4. Theoretical Framework
4.1. Cool Roof (Reflective Paint) Results
The cool roof (reflective paint) experiment conducted in Gimhae-si demonstrated a significant reduction in surface temperatures on the rooftops and external walls where reflective coatings were applied. The following key results were observed:
4.1.1 Surface Temperature Reduction:
The application of reflective coatings to rooftops led to a surface temperature reduction of up to 3°C compared to non-applied surfaces during peak heat hours (12:00–15:00). Buildings with both cool roof and cool wall treatments exhibited the greatest surface temperature reduction, consistently staying below 40°C, while untreated surfaces exceeded 40°C.
H1 (Coolwall + Roof) also showed the lowest rooftop surface temperatures, suggesting that the reflective coating on the roof effectively reduced overall heat absorption. During peak heat hours, H1 was about 2-3°C cooler than H2 and H3.
H2 (Coolwall) recorded surface temperatures higher than H1 but lower than H3, highlighting the importance of roof treatments. This suggests that while walls play a role in temperature reduction, the roof remains a critical factor in heat absorption and overall cooling. H3 (Non-applied) had the highest surface temperatures, particularly during peak hours, where temperatures often exceeded 40°C. Without reflective coatings, the roof absorbed substantial heat, leading to higher surface temperatures and increased internal and surrounding air temperatures.
4.1.2 Air Temperature Reduction:
Reflective surfaces contributed to an average air temperature reduction of 1-2°C at 1.5 meters above ground level. The largest cooling effects were observed during the hottest parts of the day, demonstrating that reflective coatings can mitigate heat buildup in the surrounding environment.
H1 (Coolwall + Roof) consistently showed the lowest air temperature readings at 1.5 meters compared to H2 (Coolwall) and H3 (Non-applied). The temperature reduction was particularly noticeable during the hottest parts of the day, where H1 remained 1-2°C cooler than H2 and H3. This highlights the efficacy of combining both cool walls and roofs in mitigating heat buildup around buildings. H2 (Coolwall) exhibited slightly higher temperatures compared to H1, but it was generally lower than H3 (Non-applied). This suggests that applying reflective paint only to the walls provided some benefit but was less effective than when both walls and roofs were treated. H3 (Non-applied) displayed the highest air temperatures, especially during afternoon peaks. This implies that without any reflective coatings, the structure absorbed and radiated more heat, leading to increased air temperatures in its vicinity.
The temperature differences between H1, H2, and H3 were most pronounced during peak heat periods (late morning to early afternoon. The cooling effect of H1 (Coolwall + Roof) was most significant during midday when solar radiation was highest, reinforcing the advantage of combining both cool walls and roofs for better temperature mitigation. Nighttime temperatures for all three areas converged, as the impact of direct solar radiation diminished after sunset, reducing the temperature differences.
4.1.3 Key Observations:
The surface temperatures in H1 stayed lower throughout the day, demonstrating the effectiveness of reflective coatings in keeping rooftops cool. This cooling likely reduced heat transfer into the building, enhancing indoor comfort as well.
These findings are consistent with previous research, confirming that cool roofs provide both direct cooling to buildings and secondary benefits by reducing the heat absorption in urban environments. H2 (Coolwall), though effective in lowering wall temperatures, had higher rooftop surface temperatures, emphasizing the need to treat both roofs and walls in heat mitigation strategies. H3 (Non-applied) exhibited the poorest thermal comfort, with much higher surface temperatures contributing to increased air temperatures and heat buildup in the surrounding environment.
Figure 8.
Comparing the 1.5M air temperatures and rooftop surface temperatures for the cool wall (top), cool wall + roof, and non-applied surfaces (bottom) during the period from August 27 to September 1, 2021. The results show significant differences in both air and surface temperatures, with the cool roof and cool wall applications reducing the surface temperature, especially during peak heat times.
Figure 8.
