Application of Solar HVAC System in Residential Buildings for Winter Conditions in Mediterranean Climate
Abstract
1. Introduction
2. Concepts
- Indoor environmental: air temperature (ta), relative air humidity (RH), mean radiant temperature (tr) and relative air velocity (va);
- Personal: metabolic rate and clothing insulation.
3. Numerical Models
3.1. CAD Software
- Space 1—External environment: The variables air temperature, air relative humidity, wind speed and direction obtained for this space are used as input data in the Building Dynamic Response numerical model;
- Space 2—Building entrance hall; it has a glazed entrance door facing south;
- Space 3—Living room; it has a large window facing south;
- Space 4—Kitchen; it has a small window facing north;
- Space 5—Bedroom; it has a window facing east;
- Space 6—Bathroom; it has a window facing south.
3.2. Building Thermal Dynamic Numerical Model
- Building geometry: This geometry is developed numerically through geometric equations or CAD software. In this study, CAD software is used (see Section 3.1). This data is used in the evaluation of the energy and mass balance integral equations;
- Materials that make up the building: Introduction of all layers of materials in the building and ducts and their respective characteristics; namely, thickness, thermal conductivity, specific mass and specific heat;
- Environmental external conditions: Air temperature, air relative humidity, wind velocity, wind direction, and CO2 concentration;
- Geographic conditions: Building location (latitude) and height above sea level;
- Space occupancy cycle: Number of people and their respective time distribution throughout the day in the building’s spaces;
- Ventilation typologies: Characterization of the distribution of air flows, throughout the day, between the different spaces and between the spaces and the external environment so that it is possible to assess the mass exchange between spaces and between the spaces and the external environment;
- Other data input.
- Heat transfer coefficients by natural, forced or mixed convection;
- Mass transfer coefficients by diffusion;
- Solar radiation on external and internal surfaces. When calculating solar radiation, existing shading devices are taken into account;
- Incident solar radiation, absorbed solar radiation by transparent bodies (glasses) and opaque bodies, and the transmitted solar radiation through the transparent (glasses) bodies. The phenomenon of radiation considers the presence of all shading devices;
- Heat exchange by radiation, in each space. In this calculation, the radiosity equations and mean radiant temperature concepts are used;
- Mass adsorption and desorption;
- Temperatures in the following opaque bodies: doors, walls, floor and ceiling;
- Temperatures in the glazed bodies;
- Temperatures in the body of each duct section;
- Temperature of the water inside the ducts;
- Temperatures of the seats, desks and other interior bodies;
- Internal air temperature of the building’s spaces;
- Mass concentration of the water vapor inside the building’s indoor spaces;
- Mass concentration of contaminants (e.g., CO2) inside the building’s indoor spaces;
- IAQ assessed by CO2 concentration released in the respiration process. When calculating this value, the air exchange rate, the number of occupants in the space and the volume of the compartment are taken into account.
4. Methodology
4.1. Case Study
- Solar water collectors, installed on the roof, whose water will be heated by solar radiation. The system consists of a duct system and a water tank. The heated water will be used in thermo-convectors. The tank is connected to water–air thermo-convectors to heat the cold air using the heated water;
- Water–air heat exchanger thermo-convectors, installed inside each space with planned occupancy, namely spaces numbered 2, 3, 4, 5 and 6. In this way, this system allows the interior air to be heated.
4.2. Building Materials
4.3. External and Geographic Conditions
- Outdoor air temperature, with values between 4.7 °C (at 6.26 am) and 15.0 °C (at 1.26 pm), with fluctuations of around 1.0 °C;
- Outdoor air relative humidity, with values between 64.0% (at 7.45 am) and 37.2% (at 1.26 pm), with fluctuations of around 5.0%;
- Average value of wind speed is 12.30 m/s, with fluctuations around 5.83 m/s;
- CO2 concentration in the external environment was taken to be 400 ppm.
4.4. Occupancy Cycle
4.5. Ventilation Topology
- When the space is unoccupied, the airflow rate is one air change per hour (ACH) obtained by air infiltration.
