Land Use Changes for Investments in Silvoarable Agriculture Projected by the CLUE-S Spatio-Temporal Model
Abstract
:1. Introduction
2. The CLUE-S Spatiotemporal Model
3. Materials and Methods
3.1. Study Area and Forecasting Period
3.2. Variables Input for CLUE-S Model
3.3. Selection and Digital Preparation of the Land Uses at Year 2020
3.4. Statistical Analysis
- The exponential coefficients (EXP (b)), as a result of the increase of the negative logarithm (e) in the value of the coefficients (bi).
- The Relative Influence Index (RII) of the independent variables, defined as exp(b x variable’s value range).
- The area under the ROC (Relative Operating Characteristic) curve (AUC) as a measure of controlling the goodness of fit of the data to the logistic regression model.
- The coefficients of elasticity of the land uses of Mouzaki against the drivers of change to which they are exposed. The value of 1 was given to those land uses that are considered stable and unchanged, so the values close to 1, as given to the categories of Unused land, Settlements, and Forests (0.9, Table 2), reflect land uses that show a high degree of stability and are considered difficult to change. The value 0 (or close to 0) was given to land uses that are vulnerable to change, such as Grasslands, Open Shrublands, and Silvopastoral, which are very easily to change. All other land uses received intermediate values (Table 2). Although most transformations were permissible, some, such as those of Dense shrubland and Forests, were considered permissible only in certain land use units. The category of Urban land was considered practically unchanged and a stable unit of the landscape, and for this reason all its transformations to another use took the value of 0. With regard to the constraints that could additionally be defined within the transformation matrix, value 16 stipulated that the conversion of grassland into forest was not permissible in the eastern areas of the landscape (Figure 2). Finally, value 110 stipulated that the direct conversion of grassland into forest would be possible only after a period of at least 10 years.
- The matrix of permissible transformations of the landscape of Mouzaki, shown in Table 3, where the rows express the current land uses while the columns represent the possible future ones to which the current ones can switch. A value of 1 indicates that transformation is permissible, while a value of 0 indicates that it is not. The results of the diagram of diachronic transformations of the landscape were utilized for the construction of the matrix.
3.5. Socioeconomic Scenarios
3.6. Data Processing in CLUE-S
3.7. Production of Probability Maps and Landscape Change
3.8. Model Validation and Calibration
4. Results
4.1. Landscape Driving Factors
4.2. Logistic Regression—Probability Maps
4.3. Implementation of Socioeconomic Scenarios
5. Discussion
5.1. Scenario Analysis
5.2. Investment on Agroforestry
5.3. EU CAP and Investment in Agroforestry
5.4. Limitations of the Research
6. Conclusions
Author Contributions
Funding
Data Availability Statement
Acknowledgments
Conflicts of Interest
References
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a/a | Independent Variables * | Type/Unite | Data Source |
---|---|---|---|
1 | Elevation zones | Continuous/m | DEM Aster 2 |
2 | Slopes | Continuous/% | DEM Aster 2 |
3 | Alluvial deposits/Very deep soils | Binary/0–1 | Soil map (Nakos 1991) |
4 | Limestone/Medium -Shallow to rocky soils | >> | >> |
5 | Flysch/Deep soils | >> | >> |