Comparing the 1.5M air temperatures and rooftop surface temperatures for the cool wall (top), cool wall + roof, and non-applied surfaces (bottom) during the period from August 27 to September 1, 2021. The results show significant differences in both air and surface temperatures, with the cool roof and cool wall applications reducing the surface temperature, especially during peak heat times.
Figure 9.
Daily temperature gaps between H1, H2, and H3 for both air temperature (top graph) and surface temperature (bottom graph). These graphs illustrate how the gaps fluctuate over the period from August 27 to August 31, 2021.
Figure 9.
Daily temperature gaps between H1, H2, and H3 for both air temperature (top graph) and surface temperature (bottom graph). These graphs illustrate how the gaps fluctuate over the period from August 27 to August 31, 2021.
4.2. Cooling Fog Results in Yechun-gun
The cooling fog system installed in Yechun-gun provided immediate and noticeable reductions in ambient air temperature in the playground where it was deployed. The key findings of the experiment are as follows.
4.2.1 Cooling Fog System Effect on Air Temperature:
The cooling fog system deployed in Yechun-gun demonstrated a clear and immediate reduction in ambient air temperature in the playground zone where it was activated. Before activation, the temperature in the cooling fog zone (W1) remained stable at approximately 35°C, while the sunny zone (W2) showed a slightly lower temperature, averaging around 30°C. After the activation of the cooling fog system at around 14:30, the air temperature in the W1 zone dropped sharply by approximately 1.3°C within the first 30 minutes, reducing the temperature to around 28.8°C. The cooling effect continued until around 15:00, with a total temperature reduction of 3.1°C compared to the pre-activation phase.
4.2.2 Humidity Increase:
In addition to temperature reduction, the cooling fog system significantly increased the relative humidity in the cooling fog zone. Before the system's activation, the humidity in the W1 zone was stable at around 41%, similar to the humidity levels in the W2 sunny zone. Once the system was turned on, the humidity in the W1 zone rose sharply to approximately 60% during the 14:30 to 15:00 period. The maximum humidity increase observed was around 20%, while the W2 zone remained stable at around 50% humidity. This shows that the fog system not only cooled the air but also increased moisture in the environment, improving thermal comfort.
4.2.3 Cooling Efficiency Analysis:
The analysis of the temperature difference between the cooling fog zone (W1) and the sunny zone (W2) further illustrates the cooling system’s efficiency. During the activation period, the temperature difference between the two zones widened, with W1 consistently remaining cooler by approximately 3°C. After the system was turned off at 15:00, the temperature in W1 gradually increased, but the cooling effect lingered, maintaining a lower temperature compared to W2, suggesting a lasting impact even after deactivation.
The overall cooling efficiency can be summarized as:
Pre-activation temperature difference: W1 was already cooler by approximately 1.8°C due to environmental factors.
Post-activation cooling effect: An additional 1.3°C temperature reduction was achieved after activation, for a total cooling effect of 3.1°C.
4.2.4 Key Observations:
Temperature Reduction: The cooling fog system led to a significant temperature reduction in the W1 zone, with a total drop of up to 3.1°C during its operational window (14:30–15:00). This cooling effect was observed rapidly within minutes of activation, proving the system's immediate efficiency.
Humidity Increase: The cooling fog system increased the relative humidity in the W1 zone by approximately 20%, further enhancing the cooling sensation and improving comfort in the surrounding area.
Extended Cooling Impact: The cooling effect was sustained even after the system was turned off, as temperatures in W1 remained lower compared to W2, suggesting that the system had a residual cooling impact.
Comparison with Sunny Zone (W2): While W2 experienced a steady temperature decrease due to natural conditions, it did not benefit from the sharp reduction observed in W1, indicating that the cooling fog system was the main driver of temperature reduction in W1.
These findings confirm that the cooling fog system is an effective tool for reducing ambient air temperature and increasing humidity, especially in outdoor recreational spaces like playgrounds. This system can be particularly useful in mitigating the effects of heat during peak afternoon hours, enhancing comfort and safety for users.
Figure 10.
