Submitted:
03 January 2024
Posted:
04 January 2024
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Abstract
Keywords:
1. Introduction
2. Materials and Methods
2.1. Modelling framework
- Open Source: TEMOA is open source, providing the transparency and customization needed for research. TEMOA's code is written in Python and optimized in Pyomo, a Python library for optimization, so it has no accessibility constraints.
- Similarity to other Models: The TEMOA model formulation is similar to the model generators MARKAL/TIMES [8,33], MESSAGE [34,35], and OSeMOSYS [36], Such tools, already commonly used in energy planning (e.g., MESSAGE in Syria [35], OSeMOSYS in Colombia [37] , TEMOA-US [38]. Moreover, TEMOA is a validated tool which convergence with the well-established TIMES framework has already been demonstrated in an Italian modeling instance [39].
2.2. Case study: The Pantelleria Island
- Consistency with research objectives: As stated in Section 1, the focus of the analysis is to test the effectiveness of a spatially explicit model on a small scale. This defines the size of the area to be studied. In addition, it was specified that the suitability phase of the land can be an important factor in reducing soil availability. Therefore, the selection of a critical context from this point of view is necessary.
- Territorial and technological diversity: According to Stolten et.al [24], the benefit of the spatially explicit planning is higher if the territory under analysis presents geographical differences from the point of view of distribution of energy resources and possible land uses. For this reason, the choice of a small area but with characteristics of diversity, is a fundamental element.
- Data availability: The analysis is more significant if the data (both for the phase of suitability of the land and for the estimation of the energy potential) are present and at high resolution.
- Availability of modeling instances: The presence of existing and validated models on the chosen platform represents a strong added value in terms of reproducibility of the study.
2.3. Geospatial data and tools for land elegibility and energy potential analysis
2.4. Land eligibility analysis
2.5. Potential Assessment
- Reanalysis: The reanalysis methodology integrates numerical weather prediction models with observed datasets, yielding comprehensive datasets encompassing various meteorological parameters [55]. Examples include ERA5 [69] and MERRA2 [68], which serve as reputable sources for historical climate data assessment in wind resource studies, while similar data sources exist for solar energy assessments [74].
- Climate models: Climate models from initiatives like the Climate Model Intercomparison Project (CMIP) and CORDEX simulate future climate conditions, facilitating the assessment of wind and solar resource variability in response to long-term climate changes ([70], [71]). These models are instrumental in understanding the potential impacts of climate change on renewable energy resources.
- Atlas: Wind and solar atlases, exemplified by the New European Wind Atlas (NEWA) and the Global Wind Atlas (GWA), offer high-resolution spatial information regarding energy potentials in specified regions ([75], [78]). These atlases play a crucial role in renewable energy planning and development by providing detailed assessments of wind and solar resources.
2.5.1. Photovoltaic Potential Assessment
- represents the average global horizontal irradiation (kWh/m2/time).
- indicates the area within grid cell 'i' suitable for PV implementation (km2).
- represents the efficiency of the PV module in converting sunlight to electricity, with an assumed value of 21% [65].
- denotes the performance ratio for the solar module, set at 0.85 [65]. This ratio accounts for the disparity between performance under standard test conditions and the actual system output, factoring in losses due to conduction and thermal effects.
- signifies the total number of hours in a year, equivalent to 8760.
- represents the power density or of the solar PV system. For this study, we employed a value of 32 MW/km2 for a fixed-tilt utility-scale solar system using mono-crystalline silicon cells, which is the most common in actual market [89].
2.5.2. Wind Potential Assessment
2.5.3. Cost Assessment
2.6. Data aggregation
2.7. Model Integration
- 1)
- Insert in TEMOA a new set that describe the land resource. Traditional ESOM elements (mainly process and commodities) do not allow for a proper land representation. Indeed, it would be wrong to model the land consumed by plants installation as a commodity or a technology, for two main reasons. First, a commodity is something that is exchanged between processes as input or output. Here, the role of land is to host its associated technology (at certain conditions of capacity factor and cost) for the lifetime of this last. Second, the commodity consumption is related to the activity of a plant, passing through its efficiency (e.g., natural gas consumption proportional to combined cycle plant activity). In this case, land is consumed when new capacity is installed and becomes available as soon as the installed technology on that land dies. As depicted in Equation(5) and (6), the new TEMOA set is called for which a value is associated, describing the available area for the land cluster “l”.
