@Article{SantosBorSilPieBez:2019:LaDuFi,
author = "Santos, Andr{\'e} Lu{\'{\i}}s Silva dos and Borges, H{\'e}lder
Pereira and Silva Junior, Celso Henrique Leite and Piedade Junior,
Raimundo Nonato and Bezerra, Denilson da Silva",
affiliation = "{Instituto Federal do Maranh{\~a}o (IFMA)} and {Instituto Federal
do Maranh{\~a}o (IFMA)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Universidade Ceuma (UNICEUMA)} and
{Universidade Ceuma (UNICEUMA)}",
title = "Modelling dunes from Len{\c{c}}{\'o}is Maranhenses National Park
(Brazil): largest dune field in South America",
journal = "Scientific Reports",
year = "2019",
volume = "9",
number = "7434",
abstract = "This paper presents a digital elevation model (DEM) of the dunes
found in the Len{\c{c}}{\'o}is Maranhenses National Park, an
environmental protection area located in the Maranh{\~a}o state
(Brazil). The DEM supports the modeling studies of sand-dune
evolution using multi-temporal satellite images and ground truth
data, obtained through the post-processed kinematic Global
Navigation Satellite System (GNSS) positioning. The study area is
located at the border of three major neotropical ecosystems: the
Amazonia, Caatinga, and Brazilian savanna. It is located in the
northeastern state of Maranh{\~a}o and encompasses the largest
dune felds in the country. Wide shrubby areas (restingas, in
Portuguese), lakes, mangroves, and a multitude of reshwater
lagoons compose the parks natural environments. The objective of
the present study is to create an DEM that can evidence the
complex dynamics of dune formation in the study area with use of
GNSS. Geodetic techniques and precision mapping were employed to
monitor the short-term coastal dynamics. The use of GNSS receivers
is justifed by the difculty of mapping the dunes features using
conventional methods such as theodolite, level, and total station
systems, due to their high cost, time restriction sand low data
precision. Surface surveys were carried out annually between
December 2015 and January 2017 to create a DEM. The study results
reveal that the area has a negative volumetric balance of erosion
and a preferential direction of sediment transport by wind, which
may justify the pattern of advancement and retraction observed in
the dunes of the studied area.",
doi = "10.1038/s41598-019-43735-0",
url = "http://dx.doi.org/10.1038/s41598-019-43735-0",
issn = "2045-2322",
label = "lattes: 0506851271452550 3 SantosBorSilPieSil:2019:LaDuFi",
language = "en",
targetfile = "s41598-019-43735-0.pdf",
urlaccessdate = "27 abr. 2024"
}