San
Fernando, LA UNION (August 16, 2003)—Pangasinan of
late has been battered by two strong typhoons, Chedeng on May 27
and Harurot on July 22. As in the past, floods would have been the
normal episode to towns along the course of the Agno River.
But things looked different this time around. According
to mayors of municipalities traversed by this river, unlike in the
past, the Agno River was very calm and quiet at the height of these
typhoons. Keen observers point to that one big difference—the
San Roque Multipurpose Dam (SRMP) in Barangay San Roque, San Miguel,
Pangasinan.
The flood control capability of SRMP was first proven
during typhoon Chedeng, when at the height of the typhoon on May
27, 2003 PAGASA recorded a six-hour rainfall of 358.0 mm and a 24-hour
rainfall of 722 mm.
According to the Mines and Geosciences Bureau Region
1, which deployed its Special Task Action Group (STAG) to monitor
the situation that time, despite the heavy and prolonged precipitation
that took place for about thirteen (13) days due to typhoon Chedeng
there was no reported flooding adjacent to the Agno River.
On the contrary, the STAG report revealed, the cities
of Dagupan and Urdaneta, and towns of Mangaldan, Mapandan, Sta.
Barbara and Calasiao—areas that are not along the course of
the Agno River but are traversed by Sinocalan, Pantal and Cayanga
rivers—have suffered from 4 to 6 feet deep floods after several
rivers have swollen due to the record-high precipitation.
“This only indicates that the SRMP has tangibly
helped in flood-control in areas traversing the Agno River,”
MGB Region 1 Director Samuel T. Paragas said.
The SRMP, a rock-filled clay-cored embankment dam,
stands at 200 meters above the existing river channel and contains
nearly 40 million cubic meters of fill materials including river
aggregates and clay materials. The dam is 1,300 meters long at its
crest elevation of 295 meters above sea level (masl). This imposing
manmade mining-spawned structure has two principal functions, power
generation and irrigation. However, there are two less recognized
but equally critical roles of the dam, flood control and water quality.
According to San Roque Power Corp. report, the SRMP
produces a marked attenuation or reduction in the perennial flooding
of the Agno River affecting at least 16 Pangasinan and Tarlac towns.
For floods up to a 50-year event, or such floods so large as to
recur only once in 50 years, peak outflows from the dam are at least
one-third (1/3) less than peak inflows to the reservoir.
The report explains that the reservoir does not
contain floods, but rather attenuates them; that is, it reduces
the outflows released downstream by storing a portion of the inflows
received from upstream. In fact, the SRMP attenuates all floods
up to the 200-year event—a flood so great as to recur only
once every 200 years. The flood attenuation gradually reduces from
about 1/3 for the 50-year flood to zero for the 200-year event.
The projected flow pattern before and after the dam is completed
is illustrated below.
During typhoons, the reservoir level is allowed
to rise above the normal maximum operating elevation of 280 masl
and may reach the maximum exceptional elevation of 290 masl, consistent
with SRMP design criteria.
During extreme events; namely, floods beyond the
200-year event, all inflows received from the upstream Cordillera
watershed must be released downstream. Then, flood conditions will
be same as those prevailing had the SRMP not been constructed.
In
other words, the spillway is operated so that the peak outflow during
a flood event does not exceed the peak that would have occurred
without the dam and the rate of rise of the water in the downstream
channel does not exceed the natural rate without the dam. (By
Roel A. Collado, Supervising Science Research Specialist, MGB-REGION
1)
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