The temperature in the cooling fog zone (W1) dropped noticeably between 14:30 and 15:00, reflecting the cooling effect of the system, while the sunny zone temperature (W2) remained relatively stable (top side). The humidity in the cooling fog zone spiked during the same period, indicating the activation of the fog system, while humidity in the sunny zone remained constant(bottom side). These graphs demonstrate the immediate cooling and humidifying effect of the cooling fog system in the playground.
Figure 10.
The temperature in the cooling fog zone (W1) dropped noticeably between 14:30 and 15:00, reflecting the cooling effect of the system, while the sunny zone temperature (W2) remained relatively stable (top side). The humidity in the cooling fog zone spiked during the same period, indicating the activation of the fog system, while humidity in the sunny zone remained constant(bottom side). These graphs demonstrate the immediate cooling and humidifying effect of the cooling fog system in the playground.
4.3. Shading Structure Results in Geyang-gu
The installation of shading structures in public spaces in Geyang-gu has shown promising results in reducing direct solar exposure and lowering air temperatures in shaded areas.
4.3.1 Shading Effect on Surface Temperature:
The installation of shading structures in the public playground of Geyang-gu had a significant effect on reducing surface temperatures in the shaded area (S1) compared to the unshaded sunny area (S2). In the early morning, surface temperatures in both zones remained relatively cool, ranging between 15°C to 20°C.
However, as sunlight exposure increased, the sunny zone (S2) experienced a sharp rise in surface temperature, peaking at approximately 55°C during midday. On the other hand, the surface temperature in the shaded zone (S1) rose more gradually, with maximum temperatures reaching around 45°C. The shading structure helped to maintain surface temperatures in S1 at a significantly lower level, especially during the hottest hours of the day. The maximum observed temperature difference between S1 and S2 was approximately 10°C.
4.3.2 Surface Temperature Reduction Efficiency:
The temperature difference between the shaded zone (S1) and the sunny zone (S2) became most pronounced during the peak sunlight hours, from approximately 12:00 PM to 3:00 PM. While the unshaded surfaces in S2 reached extreme temperatures of up to 55°C, the shaded zone (S1) remained consistently cooler by about 8°C to 10°C.
This effect demonstrates that the shading structure not only reduces direct sunlight exposure but also plays a crucial role in lowering surface temperatures, which is critical for improving the comfort and safety of users in public playgrounds and other outdoor spaces. The shading effect was most effective during midday when solar radiation was at its highest.
4.3.3 Cooling Efficiency Analysis:
The comparison of surface temperatures between the shaded zone (S1) and the sunny zone (S2) reveals the efficiency of the shading structure in mitigating heat. During peak sunlight, S2 surface temperatures spiked rapidly, while S1 surfaces increased at a much slower rate.
Throughout the day, the surface temperature difference between the two zones remained significant, particularly during the hottest parts of the day. The shaded zone (S1) consistently stayed cooler, with temperature reductions ranging from 5°C to 10°C compared to the sunny zone (S2). This difference highlights the effectiveness of the shading structure in cooling surfaces exposed to intense sunlight.
Summary of Cooling Efficiency:
Pre-peak temperature difference: S1 was cooler by an average of 2°C to 3°C in the morning.
Peak sunlight cooling effect: S1 surfaces were up to 10°C cooler than S2 during peak sunlight hours.
Overall cooling efficiency: The shading structure provided a substantial cooling effect, with up to 10°C surface temperature reduction compared to unshaded surfaces.
4.3.4 Key Observations:
Surface Temperature Reduction: The shading structure led to a notable reduction in surface temperature within the shaded zone (S1). During the hottest part of the day, the temperature in S1 was reduced by as much as 10°C compared to the sunny zone (S2), proving the structure's effectiveness in moderating surface heat.
Sustained Cooling Impact: Even after peak sunlight hours, the cooling effect in S1 persisted. The surface temperatures in the shaded zone remained significantly lower than those in the sunny zone, indicating a lasting cooling impact provided by the shading structure.
