The SiSeRHMap (simulator for mapped seismic response using a hybrid model) is a computerized methodology capable of elaborating prediction
maps of seismic response in terms of acceleration spectra. It was realized
on the basis of a hybrid model which combines different approaches and
models in a new and non-conventional way. These approaches and models are
organized in a code architecture composed of five interdependent modules. A
GIS (geographic information system) cubic model (GCM), which is a layered
computational structure based on the concept of lithodynamic units and
zones, aims at reproducing a parameterized layered subsoil model. A
meta-modelling process confers a hybrid nature to the methodology. In this
process, the one-dimensional (1-D) linear equivalent analysis produces
acceleration response spectra for a specified number of site profiles using
one or more input motions. The shear wave velocity–thickness profiles,
defined as trainers, are randomly selected in each zone. Subsequently, a
numerical adaptive simulation model (Emul-spectra) is optimized on the above
trainer acceleration response spectra by means of a dedicated evolutionary algorithm (EA) and the Levenberg–Marquardt algorithm (LMA) as the final
optimizer. In the final step, the GCM maps executor module produces a serial
map set of a stratigraphic seismic response at different periods,
grid solving the calibrated Emul-spectra model. In addition, the spectra
topographic amplification is also computed by means of a 3-D validated
numerical prediction model. This model is built to match the results of the
numerical simulations related to isolate reliefs using GIS morphometric
data. In this way, different sets of seismic response maps are developed on
which maps of design acceleration response spectra are also defined by
means of an enveloping technique
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