6 | Tertiary deposits/Deep to medium depth soils | >> | >> |
7 | Peridotite-Gabbro/Medium depth soils | >> | >> |
8 | Schist/Deep soils | >> | >> |
9 | River bedrock/Rocky soils | >> | >> |
10 | Erosion potential | Continuous/(t × Ha−1 × year−1) | Soil Erosion by Water (RUSLE 2015)/ESDAC ** |
11 | Distance from road network | Continuous/m | Digital files from State Cadastre, Google Earth |
12 | Distance from hydrological network | >> | Hydrological model from DEM, topographic maps, Google Earth |
13 | Distance from urban centres | >> | Land use map 2020 |
14 | Inhabitant density | Continuous/Number × Ha−1 of the total area | Official State Data (statistics.gr) |
15 | Sheep density | >> | Municipality services of Mouzaki |
16 | Goat density | >> | >> |
Land Use Categories | Coefficient of Elasticity |
---|---|
Agricultural land | 0.5 |
Silvoarable land | 0.8 |
Grassland | 0.0 |
Silvopastoral woodland (10–40% tree cover) | 0.1 |
Forest (40–100% tree cover) | 0.5 |
Sparse shrubland (10–40% shrub cover) | 0.1 |
Dense shrubland (40–100% shrub cover) | 0.9 |
Urban land | 0.9 |
Barren land | 0.9 |
SA (0) | AL (1) | G (2) | SS (3) | DS (4) | SW (5) | F (6) | ST (7) | BL (8) | |
---|---|---|---|---|---|---|---|---|---|
SA (0) | 1 | 1 | 1 | 1 | 1 | 1 | 1 | 1 | 0 |
AL (1) | 1 | 1 | 1 | 1 | 1 | 1 | 110 | 1 | 0 |
G (2) | 1 | 1 | 1 | 1 | 1 | 1 | 16 | 1 | 0 |
SS (3) | 1 | 1 | 1 | 1 | 1 | 1 | 1 | 1 | 0 |
DS (4) | 0 | 0 | 0 | 1 | 1 | 1 | 1 | 1 | 0 |
SW (5) | 1 | 1 | 0 | 0 | 0 | 1 | 1 | 1 | 0 |
F (6) | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 |
ST (7) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
BL (8) | 1 | 1 | 1 | 1 | 1 | 1 | 1 | 1 | 1 |
Independent Variables * | SA | AL | G | SS | DS | SW | F | ST | BL |
---|---|---|---|---|---|---|---|---|---|
Elevation zones | −0.005 | 0.005 | −0.002 | −0.004 | −0.001 | −0.001 | |||
(0.995) | (1.005) | (0.998) | (0.996) | (0.999) | (0.999) | ||||
[−6086.3] | [7181.3] | [−33.45] | [−1114.5] | [−2.871] | [−14.17] | ||||
Slopes | −0.043 | −0.084 | −0.009 | −0.013 | 0.012 | 0.007 | 0.018 | 0.076 | |
(0.958) | (0.920) | (0.991) | (0.987) | (1.012) | (1.007) | (1.019) | (1.079) | ||
[−132.0] | [−12,296.5] | [−2.674] | [−4.427] | [3.699] | [2.138] | [7.942] | [5288.5] | ||
Alluvial deposits/Very deep soils | 1.428 | 2.425 | 1.828 | −2.513 | −3.745 | 3.352 | |||
(4.169) | (11.30) | (6.223) | (0.081) | (0.024) | (28.57) | ||||
[4.169] | [11.30] | [6.223] | [−12.34] | [−42.31] | [28.57] | ||||
Limestone/ Medium—Shallow to rocky soils | 5.448 | 7.792 | −0.531 | ||||||
(232.2) | (2420.5) | (0.588) | |||||||
[232.2] | [2420.5] | [−1.700] | |||||||
Flysch/Deep soils | 2.227 | 0.891 | 1.801 | 6.811 | 0.926 | −1.474 | |||
(9.276) | (2.438) | (6.057) | (907.6) | (2.524) | (0.229) | ||||
[9.276] | [2.438] | [6.057] | [907.6] | [2.524] | [−4.368] | ||||
Tertiary deposits/Deep to medium depth soils | 1.737 | 3.169 | 4.180 | 6.964 | −1.081 | −0.807 | |||
(5.678) | (23.79) | (65.35) | (1058.1) | (0.339) | (0.446) | ||||
[5.678] | [23.79] | [65.35] | [1058.1] | [−2.947] | [−2.241] | ||||
Peridotite-Gabbro/Medium depth soils | 7.032 | 8.260 | |||||||
(1132.5) | (3867.9) | ||||||||
[1132.5] | [3867.9] | ||||||||
Schist/Deep soils | 1.869 | −0.999 | 4.609 | ||||||
(6.483) | (0.368) | (100.4) | |||||||
[6.483] | [−2.715] | [100.4] | |||||||
River bedrock/Rocky soils | 1.006 | −1.643 | 4.714 | ||||||
(2.734) | (0.193) | (111.5) | |||||||
[2.734] | [−5.171] | [111.5] | |||||||
Erosion potential | 0.027 | 0.023 | 0.020 | 0.027 | −0.015 | 0.021 | |||