Comparison with Sunny Zone (S2): While the sunny zone (S2) experienced extremely high surface temperatures during midday (up to 55°C), the shaded surfaces in S1 remained much cooler. This demonstrates that shading is a critical factor in reducing surface temperatures in public spaces, making them safer and more comfortable for users.
These results confirm that shading structures can be highly effective in reducing surface temperatures in outdoor environments, particularly during the peak hours of sunlight. This has important implications for urban heat mitigation strategies, especially in spaces designed for public use, such as playgrounds and recreational areas.
Figure 11.
Surface temperature comparison between cool shadow zone(S1) and sunny zone (S2).As seen in the graph, the Sunny Zone experiences significantly higher temperature peaks compared to the Cool Shadow Zone, particularly during daytime hours. This illustrates the impact of shading structures in reducing temperature in public spaces.
Figure 11.
Surface temperature comparison between cool shadow zone(S1) and sunny zone (S2).As seen in the graph, the Sunny Zone experiences significantly higher temperature peaks compared to the Cool Shadow Zone, particularly during daytime hours. This illustrates the impact of shading structures in reducing temperature in public spaces.
Figure 12.
The temperature gap between the Sunny Zone (S2) and the Cool Shadow Zone (S1) over time. The graph illustrates that during peak sunlight hours, the temperature difference can reach up to 25°C, with the Sunny Zone (S2) being significantly hotter than the shaded area (S1). This demonstrates the substantial cooling effect of the shading structure, particularly during the hottest parts of the day.
Figure 12.
The temperature gap between the Sunny Zone (S2) and the Cool Shadow Zone (S1) over time. The graph illustrates that during peak sunlight hours, the temperature difference can reach up to 25°C, with the Sunny Zone (S2) being significantly hotter than the shaded area (S1). This demonstrates the substantial cooling effect of the shading structure, particularly during the hottest parts of the day.
4.4. Small water path Results in Sangju-si
The small water path installed in Namsan Park in Sangju-si demonstrates the cooling potential of passive water features in urban parks. The waterway provided a continuous cooling effect throughout summer.
4.4.1 Small Water Path Effect on Air Temperature::
The small water path installed in Namsan Park, Sangju-si, demonstrated a continuous cooling effect on air temperature in the immediate surroundings. Before the cooling effect of the water path became noticeable, temperatures in both the water path zone (P1) and the sunny zone (P2) remained relatively close, with P1 averaging approximately 35°C and P2 at around 36°C in the early afternoon on August 6.
As the day progressed and the water path's cooling influence became more apparent, P1 began to show consistently lower temperatures compared to P2. On average, the temperature in P1 was around 0.5°C to 1°C lower than P2 during the peak daytime hours. This cooling effect was most pronounced in the late afternoon and evening, demonstrating the water path's ability to moderate air temperature, particularly during the hottest periods of the day.
4.2.2 Humidity Increase:
In addition to reducing air temperature, the presence of the small water path led to an increase in relative humidity in the surrounding area. The humidity in the water path zone (P1) remained consistently higher than the sunny zone (P2) throughout the observation period.
In the morning of August 6, the humidity in P1 and P2 was relatively close, with both zones exhibiting levels between 60% and 65%. However, as the day progressed, P1 saw a sharp rise in humidity, peaking at over 90% in the late afternoon, while P2 remained slightly lower, averaging around 85%. This increase in relative humidity around the water path indicates that the feature not only cools the surrounding air but also adds moisture, improving thermal comfort.
4.2.3 Cooling Efficiency Analysis:
The temperature difference between the small water path zone (P1) and the sunny zone (P2) highlights the cooling efficiency of passive water features. During the observation period, P1 consistently remained cooler than P2, with the most significant temperature gap occurring in the late afternoon, where P1 was up to 1.5°C cooler than P2.
This cooling effect was sustained through the evening, as the water path continued to moderate the air temperature. Even during peak heat, the presence of the water path prevented the air in P1 from rising as sharply as in P2, creating a more comfortable environment for park users.
