Remote Sensing-Based Land Suitability Analysis for Forest Restoration in Madagascar
Abstract
:1. Introduction
2. Materials and Methods
2.1. The Study Area
2.2. The Suitability Analysis
- (1)
- identification of a set of restoration criteria
- (2)
- acquisition of available GIS datasets for each criterion
- (3)
- generating suitability maps for each criterion
- (4)
- conception of a suitability analysis model
- (5)
- design of potential sites for restoration.
2.2.1. Identification of Criteria for Land Suitability Analysis
- Land cover class- The land cover classes of interest include seven categories which are: dense forest (primary forest and mangroves), degraded forest (degraded continuous forest and forest fragments), grassland (nonwoody vegetation such as grasses, herbaceous plants), agriculture areas (mostly rice field, commercial crops, tannes. The term ‘tannes’ refers to the inner part of mangroves, coastal wetlands found in tropical and subtropical regions. They represent the least frequently submerged zones, with soils generally oversalted or acidified, developing at the expense of a mangrove. We distinguish between “naked tannes” and “herbaceous tannes” according to the vegetation cover in mangrove areas, agroforestry), and minor land cover classes such as waterbody (river, lake, stream), bare land, and limestone massif (classified as rock). Forests (dense and degraded) and grassland were given priority in our criteria to assess the Ecological factor (Figure 2a).
- Distance from protected sites and forest patches—Restoration in and around a protected site and forest patches means both enhancing the forested ecosystem and creating a buffer zone that prevents the site from being disturbed. In addition, areas around existing forests are a priority for their proximity to reservoirs of native species [28]. The location of protected sites and forest cover in the watershed region are shown in Figure 2b.
- Settlements—Settlements include human habitation and build infrastructures (hospitals, schools, churches and sports areas). High concentration of human activities in cities and villages are considered a driver for land degradation and natural resources exploitation in the nearby forest area. In a study of deforestation in the northeast part of the country [11], it was proposed that the range of influence of land users is at a maximum of about 2.5 km from the home village, which can be extrapolated to about 20 km2 neighborhood area from the village. A settlement map is produced using Landsat 8 OLI satellite images and verified with Google Earth map (Figure 2c).
- Risk of soil erosion—To achieve restoration objectives in a watershed, soil loss due to erosion is an important criterion to consider in choosing priority areas for restoration. Preventing and stabilizing erosion-prone land by increasing the vegetation cover is among the main objectives of restoration activities in a watershed [28]. A soil erosion map is produced using a method called Revised Universal Soil Loss Equation (RUSLE), explained in Section 2.2.3—Soil Erosion Map.
2.2.2. Data Acquisition and Sources
2.2.3. Map Generation for Each Criterion
Image Processing for Land Use/Land Cover (LULC)
Accuracy Assessment for LULC Classification Map
Soil Erosion Map
- A = the average annual soil loss (ton ha−1 yr−1)
- R = the rainfall-runoff erosivity factor (MJ mm ha−1 hr−1 yr−1)
- K = soil erodibility factor (ton ha hr MJ−1 ha−1 mm−1)
- LS = topographic steepness factor (based on length and slope)
- C = land cover management factor
- P = erosion-control practices factor
Factor | Estimation of Factor | Description | Source | |
---|---|---|---|---|
R | (3) | It quantifies the amount of runoff associated with the rain and was computed using global rainfall information from the Climatic Research Unit Database, based on 10-year average rainfall record (2011–2021). | [55] | |
where:
| ||||
K | (4) | It represents the susceptibility of soil to erosion depending on soil properties, rainfall, and runoff. Global Soil Data from the FAO Database was used to process K factor. | [56] | |
where:
| ||||
LS | (5) | It reflects the influence of topography on soil loss and computed using elevation data. | [57] | |
where:
| ||||
C, P | Refer to Table 3 | C factor denotes the rate of soil loss associated with a land use class and management practices and calculated using land cover classification of the study area from the classified satellite data. P factor reflects the rate of soil loss associated with support conservation practices such as contour farming, strip cropping, and terracing. | [52,58] |
2.2.4. Conception of the Land Suitability Analysis Model
- Reclassification of each criterion map: Once the five maps are generated, they are combined using a multicriteria analysis to generate the final suitability map. However, to make them comparable before the computation, a reclassification process was performed. Reclassification of the selected criteria is performed to better understand the importance of each criterion in the suitability assessment. It consists of replacing a new value in each criterion map to reclassify the vector and raster data [6,28]. The reclassification is based on the following levels of suitability: highly suitable (S1), moderately suitable (S2), marginally suitable (S3) and not suitable (N) (Table 4).
