System Improves Monitoring of Waves on Brazilian Coast
Hello
reader!
It
follows an article published day (04/17) in the english website of the Agência
FAPESP reporting that a system improves the monitoring of waves on the
Brazilian Coast.
Duda Falcão
System
Improves Monitoring
of Waves on Brazilian Coast
By Luiz
Paulo Juttel
April
17, 2013
Operating on a supercomputer,
the Coastal Forecasting and
Monitoring System forecasts
the movement and height of
waves at 61 points on the
coast
|
Agência FAPESP – Monitoring and forecasting coastal processes
are activities that interest several sectors of society. Data on sea waves from
computer simulations allow scientists to identify the generation and arrival of
energetic events, such as cyclones, so that individuals engaged in sailing,
fishing and oil exploration activities can prepare.
Brazil has recently gained a mathematical modeling tool focused on this
type of analysis. The Coastal Forecasting and Monitoring System (SIMCos) was
developed by researchers at the National Institute for Space Research (INPE),
Universidade Federal do Rio de Janeiro (UFRJ), Universidade Federal do Espírito
Santo (Ufes) and Universidad Nacional Autónoma do México (Unam) to simulate
diverse characteristics of waves that reach the Brazilian coast.
The platform produces information about the significant wave height,
potential height, period and direction of waves that reach 61 distinct points
on the country’s coast. The simulated attributes are generated based on surface
wind data (10 meters above sea level).
“We calibrated the model based on the climatology of the waves in the
last 30 years, from 1979 to 2010. The surface winds were calculated based on a
mathematical scheme known as data assimilation. This mixes observations and
results of models with spatial and temporal resolutions of 0.3125˚ and 1 h,
respectively,” explained the coordinator of the project, Valdir Innocentini, of
INPE.
The SIMCos is part of FAPESP’s thematic project “SMCos: monitoring system and studies of
coastal processes.” The participants in the study, which began in 2007, include
geologists, oceanographers, meteorologists, physicists and mathematicians. The
team created to make the simulations generated by the system available to the
public in real time has launched a website, which is still in its testing stages.
The unique aspect of SIMCos is not the creation of the mathematical
model in itself because that modeling tool is already widely known in
oceanography. The project’s novelty is the implementation of this model in a
system that forecasts and monitors the movement and height of waves at several
points along the Brazilian coastline.
Another highlight is the simulation and the monitoring of the potential
height of waves at the 61 selected points. This calculation shows the flow of
energy, the product of the square of the height and the time between the
passage of two consecutive wave crests.
The INPE researchers explained that if waves that are low on the high
seas have a significant height potential, they often change into high waves
when they reach areas near the coast, causing movements of sediments and
producing erosion. This process creates a dangerous situation for beach-goers
and sailors.
The Brazilian system offers a simulation of the energy contained in the
waves that will hit a particular coast in the next five days, in intervals of
three hours. SIMCos also offers graphs that show the probability of waves
between 0.5 and 6 meters in height at each of the 61 points analyzed.
The regions that are part of the system were selected to cover the
entire Brazilian coastline. According to Innocentini, running the model daily
for the country’s entire coastline would be infeasible because of the high
computer processing demands.
On the high seas, those with depths of 100 meters or more, mathematical
models can predict the movement of waves continuously around the globe. “In
shallow waters, the velocity of waves diminishes, and the physics involved in
the process becomes more complex, which makes it difficult to create efficient
simulation processes and requires the use of high-performance computers to run
these models,” explained Innocentini.
SIMCos is currently run on the Robura supercomputer, which cost R$
200,000 and has more than 120 processors at INPE in São José dos Campos.
Next Steps
The data on surface winds that supply SIMCos were extracted from
atmospheric models because no equipment for conducting the required surface
wind measurements is located along the Brazilian coast.
According to Innocentini, the use of the atmospheric models in no way
invalidates the information generated by the system for two reasons. The first
reason is that these atmospheric models have a high level of precision. The
second reason is that Brazilian researchers have compared SIMCos results with
information on the height of waves from satellites, buoys and consolidated
mathematical models that analyze coastal processes in the North Atlantic Ocean,
obtaining similar data in both cases.
The next step in the study is to combine some of the data generated by
SIMCos with the hydrodynamic model (MOHID)
of coastal circulation developed by the Superior Technical Institute (IST) in
Portugal. This model simulates the ocean currents closest to the coastline, the
tides, sediment transport and erosion.
The combined use of these systems will allow for evaluation, for
example, of the impact of human activity on sediment transport in coastal
areas. Giant waves can drastically alter the coast in a region. Over time,
however, other currents can gradually reconstruct the affected area.
“If there is some human interference, like the construction of a port or
wharf, the flow of reconstructive currents could be interrupted and the
sediments of that region will not be recovered. Our model can point out these
cases,” explained Innocentini.
SIMCos, coupled with MOHID, could also be employed in the analysis of
the impact of climatic phenomena such as El Niño and in the analysis of the
effects of the alteration of the average sea level on waves and coastal regions
in Brazil.
Source: English
WebSite of the Agência FAPESP
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