Summary of Cooling Efficiency:
Initial temperature difference: In the early afternoon, the temperature difference between P1 and P2 was minimal, with P1 being only about 0.5°C cooler.
Peak cooling effect: The maximum cooling effect was observed in the late afternoon, where P1 was up to 1.5°C cooler than P2.
Overall cooling impact: The small water path provided a consistent cooling effect, with an average temperature reduction of around 0.5°C to 1°C compared to the sunny zone.
4.2.4 Key Observations:
Temperature Reduction: The small water path demonstrated a significant temperature reduction effect, with air temperatures in P1 being up to 1.5°C cooler than the sunny zone (P2) during peak sunlight hours. This cooling effect was sustained throughout the day, particularly in the late afternoon.
Humidity Increase: The relative humidity in the water path zone (P1) was consistently higher than in the sunny zone (P2), with humidity levels in P1 reaching up to 90% during the hottest part of the day, compared to around 85% in P2. This indicates that the water path not only reduced air temperature but also increased moisture in the surrounding area, enhancing comfort.
Extended Cooling Impact: The cooling effect of the water path was maintained even after peak sunlight hours, suggesting a lasting cooling impact. As temperatures in P2 began to decline naturally, P1 continued to remain slightly cooler, demonstrating the residual cooling benefit of the water path.
Comparison with Sunny Zone (P2): While both zones experienced similar temperature trends throughout the day, P2 consistently showed higher temperatures, indicating that the small water path was the primary driver of the cooling effect in P1.
These findings confirm that passive water features, such as small water paths, are an effective tool for reducing air temperatures and increasing humidity in urban parks. These features are particularly useful for mitigating the effects of heat during peak afternoon hours, providing a more comfortable and enjoyable environment for park visitors.
Figure 13.
(a) Comparison of hourly air temperature measurements; (b) Comparison of hourly humidity measurements Here is the temperature comparison graph between the Small Water Path (P1) and the Sunny Zone (P2) from August 5 to August 8. The data indicates that the water path (P1) consistently showed lower temperatures than the sunny zone (P2), particularly during the night and early morning hours. However, during peak daylight, the temperatures of both zones remained quite close.
Figure 13.
(a) Comparison of hourly air temperature measurements; (b) Comparison of hourly humidity measurements Here is the temperature comparison graph between the Small Water Path (P1) and the Sunny Zone (P2) from August 5 to August 8. The data indicates that the water path (P1) consistently showed lower temperatures than the sunny zone (P2), particularly during the night and early morning hours. However, during peak daylight, the temperatures of both zones remained quite close.
Figure 14.
The temperature gap between the Sunny Zone (P2) and the Small Water Path (P1) from August 5 to August 8. The temperature difference fluctuates throughout the day, with P2 (sunny zone) generally being slightly warmer than P1 (water path), especially during the daytime. However, there are periods where P1 is briefly warmer, possibly due to local variations in air temperature.
Figure 14.
The temperature gap between the Sunny Zone (P2) and the Small Water Path (P1) from August 5 to August 8. The temperature difference fluctuates throughout the day, with P2 (sunny zone) generally being slightly warmer than P1 (water path), especially during the daytime. However, there are periods where P1 is briefly warmer, possibly due to local variations in air temperature.
Figure 15.
Humidity comparison between the Small Water Path (P1) and the Sunny Zone (P2) from August 5 to August 8. The small water path (P1) generally has higher humidity levels compared to the sunny zone (P2), especially during the late afternoon and evening hours. This shows the cooling water path's ability to increase moisture in the air, contributing to a more comfortable environment.
Figure 15.
Humidity comparison between the Small Water Path (P1) and the Sunny Zone (P2) from August 5 to August 8. The small water path (P1) generally has higher humidity levels compared to the sunny zone (P2), especially during the late afternoon and evening hours. This shows the cooling water path's ability to increase moisture in the air, contributing to a more comfortable environment.
