Abstract

Flood modeling is one of the layers that compose the preliminary susceptibility map, which after the field investigation step is part of the Mass and Flood Movement Susceptibility Map. These maps are produced by the Geological Survey of Brazil, through the National Plan for Risk Management and Response to Natural Disasters (Programa Nacional de Gestao de Riscos e Respostas a Desastres Naturais, PNGRRDN). Initially, the flood modeling methodology consisted of applying the HAND model based on the following variables, hydrographic basin, and soil susceptibility. However, several inconsistencies were observed during fieldwork, especially regarding the model capacity to describe regions with specific hydrological regimes. A methodological improvement using other variables became necessary. Among the proposed variables, the relief susceptibility to floods yielded the most satisfactory results, especially since it could be applied to the entire national territory and was, therefore, introduced to replace the hydrographic basin susceptibility. Furthermore, the methodology used for defining the thresholds of the three flooding susceptibility classes (high, average and low) has also been modified by using the quartile deviation, which provides a less subjective class distribution. Using relief susceptibility and quartile deviation in flood modeling was tested in the Conceicao do Castelo and Presidente Kennedy municipalities (Espirito Santo, Brazil), where the morphological configuration covers a wide variety of environments, which is fundamental for the validation of the new variable. The results of the new model were satisfactory. The various types of plains continue to be well represented while a substantial improvement has been observed in the representation of flood-susceptible areas such as marine terraces and colluvium ramps.

Highlights

  • Floods are hydrological processes that cause damages and disruptions every year, especially when occurring in urban centers that have been occupied or expanded in a disorganized way toward the seasonally flooded river plains (Goerl and Kobiyama 2013; Stevaux and Latrubesse 2017)

  • Using relief susceptibility and quartile deviation in flood modeling was tested in the Conceição do Castelo and Presidente Kennedy municipalities (Espírito Santo, Brazil), where the morphological configuration covers a wide variety of environments, which is fundamental for the validation of the new variable

  • This study aims at presenting the results of tests using relief patterns to replace morphometry of the sub-basins and applying the quartile deviation for determining the Height Above Nearest Drainage (HAND) susceptibility thresholds, in order to redefine some methodological criteria related to the terrain morphological characteristics and their respective susceptibility to flooding

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Summary

Introduction

Floods are hydrological processes that cause damages and disruptions every year, especially when occurring in urban centers that have been occupied or expanded in a disorganized way toward the seasonally flooded river plains (Goerl and Kobiyama 2013; Stevaux and Latrubesse 2017). The aforementioned issues and the objective of minimizing the damage caused by natural disasters led to the formation of the National Policy for Civil Protection and Defense (Politíca Nacional de Proteção e Defesa Civil) according to Federal Law No 12.608/2012 (Brasil 2012), which provides for the identification and evaluation of areas susceptible to geological and hydrological processes. To this end, the Plano Nacional de Gestão de Riscos e Resposta a Desastres Naturais (Brasil 2013) instructed the Geological. The variables, initially, flood susceptibilities of both the local sub-basins (defined by the morphometric parameters) and the terrain itself, were calculated by the heights relative to the local base level defined by the thalwegs of the channel networks using the Height Above Nearest Drainage (HAND) model, according to Rennó et al (2008) and Nobre et al (2016)

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