@Article{PrudenteMaViSiAdSa:2020:LiClCo,
author = "Prudente, Victor Hugo Rohden and Martins, Vitor Souza and Vieira,
Denis Corte and Silva, Nildson Rodrigues de Fran{\c{c}}a and
Adami, Marcos and Sanches, Ieda Del'Arco",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Iowa State
University} and {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 = "Limitations of cloud cover for optical remote sensing of
agricultural areas across South America",
journal = "Remote Sensing Applications: Society and Environment",
year = "2020",
volume = "20",
pages = "e100414",
month = "Nov.",
keywords = "Crop monitoring, Optical data, Cloud frequency, MAIAC.",
abstract = "Earth Observation data support the large-scale monitoring of
croplands across South America (SA). For instance, optical remote
sensing (ORS) data are typically used to map and monitor plant
development during a crop season. However, the monitoring of
agricultural areas is highly affected by cloud cover frequency
(CCF), especially in the rainy season, and the implications of
cloud cover for ORS of agricultural areas are still poorly
understood in SA. In this study we evaluated the monthly CCF and
variability focused on implications for agricultural monitoring in
SA. Cloud cover was derived from daily MCD19A2 Collection 6
Moderate Resolution Imaging Spectroradiometer (MODIS) product
between 2000 and 2015. A monthly average was computed using daily
observations for the studied period. To evaluate the effects of
clouds in agricultural areas, we used a cropland mask from the
Worldwide Croplands project and divided the CCF into quarters. The
results show that cloud cover affects the monitoring of croplands
depending on geographic location and crop season. In the P1 period
(September to November) 68% of South American croplands have CCF
between 40% and 60%. In the P2 period (December and February), SA
croplands have CCF concentrated in the classes of 40%50% and
70%80%. In the P3 period (March to May) 42% of SA croplands have
CCF concentration in class 5 (40-50% of cloud cover). In the P4
period (June to August), we observed values from 30% to 60% of
cloud cover in 41% of South American croplands. These patterns
make summer crop monitoring via ORS data difficult, mainly soybean
and maize. In this sense, for the Brazilian states of Mato Grosso,
Goias, Bahia, Tocantins, and Parana, the use of ORS is limited in
providing an accurate summer crop monitoring. While cloud cover is
an intrinsic challenge for agricultural monitoring of some crops,
the combination of multi-sensors (e.g. microwave and optical
sensors) and CubeSats can improve the earth observation frequency
and help to work around this limitation, thus enabling a better
time series analysis.",
doi = "10.1016/j.rsase.2020.100414",
url = "http://dx.doi.org/10.1016/j.rsase.2020.100414",
issn = "2352-9385",
language = "en",
targetfile = "prudente_limitations.pdf",
urlaccessdate = "13 maio 2024"
}