4.5. Comparative Analysis of Technologies
The results demonstrated that each cooling technology provided measurable benefits in reducing temperatures and improving thermal comfort, albeit in different ways. Cooling fog and shading structures provided immediate relief in high-traffic areas, whereas cool roofs offered long-term reductions in building surface and indoor temperatures. Waterway shelters, such as the small water path, offer a steady cooling effect and enhance the aesthetic and psychological experiences in urban parks.
Cool Roof + Cool Wall: Combined treatments showed a 2-3°C reduction in surface temperature during peak hours, providing the greatest cooling effect on both air and surface temperatures. Shading Structures: 2.5°C reduction in air temperature, with a 50% reduction in solar radiation.
Cool Wall: A 1-2°C reduction in surface temperature, demonstrating that reflective walls are effective, but less so compared to when both roofs and walls are treated.
Cooling Fog: Showed an up to 3.1°C reduction in ambient air temperature during its operational window, making it highly effective for immediate cooling in high-traffic outdoor areas.
Shading Structures: Reduced surface temperatures by up to 10°C during peak sunlight hours, demonstrating significant cooling potential for public playgrounds and parks.
Small Water Path: Provided a 1.5°C reduction in air temperature during peak sunlight hours, with an additional benefit of increased humidity levels that enhanced thermal comfort
All technologies contributed to significant improvements in thermal comfort. Cooling fog was particularly effective in outdoor high-traffic areas, while shading structures and small water paths were well-received in parks and public spaces. Cool roofs and walls helped to mitigate heat in and around buildings, contributing to both indoor comfort and energy savings.
These results suggest that a combination of cooling fog, shading structures, and cool roofs could be the most effective solution for mitigating heat stress in urban environments, particularly for vulnerable populations. Small water paths, while offering less dramatic temperature reductions than cooling fog, provide steady, passive cooling solutions that are aesthetically pleasing and were well-received by park visitors.
Table 7.
Cooling solutions, their effectiveness in reducing temperatures, and key observations.
Table 7.
Cooling solutions, their effectiveness in reducing temperatures, and key observations.
Cooling Solution |
Temperature Reduction |
Key Observation |
Measurement Period |
Cool Roof + Cool Wall |
2-3°C during peak hours |
Combining both cool roof and cool walls showed the best reduction in surface and air temperatures. |
27 Aug. 2021 - 1 Sep. 2021 |
Cool Wall |
1-2°C compared to non-applied surfaces |
Effective for reducing wall temperatures but less effective compared to combined treatments. |
27 Aug. 2021 - 1 Sep. 2021 |
Cooling Fog System |
Up to 3.1°C during operational window |
Immediate reduction of ambient air temperature after system activation. |
13 Sep. 2021 (2:00 PM – 4:30 PM) |
Shading Structure |
Up to 10°C during peak sunlight |
Consistent cooling effect, especially during the hottest part of the day. |
30 Sep. 2021 - 4 Oct. 2021 |
Small Water Path |
Up to 1.5°C during peak sunlight |
Moderate temperature reduction with increased humidity levels in the surrounding area.1 |
5 Aug. 2023 - 8 Aug. 2023 |
5. Conclusion and Recommendations
5.1. Conclusion
This study evaluates the performance of several urban heat mitigation technologies, including cooling fog systems, cool roofs (reflective paint), shading structures, and small water paths, with a focus on improving the thermal comfort of vulnerable populations. Field tests, conducted from 2021 to 2023 in collaboration with the Korean Ministry of Environment, demonstrated that each technology has unique strengths in reducing surface and ambient temperatures, improving thermal comfort, and contributing to energy savings.
Cooling Fog was one of the most effective solutions for providing immediate temperature reductions in high-traffic outdoor areas, reducing ambient temperatures by up to 3.1°C during operational periods, which greatly improved perceived comfort.
Cool Roofs (Reflective Paint) offered significant reductions in both surface and indoor temperatures, contributing to long-term energy savings. Buildings treated with reflective coatings experienced surface temperature reductions of 2-3°C.