4.6. Solar HVAC System Operation
- The solar HVAC system is running between 8 a.m. and 7 p.m. in the spaces (numbered 2, 3, 4, 5 and 6) with expected occupancy;
- The solar HVAC system is turned off between 7 p.m. and 8 a.m. in the same spaces mentioned above.
5. Results and Discussion
5.1. Environmental Variables
5.2. Thermal Comfort
5.3. Indoor Air Quality
6. Discussion
7. Conclusions
- During the day, the indoor air temperature and the PMV index in space 6 with a south-facing window are not affected by the use of the solar HVAC system as the entry of solar radiation into that space is sufficient to guarantee acceptable levels of thermal comfort.
- During the day, the indoor air temperature and the PMV index in space 3 with a south-facing window are affected by the use of the solar HVAC system in the early morning and late afternoon, contributing to these periods to provide acceptable levels of thermal comfort. Between these two periods, the acceptable level of thermal comfort is due to the entry of solar radiation into this space.
- During the day, the indoor air temperature values and the PMV index in spaces 2, 4 and 5 are positively affected by the use of the solar HVAC system, contributing to improving thermal comfort levels so that they are within acceptable levels between mid-morning and late afternoon.
- During the night occupancy period, thermal comfort levels are close to the acceptable level due to negative values of the PMV index.
- The use of the solar HVAC system allows for a reduction in CUH values of 55.0%, 85.7% and 18.8% in compartments 3, 4 and 5, respectively.
- In general, in spaces with windows facing south (during the day), in occupied spaces (during the night), and in spaces where the solar HVAC system is on, the value of the indoor air temperature is higher than the value of the mean radiant temperature.
- The proposed ventilation system provides an acceptable IAQ level.
Author Contributions
Funding
Institutional Review Board Statement
Informed Consent Statement
Data Availability Statement
Acknowledgments
Conflicts of Interest
References
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| Space Number | Time Period (Hours) | |||||
|---|---|---|---|---|---|---|
| 0:00–8:00 | 8:00–12:00 | 12:00–14:00 | 14:00–18:00 | 18:00–19:00 | 19:00–24:00 | |
| 3 | 0 | 0 | 0 | 0 | 0 | 2 |
| 4 | 0 | 0 | 2 | 0 | 1 | 0 |
| 5 | 2 | 0 | 0 | 0 | 0 | 0 |
| 6 | 0 | 0 | 0 | 0 | 1 | 0 |
| Compartment | 2 | 3 | 4 | 5 | 6 | |
|---|---|---|---|---|---|---|
| Solar HVAC system off | WUH | 0 | 0 | 0 | 0 | 0 |
| CUH | 0 | 3.42 | 5.86 | 15.33 | 0 | |
| Solar HVAC system on | WUH | 0 | 0 | 0 | 0 | 0 |
| CUH | 0 | 1.54 | 0.84 | 12.45 | 0 | |
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Conceição, E.; Gomes, J.; Conceição, M.; Conceição, M.I.; Lúcio, M.M.; Awbi, H. Application of Solar HVAC System in Residential Buildings for Winter Conditions in Mediterranean Climate. Atmosphere 2026, 17, 211. https://doi.org/10.3390/atmos17020211
Conceição E, Gomes J, Conceição M, Conceição MI, Lúcio MM, Awbi H. Application of Solar HVAC System in Residential Buildings for Winter Conditions in Mediterranean Climate. Atmosphere. 2026; 17(2):211. https://doi.org/10.3390/atmos17020211
Chicago/Turabian StyleConceição, Eusébio, João Gomes, Margarida Conceição, Maria Inês Conceição, Maria Manuela Lúcio, and Hazim Awbi. 2026. "Application of Solar HVAC System in Residential Buildings for Winter Conditions in Mediterranean Climate" Atmosphere 17, no. 2: 211. https://doi.org/10.3390/atmos17020211
APA StyleConceição, E., Gomes, J., Conceição, M., Conceição, M. I., Lúcio, M. M., & Awbi, H. (2026). Application of Solar HVAC System in Residential Buildings for Winter Conditions in Mediterranean Climate. Atmosphere, 17(2), 211. https://doi.org/10.3390/atmos17020211

