October/24 Report
DEFORESTATION MONITORING TECHNICAL REPORT
Last updated
DEFORESTATION MONITORING TECHNICAL REPORT
Last updated
The study area comprises the farm "Fazenda Floresta AmazΓ΄nica" located in the municipality of ApuΓ- AM (Figure 1). According to the vegetation classification by IBGE (2021), the farm area is situated within two types of vegetation: Open Ombrophilous Forest (OOF) and Dense Ombrophilous Forest (DOF).
This technical report uses NDVI vegetation cover monitoring to monitor possiblechanges in vegetation within the area called "Amazon Forest Farm", as well as detect possible degraded and deforested areas. Furthermore, based on images of deforestation alerts from the INPE and Imazon database, deforestation alerts were monitored in the period from October 1st to 31th, 2024, both in the farm area and in its surroundings.
In remote sensing, monitoring changes in vegetation cover at regionaland global scales, the normalized difference vegetation index (NDVI) is commonly used (Shi et al., 2021, Wu et al., 2020). NDVI is an important indicatorthat reflects the state of vegetation, which is affected by precipitation, anthropogenic activities, temperature and soil water content.
To prepare the Normalized Difference Vegetation Index (NDVI) map for the period established between 10/01/24 to 10/15/24 and 10/16/24 to 10/31/24, Sentinel L2A satellite images were used. On 10/08, satisfactory conditions were verified for preparing the NDVI map, with a cloud cover of 0%. Additionally, the image from October 8th was used, showing a cloud cover of 10%.
Following the standard procedure, NDVI was obtained by applying an algorithm based on the difference in near-infrared (NIR) and red reflectance divided by their sum of spectral bands (1), where NIR represents near-infrared electromagnetic spectrum and R the red electromagnetic spectrum, ranging between -1 and 1 (ROUSE et al., 1974), as follows:
Sentinel-L2A
10/08/24
2024
B8-B4
Sentinel-L2A
10/18/24
2024
B8-B4
Table 1. Specifications of the satellite image used for NDVI calculation
Additionally, a Soil Adjusted Vegetation Index (SAVI) map was developed to assess and confirm that thereis no deforestation occurring within the study area. The Soil Adjusted Vegetation Index (SAVI) is a variation of the Normalized Difference Vegetation Index (NDVI) that takes into account the influence of soil on the spectral response of plants. It is used to estimate vegetation density and vigor by correcting soil effects present in satellite images.
The same images from NDVI captured on August 09th were used. The formula for SAVI is as follows:
Where: NIR is the reflectance value in the near-infrared band; RED is the reflectance value in the red band; and L is the soil adjustment factor, which ranges from -1 to 1 (typically set to 0.5).
The inclusion of the soil adjustment factor (L) in the formula allows compensating the influence of soil reflectance, especially in areas with sparse vegetation or exposed soil. The value of L is typically set to 0.5, but it can vary depending on the characteristics of the vegetation and soil in the study area.
To provide a more comprehensive understanding of the indexes used in the study area, a Normalized Burn Ratio (NBR) map was also created in QGIS. This index is widely used to detect areas affected by fires (Key and Benson, 1999), deforestation, or damaged vegetation. It utilizes the near- infrared (NIR) and mid-infrared (MIR) bands from satellite images to map the extent and severity of burns. Landsat 8 satelliteimages, specifically bands 5 and 7 dated from October 06th, 2024, were used (available at https://earthexplorer.usgs.gov/).
Where: NIR is the reflectance value in the near-infrared band, and MIR is the reflectance value in the midinfrared band.
The Normalized Burn Ratio (NBR) varies on a scale of values depending on the methodology and scale used. However, a common convention is for NBR to range from -1 to 1. Negative values of NBR (-1 to 0) typically indicate areas affected by recent fires, deforestation, or damaged vegetation. Values closer to -1 indicate higher severity of the burn or vegetation damage. Positive values of NBR (0 to 1) are often associated with areas of healthy vegetation. Values closer to 1 indicate greater vegetation vigor.
To assess deforestation expansion around the farm "Fazenda Floresta AmazΓ΄nica" area, a radius of 50 km was determined. Databases from deforestation alerts provided by INPE and Imazon were utilized. The data obtained for October were in shapefile format, and all processing and filtering of alert points within the radius were conducted using QGIS software.
The Imazon Deforestation Alert System (SAD) currently employs NASA's Landsat 7 and 8 satellites, as well as ESA's Sentinel 1A, 1B, 2A, and 2B satellites. SAD detects forest degradation or deforestation events that occur in areas larger than 1 hectare.
INPE utilizes imagery from the WFI sensor on the CBERS-4 satellite and the AWiFS sensor on the Indian Remote Sensing Satellite (IRS), which have spatial resolutions of 64 and 56 meters, respectively.
The data is sent daily to the Brazilian Institute of Environment and Renewable Natural Resources (IBAMA) without a minimum mapped area restriction. However, for the general public, polygons are made available with a minimum size of 6.25 hectares, allowing for comparison with data generated by the PRODES project.