Shading Structures provided a low-maintenance solution for mitigating solar exposure and improving thermal comfort in outdoor public spaces. Surface temperature reductions of up to 10°C were recorded in shaded areas, particularly during peak sunlight hours.
Waterway Shelters offered steady passive cooling, with air temperature reductions of up to 1.5°C and humidity increases that enhanced thermal comfort for park visitors. This cooling effect was particularly noticeable in the late afternoon and evening hours.
The results suggest that a combination of these technologies can effectively mitigate heat stress in urban environments, especially for vulnerable populations such as the elderly, children, and individuals with health conditions. By integrating active cooling technologies (such as cooling fog systems) with passive solutions (such as shading structures, cool roofs, and small water paths), cities can create more thermally comfortable and sustainable environments.
5.2. Recommendations
Based on the findings of this study, the following recommendations are proposed for urban planners, policymakers, and local governments seeking to implement effective heat-mitigation strategies:
- 1.
Adopt a Holistic Approach to Urban Heat Mitigation
Cities should integrate both active and passive cooling technologies to address heat stress across a variety of environments. Cooling fog systems should be installed in high-traffic areas such as playgrounds, public squares, and transport hubs, whereas cool roofs and shading structures should be prioritized in areas where long-term energy savings and comfort are needed. Small water paths can be incorporated into parks and recreational spaces to provide passive cooling and enhance the aesthetic value of urban areas.
- 2.
Prioritize Vulnerable Populations in Heat Mitigation Efforts
Urban heat mitigation strategies should prioritize the protection of vulnerable populations, including the elderly, children, and low-income communities, who are disproportionately affected by extreme heat. The Korean Ministry of Environment’s initiative to fund and implement heat mitigation technologies in cities such as Yechun-gun and Sangju-si serves as a model for how local governments can support vulnerable groups through targeted interventions. Similar projects should be replicated in other regions to ensure that urban populations are protected from the adverse effects of climate change and heat waves.
- 3.
Incorporate Heat Mitigation into Urban Planning Policies
Urban planning policies should incorporate heat-mitigation measures as part of broader climate adaptation strategies. Local governments should mandate the use of cool roofs in new buildings, particularly in dense urban areas, and encourage the adoption of shading structures in public spaces. Additionally, small water paths and green infrastructure should be integrated into the design of parks and public spaces to provide passive cooling solutions that are both sustainable and aesthetically pleasing.
- 4.
Monitor and Evaluate the Effectiveness of Cooling Technologies
Continuous monitoring and evaluation of cooling technologies are essential to ensure their long-term effectiveness. Data collected through IoT-based sensors and user feedback should be analyzed regularly to assess the performance of cooling systems and identify areas for improvement. Policymakers should allocate resources for ongoing research and development of heat mitigation technologies, with a focus on optimizing their effectiveness under different environmental conditions.
- 5.
Collaborate with International Cities to Share Best Practices
Given the global nature of climate change, international collaboration between cities is crucial for sharing best practices and lessons learned from heat-mitigation projects. The successful implementation of heat mitigation technologies in Korea’s urban centers can serve as a valuable reference for other cities worldwide. Local governments should seek opportunities to collaborate with international partners to exchange knowledge, develop innovative solutions, and improve their resilience to extreme heat.
5.3. Future Research
While this study provides valuable insights into the effectiveness of various cooling technologies, further research is needed to explore the long-term impacts of these interventions under changing climate conditions. Future studies should focus on the following aspects.
Long-term Monitoring: The monitoring period should be extended to assess the year-round performance of cooling technologies and their effectiveness under different seasonal conditions.
Cost–benefit Analysis: Future studies should conduct detailed cost-benefit analyses of cooling technologies to determine the most cost-effective solutions for urban areas with varying budget constraints.
Integration of Green Infrastructure: Research should explore how cooling technologies can be combined with green infrastructure (e.g., urban forests and green roofs) to maximize their cooling potential while enhancing biodiversity and environmental sustainability.