- Distance from protected areas and forest patches: The ranking system was based on natural forest regeneration through seed dispersal limitations Natural regeneration is highly favored in areas within an 100 m radius via short-distance dispersal (e.g., wind, gravity) [61,62] and still be possible via longer-distance dispersal within 100–1000 m (e.g., birds, bats, primates) [62].
- Soil loss priority and severity ranking: This was based on soil loss potential of the Abay river basin in Ethiopia, Africa, in which catastrophic soil loss is classified as greater than 500 t ha−1 yr−1, severe is between 50 to 500 t ha−1 yr−1, and less than 50 t ha−1 yr−1 is moderate to slight soil loss [61].
Suitability Class | |||||
---|---|---|---|---|---|
Criteria | Highly Suitable (S1) | Moderately Suitable (S2) | Marginally Suitable (S3) | Not Suitable (N) | Literature |
Distance from protected areas and forest patches (m) | <100 | 100–500 | 500–1000 | >1000 | [61,62] |
LULC | Forest (dense and degraded) | Grassland | Agriculture land, Bare land | Water, Rock | [6] |
Soil loss (t ha−1 yr−1) | >500 | 50–500 | 0–50 | [63] | |
Distance from settlements (m) | >2500 | 2000–2500 | 1500–2000 | <1500 | [7,11] |
Distance from roads (m) | >500 | 250–500 | 50–250 | <50 | [63] |
- Distance from settlements: we based the rank on the assessment made by [11] in north-eastern Madagascar, in which they conclude the range of influence of land users within a radius of about 2.5 km from the home village. We therefore set the distance of the most suitable areas to greater than 2500 m from settlements. However, we considered, at our own discretion, the radius within 1500–2500 m as moderately and marginally suitable because of some restoration activities such as agroforestry that local people usually practice around their villages [7,11].
- Distance from roads: the suitability class for distance from roads was estimated from a buffer analysis, based on previous urban development studies [64], and the influence of human disturbance from road infrastructures. Based on buffer analysis, the spatial agglomeration impacts of road infrastructures in the region are within 500 m in large cities and within 50 m in rural areas. Therefore, we set a margin value between 50 to 500 m as the basic buffer value.
- Designing Options for Priority Restoration Sites: The basic assumption that guided the process of land suitability is that a site can be restored only if it is sufficiently within or around forests and nature reserves; not in close proximity to agriculture, roads and settlements; and in erosion-prone land areas [28]. In other words, the most suitable site to be restored is that minimizing landscape fragmentation (distance from protected areas and forest patches, LULC), minimizing conflicts with human settlements, infrastructures, and agricultural fields (distance from settlements and roads, LULC), minimize soil erosion (soil loss). The rationale for this assumption was that restoring erosion-prone lands within a watershed with potential agricultural outcomes is likely to improve provision of ecosystem services, in particular water and soil quality, precisely where people are most exposed to land degradation, as in many rural areas in the Mahavavy region. For this reason, criteria related to distance from protected areas and forest patches, LULC, and soil loss were considered benefits, while criteria related to distance from settlements and distance from roads were considered costs.