- 2)
- Insert in the model a new parameter and new constraint, linking the capacity installation to land consumption. Indeed, as shown in Equation (7), the Land Use Intensity (LUI) parameter acts as a critical bridge linking the land clusters “ ” with the applicable technologies “j”. It quantifies the amount of land required for the installation of a unit of technology (e.g., megawatt of wind or solar power). The LUI parameter ensures that the model's solutions are not just economically optimized but also spatially feasible. If an LUI is not defined for a specific technology within a given land cluster, it implies that the technology cannot be installed in that cluster, thereby introducing a direct spatial constraint into the optimization process.
3. Results
3.1. TEMOA-Pantelleria input differences
3.2. TEMOA-Pantelleria energy scenario analysis
4. Discussion
5. Conclusions
Author Contributions
Funding
Acknowledgments
Conflicts of Interest
References
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| Administrative | Technical | Economic | Social | Year | Source |
|---|---|---|---|---|---|
| v | v | 2014 | [51] | ||
| v | v | v | v | 2018 | [21] |
| v | v | v | 2020 | [52] | |
| v | v | v | v | 2020 | [53] |
| v | v | v | v | 2021 | [27] |
| v | v | 2022 | [54] | ||
| v | v | v | v | 2022 | [55] |
| v | v | v | v | 2023 | [56] |
| Area | Constraint | Exlcusion rule | Source |
|---|---|---|---|
| Environmental/Technical | Wind Speed | below 4.5 m/s | RSE [43] |
| Irradiance | below 3.0 kWh/m2 day | UMEP ERA 5 [62] | |
| Slope | ≥15% | TinItaly [63] | |
| Permanent crops | Inside | CLC [60] | |
| Water bodies | Inside | - | |
| Rocks | Inside | - | |
| Coast | Inside | - | |
| Administrative/Habitat | Natural Habitats | Inside | Natura 2000 [64] |
| Bird Areas | Inside | - | |
| Biospheres | Inside | WDPA [58] | |
| Protected Landscape | <1000 m | - | |
| Reserves | Inside | - | |
| Parks | Inside | - | |
| Monuments | 1000 m | - | |
| Hydrological risk | Inside | GeoPortale [] | |
| Anthropic | Road distance | 100 m | OpenStreetMap [59] |
| Urban settlement | 200 m | - | |
| Industrial sites | 200 m | - | |
| Airport | 1500 m (Wind Only) | - | |
| Recreational Areas | 200 m | - |
| Technology | Data typology | Database names | Coverage | Resolution | |||
|---|---|---|---|---|---|---|---|
| Spatial | Temporal | Spatial | Temporal | ||||
| General | Observation | HadISD [66], Tall Tower Database [67] | Global | Historical, 20-50 years | Site specific | 5 min - 1 hr | |
| Reanalysis | MERRA-2 [68], ERA5 [69] | Global | Historical, 40-70 years | 30-60 km | 1-6 hr | ||
| Climate models | CMIP5 [70],EUROCORDEX [71] | Global | Historical and future, 80-250 years | 10-300 km | Hr- Montly | ||
| Solar | Atlas | GSA [72], SolarGIS [73] | Global | Historical | 90 m | 0.5-1 hr | |
| Reanalysis | HelioClim-3 [74] | Global | Historical and real time | 3 km | 15 min - 1 hr | ||
| Wind | Reanalysis | NEWA [75], DOWA [76], RSE[77] | Regional (EU) | Historical, 11-30 years | 1,5-3 km | 0.5-1 hr | |
| Atlas | GWA [78] | Global | Historical average | 50-200 m | N/A | ||
| Reanalysis | WINDographer [79], Mesonet [80] | USA | Historical | 3 km | Hourly | ||
| Reference Height [m] | WTG model | Nominal Power [MW] | Rotor Diameter [m] | Hub Height [m] |
|---|---|---|---|---|
| 50 m | Riva Calzoni 500.54 | 0.5 | 54 | 50 |
| 75 m | Leitwind LTW90- 950 | 0.95 | 90 | 80 |
| 100 m | Vestas V117 3450 | 3,45 | 117 | 91 |
| 125m | NREL_6MW_RTW | 6 | 128 | 119 |
| Method | Silhouette Score | Time (seconds) | Memory (MB) |
|---|---|---|---|
| HDBSCAN | 0.527 | 1,729 | 2,246 |
| Kmeans | 0.827 | 0.369 | 0.224 |
| DBSCAN | 0.807 | 2,940 | 0.810 |
| Land Cluster | Available area [km2] | Installable technologies |
|---|---|---|
| LC_1 | 2,850 | PV2_N |
| LC_2 | 0.457 | WIN1_N, PV_1 |
| LC_3 | 4,909 | PV_1 |
| LC_4 | 1,947 | PV_ 3, WIN2_N |
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