The identification of forest cover change patterns is conducted through visual interpretation based on five main elements (color, tone, texture, shape, and context), using the Spectral Mixture Analysis (SMA) technique along with multispectral imagery in color composition to map the following classes:
Deforestation with exposed soil and deforestation with vegetation and mining;
Degradation, forest fire scar;
Selective Logging Type 1 (Disordered)
Selective Logging Type 2 (Geometric).
Analysis of the spatio-temporal distribution of the Normalized Difference Vegetation Index (NDVI), obtained from Sentinel- L2A images dated from October 8th, revealed a wide variety of values, covering the range from -0.60 to 0.91. These data offer a significant interpretation of vegetation cover in the study region. Lower NDVI values, between -0.60 and 0.0, generally correspond to bodies of water, such as rivers, and small areas devoid of vegetation along the banks of these bodies of water. This distinction occurs due to the presence of water, which reduces NDVI values, as well as the opening of the forest canopy in these regions. On the other hand, values between 0.4 and 0.91 are related to areas of dense and healthy forests. This higher range of NDVI indicates robust vegetation, reflecting the density and health of the forest canopy in these specific areas.
When examining the NDVI images dated October 18 (as illustrated in Figure 3), a continuity in the NDVI values similar to the ones recorded on October 8 was observed, ranging from -0.99 to 0.93. The consistency of these patterns over time strengthens the understanding of the stability and vitality of the vegetation cover in the region under analysis.
When examining the Soil Adjustment Vegetation Index (SAVI), a variation in values between -0.11 and 0.74 was identified. These results reinforce the conclusion that there is no evidence of deforestation or significant human activities in the study area. Values in the range of -0.11 to 0.3 can be associated with water bodies, such as rivers, and exposed areas on river banks. On the other hand, values greater than 0.35 indicate areas covered by dense forests and in a good state of preservation.
Analysis of the Normalized Burning Index (NBR) carried out on October 6 revealed considerable variations in the mapped values, which ranged from -0.02 to 0.54. Negative values close to zero were identified, which indicates a possible relationship with the low volume of the rivers, resulting in the exposure of sandbanks and rocks on the banks.
Furthermore, the absence of negative values in the NBR indicates that there were no significant biomass losses due to fires, which is a positive sign for the conservation of local biodiversity. Positive index values suggest relatively healthy vegetation and soil that has not suffered degradation from fires. The analysis of this data is fundamental for planning environmental management strategies, allowing the implementation of preventive measures against forest fires and the promotion of sustainable land use practices
October, 22 deforestation alerts were identified within a 50 km radius of the farm. As illustrated in Figure 6, these alerts are concentrated near the city of ApuΓ, in previously deforested areas, which facilitate the illegal transportation of extracted timber. There was also a significant increase in deforestation alerts throughout the month. In addition, the Amazon region faced one of the most severe droughts in recent years, recording the highest number of fires since 2014
Table 1 shows the UTM coordinates of each deforestation alert point, the satellite responsible for identifying the deforested polygon and the size of the deforested area at each point. This information makes it easier to locate alerts for future inspections.
Analysis of NDVI values throughout the month of October suggests stability in the region's vegetation cover, with no significant signs of deforestation or forest clearing. SAVI reinforced this stability, the absence of deforestation or relevant human activities, while NBR did not detect recent signs of fires in the monitored areas, confirming that the forest ecosystems maintained their integrity during this period.
However, the identification of 22 deforestation alert points within a 50 km radius of the farm during October highlights the need for constant surveillance and preventive actions to prevent the advancement of these activities.
These alerts reinforce the importance of effective monitoring and control over the exploitation of resources, which is essential to mitigate environmental management. The information obtained is essential to support conservation policies, promote sustainable land use management and implement protection measures, ensuring the preservation of natural ecosystems.
Cunha, A.P.M., Alvala, R.C., Nobre, C.A., Carvalho, M.A., 2015. Monitoring vegetative drought dynamics in the Brazilian semiarid region. Agric. For. Meteorol. 214, 494β505. https://doi.org/10.1016/j.agrformet.2015.09.010.
Chu, H.S., Venevsky, S., Wu, C., Wang, M.H., 2019. NDVIbased vegetation dynamics and its response to climate changes at Amur-Heilongjiang River Basin from 1982 to 2015. Sci. Total Environ. 650, 2051β2062. https://doi.org/10.1016/j.scitotenv.2018.09.115.
Valle JΓΊnior, R.F., Siqueira, H.E., Valera, C.A., Oliveira, C.F., Fernandes, L.F.S., Moura, J. P., Pacheco, F.A.L., 2019. Diagnosis of degraded pastures using an improved NDVI-based remote sensing approach: an application to the environmental protection area of uberaba river basin (minas gerais, Brazil). Remote Sensing Applications: Society and Environment 14, 2033. https://doi.org/10.1016/j.rsase.2019.02.001.
Xu, H.J., Wang, X.P., Yang, T.B., 2017. Trend shifts in satellitederived vegetation growth in Central Eurasia, 1982β2013. Sci. Total Environ. 579, 1658β1674. https://doi.org/10.1016/j.scitotenv.2016.11.182.
Botucatu (SP), October 4th, 2024.
(11) 94004-0092 alessandro@zabottoambiental.com.br www.zabottoambiental.com.br
The formula for NBR is as follows: