@InProceedings{MartinsNoguSetzMore:2019:ApCoDi,
author = "Martins, Guilherme and Nogueira, Joana and Setzer, Alberto
Waingort and Morelli, Fabiano",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)}",
title = "Fire Patterns in the Brazilian Cerrado: an Approach Comparing
Different Input Datasets in the Fire Risk Modelling",
booktitle = "Anais...",
year = "2019",
organization = "International Wildland Fire Ecology and Fire Management Congress,
7.",
keywords = "Fire modelling, fire season, savannas, Brazil, land use.",
abstract = "Emissions from vegetation fires are relevant in the
atmosphere-biosphere interaction. Nevertheless, fire is still
intensely used as a tool in land management, modifying natural
fire patterns in fire-prone ecosystems. The Brazilian Cerrado has
shown increased anthropogenic fire ignitions, especially due to
deforestation that removed ~50% of its original cover and unusual
droughts. Fire risk (FR) models using meteorological and
vegetation parameters have been used to estimate fire patterns at
biome level. Theaim of this study was to evaluate the performance
of INPEs FR model using different climate and land cover (LC)
datasets (versions 0 and 1) to estimate FR patterns in the
Cerrado. Meteorological datasets from CoSch and MCD12Q1-IGBP V006
land cover data represent v0 while v1 is composed by IMERG and
Mapbiomas v3.0 datasets. The analyses were performed in the wet
(W: November-March) and dry (D: May-September) seasons from 2015
to 2018 at 1km of spatial resolution. The versions were compared
using the seasonal predominance of FR (PFR) and evaluated in five
categories: minimum, FR<=0.15; low, 0.15<FR<=0.40; medium,
0.40<FR<=0.70; high, 0.70<FR<=0.95 and critical, 0.95<FR<=1.0. The
main fire pattern differences between v0 and v1 were observed in
D, when the PFR remains high during all season according to v0,
while v1classifies critical PFR from July to September. In W,
differences were not observed, except for November, classified as
low PFR by v0 and minimum PFR in v1. These differences can
berelated to the higher LC spatial resolution and definition of
vegetation types in v1 such as woody savannas; v1 is based on
Landsat medium resolution spectral images (~30m) while v0 uses
MODIS low resolution (~500m). Concerning precipitation, the
information has a higher spatial consistency using 10 km of
spatial resolution in v1 while v0 uses 25 km of spatial
resolution. With new Mapbiomas editions and revisions released
every year, INPEs FR will be updated accordingly, allowing a
realistic temporal modeling of the vegetation; including terrain
data in this condition will allow a new FR product at 30m
resolution for protected areas our next goal.",
conference-location = "Bras{\'{\i}}lia, DF",
conference-year = "2019",
doi = "10.37002/biodiversidadebrasileira.v10i1.1563",
url = "http://dx.doi.org/10.37002/biodiversidadebrasileira.v10i1.1563",
language = "en",
targetfile = "1563-Texto do Artigo-6511-1-10-20200401.pdf",
urlaccessdate = "03 maio 2024"
}