that 6.60
inches in a consecutive 48
-hour period is said to have
a 100-year recurrence
interval. Likewise, using
frequency analysis,
there is a 1 in 100
chance that a stream flow of
1000 cubic feet per second
will occur during any year
at a certain stream
flow-measurement site.
Therefore, that site is said
to have a 100-year
recurrence interval.
Ten or
more years of data are
required to perform a
frequency analysis for the
determination of recurrence
intervals. Ruidoso has 67
years of historical data and
hydrologist have more
confidence in an analysis of
at least 30 years of
records. Based on the
historical data, the
following chart depicts the
recurrence interval, or what
percent of probability, of
future flooding of
the Rio Ruidoso.
Ruidoso's
data is typically taken at
the reservation line in the
upper canyon at the USGS
station and not the
Hollywood
USGS station due to
the fact that officials are
measuring
initial impact on the
village. When rainfall data
is collected at a point
within a stream basin, it is
highly unlikely that the
same amount of rainfall
occurred uniformly
throughout the entire basin.
During intensely localized
storms, rainfall amounts
throughout the basin can
differ greatly form the
rainfall amount measured at
the location of the rain
gage. Ruidoso experienced
this in almost all known
floods, especially the 1965
flood.
The
100-year flood level can
change.
Since
the 100-year flood level is
statistically computed using
past and current data, as
more data comes in, the
level of the 100-year flood
will change. (Especially if
a huge flood hits in the
current year.) As more data
is collected, or when the
river basin is altered in a
way that affects the flow of
water in the river,
scientist re-evaluate the
frequency of flooding
necessitating the redesign
of structures, such as
bridges, to meet the 1000
cubic feet per second flow.
Ruidoso's past history
indicates that bridges have
been designed to accommodate
300 to 500 cubic feet per second.
Based
on the 100-year flood
assumption, every year there
is a 1% chance of recurrence.
However, 100-year
floods can happen two years
in a row and can be analyzed
using the
frequency analysis
process for a given area.
Ruidoso Flood History
1500
1400
1300
1200
1100
1000
*
*
cubic
feet/sec
900
800
700
600
500
*
*
400
300
*
*
1941
1965
1978
1984
2006
2008
(2008-1941=
67 years)
2
floods in 67 years= 1000 cfs
6 floods in 67
years=300 cfs+
2.99%
8.95%
4
floods in 67 years=500 cfs+
5.97%
You
are welcome to use this
information, with
attribution to
RuidosoToday.com of course
If you have an event you
wish published on
RuidosoToday.com
e-mail
the information to theboss@ruidosotoday.com
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