(1.027) | (1.023) | (1.020) | (1.028) | (0.985) | (1.021) | ||||
[158.0] | [78.39] | [42.79] | [173.2] | [−17.51] | [55.19] | ||||
Distance from road network | −0.001 | 0.002 | 0.006 | ||||||
(0.999) | (1.002) | (1.006) | |||||||
[−3.520] | [9.924] | [8932.9] | |||||||
Distance from hydrological network | −0.001 | 0.001 | 0.001 | 0.001 | −0.001 | −0.002 | |||
(0.999) | (1.001) | (1.001) | (1.001) | (0.999) | (0.998) | ||||
[−8.288] | [2.423] | [4.146] | [3.996] | [−3.234] | [−15.21] | ||||
Distance from urban centres | −0.001 | 0.001 | 0.000 | 0.000 | 0.003 | −0.006 | |||
(0.999) | (1.001) | (1.000) | (1.000) | (1.003) | (0.994) | ||||
[−365.2] | [471.9] | [6.235] | [−8.351] | [10,681,724.0] | [−5.0 × 1012] | ||||
Inhabitant density | −4.955 | 0.281 | 0.692 | −2.358 | (1.000) | −0.546 | −0.904 | 1.009 | |
(0.007) | (1.325) | (1.999) | (0.095) | (0.579) | (0.405) | (2.744) | |||
[−12,114.4] | [1.706] | [3.721] | [−87.81] | [−2.820] | [−5.558] | [6.788] | |||
Sheep density | (1.000) | 1.108 | 0.468 | 0.271 | 0.375 | 0.431 | −28.026 | −18.535 | −32.210 |
(3.029) | (1.596) | (1.311) | (1.455) | (1.539) | (0.000) | (0.000) | (0.000) | ||
[1101.4] | [19.22] | [5.546] | [10.69] | [15.25] | [−8.4 × 1076] | [−7.5 × 1050] | [2.6 × 1088] | ||
Goat density | 1.711 | −2.220 | 0.997 | 0.652 | 0.859 | −35.78 | −27.80 | ||
(5.532) | (0.109) | (2.709) | (1.920) | (2.361) | (0.000) | (0.000) | |||
[81.14] | [−300.2] | [12.95] | [5.345] | [9.097] | [−8.5 × 1039] | [−1.1 × 1031] | |||
Constant | −2.265 | −2.970 | −6.766 | −7.273 | −9.948 | −1.624 | 0.581 | 2.461 | −8.512 |
(0.104) | (0.051) | (0.001) | (0.001) | (0.000) | (0.197) | (1.787) | (11.71) | (0.000) | |
AUC | 0.939 | 0.968 | 0.835 | 0.937 | 0.923 | 0.867 | 0.997 | 0.982 | 0.946 |
Land Use | 2020 | BAU 2040 | RED 2040 | ELP 2040 |
---|---|---|---|---|
Silvoarable | 565 | 645 (+14.16%) | 887 (+56.99%) | 557 (−1.42%) |
Agricultural land | 11,148 | 10,358 (−7.09%) | 11,149 (+0.01%) | 10,344 (−7.21%) |
Grassland | 2421 | 1990 (−17.80%) | 2044 (−15.57%) | 1990 (−17.80%) |
Sparse shrubland | 503 | 514 (+2.19%) | 503 (-) | 505 (+0.40%) |
Dense shrubland | 782 | 608 (−22.25%) | 611 (−21.87) | 609 (−22.12%) |
Silvopastoral woodland | 3819 | 4003 (+4.82%) | 3819 (-) | 3818 (−0.03%) |
Forest | 10,561 | 11,682 (+10.61%) | 10,617 (+0.53%) | 12,036 (+13.97%) |
Settlements | 1458 | 1458 (-) | 1687 (+15.71%) | 1458 (-) |
Barren land | 90 | 89 (−1.11%) | 30 (−66.67% | 30 (−66.67%) |
Total (Ha) | 31,347 | 31,347 | 31,347 | 31,347 |
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Nasiakou, S.; Vrahnakis, M.; Chouvardas, D.; Mamanis, G.; Kleftoyanni, V. Land Use Changes for Investments in Silvoarable Agriculture Projected by the CLUE-S Spatio-Temporal Model. Land 2022, 11, 598. https://doi.org/10.3390/land11050598
Nasiakou S, Vrahnakis M, Chouvardas D, Mamanis G, Kleftoyanni V. Land Use Changes for Investments in Silvoarable Agriculture Projected by the CLUE-S Spatio-Temporal Model. Land. 2022; 11(5):598. https://doi.org/10.3390/land11050598
Chicago/Turabian StyleNasiakou, Stamatia, Michael Vrahnakis, Dimitrios Chouvardas, Georgios Mamanis, and Vassiliki Kleftoyanni. 2022. "Land Use Changes for Investments in Silvoarable Agriculture Projected by the CLUE-S Spatio-Temporal Model" Land 11, no. 5: 598. https://doi.org/10.3390/land11050598
APA StyleNasiakou, S., Vrahnakis, M., Chouvardas, D., Mamanis, G., & Kleftoyanni, V. (2022). Land Use Changes for Investments in Silvoarable Agriculture Projected by the CLUE-S Spatio-Temporal Model. Land, 11(5), 598. https://doi.org/10.3390/land11050598