3. Results
3.1. Soil Quantification and Mapping
3.2. Accuracy Assessment for LULC Classification
3.3. Land Suitability Analysis for Priority Restoration Areas
3.3.1. Reclassification of Criteria
3.3.2. Land Suitability Analysis
4. Discussion
5. Conclusions
Author Contributions
Funding
Data Availability Statement
Acknowledgments
Conflicts of Interest
References
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No. | Criteria | Scale/Resolution | Data Source |
---|---|---|---|
1 | Land use/Land cover | 30 m resolution | 2021, Landsat 8 OLI |
2 | Ambilobe District boundary Mahavavy Watershed boundary | 1:13,300,000 | Dataset- Humanitarian Data Exchange https://data.humdata.org. (Last accessed 19 October 2022) |
3 | Settlement | 30 m resolution | Landsat 8, Google Earth |
4 | Roads | 1:1,300,000 | Madagascar—Geofabrik Download Server https://download.geofabrik.de/africa/madagascar.html (Last accessed 19 October 2022 ) |
5 | Soil erosion | 1:1,300,000 | Elevation data using ASTER Global Digital Elevation Model (GDEM) from Earthdata.nasa.gov Global Soil Data from FAO Database https://data.apps.fao.org/map/catalog/srv/eng/catalog.search#/metadata/446ed430-8383-11db-b9b2-000d939bc5d8 (last accessed 19 October 2022) Rainfall Data 1901–2021 from CRU Database https://crudata.uea.ac.uk/cru/data/hrg/ (Last accessed 19 October 2022) |
The C Factor | The P Factor | ||
---|---|---|---|
Land Use/Land Cover Class | C Factor | Slope (%) | Contouring |
Dense forest | 0.0015 | 0.0–7.0 | 0.55 |
Degraded forest | 0.0200 | 7.0–11.3 | 0.60 |
Agriculture land | 0.4000 | 11.3–17.6 | 0.80 |
Water | 0.0000 | 17.6–26.8 | 0.90 |
Rock | 0.0000 | >26.8 | 1.00 |
Grassland | 0.0150 |
Weight | ||||
---|---|---|---|---|
Ecological Factors | Socio-Economic Factors | |||
Distance from protected areas and forest patches | LULC | Soil loss | Distance from settlements | Distance from roads |
0.25 | 0.25 | 0.16 | 0.17 | 0.17 |
Total weight: 0.50 | Total weight: 0.50 |
LULC Classification | Accuracy Assessment (%) | |||
---|---|---|---|---|
Producer’s Accuracy | User’s Accuracy | Overall Accuracy | Kappa Coefficient | |
Dense forest | 91.67 | 94.28 | 87.1 | 0.85 |
Degraded forest | 76.19 | 91.42 | ||
Grassland | 72.09 | 88.57 | ||
Agriculture land | 93.54 | 85.29 | ||
Waterbody | 100 | 96 | ||
Bare land | 100 | 71.43 | ||
Rock | 100 | 81.81 |
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Rajaonarivelo, F.; Williams, R.A. Remote Sensing-Based Land Suitability Analysis for Forest Restoration in Madagascar. Forests 2022, 13, 1727. https://doi.org/10.3390/f13101727
Rajaonarivelo F, Williams RA. Remote Sensing-Based Land Suitability Analysis for Forest Restoration in Madagascar. Forests. 2022; 13(10):1727. https://doi.org/10.3390/f13101727
Chicago/Turabian StyleRajaonarivelo, Fitiavana, and Roger A. Williams. 2022. "Remote Sensing-Based Land Suitability Analysis for Forest Restoration in Madagascar" Forests 13, no. 10: 1727. https://doi.org/10.3390/f13101727
APA StyleRajaonarivelo, F., & Williams, R. A. (2022). Remote Sensing-Based Land Suitability Analysis for Forest Restoration in Madagascar. Forests, 13(10), 1727. https://doi.org/10.3390/f13101727