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Article

Thermal Comfort in Urban Open Green Spaces: A Parametric Optimization Study in China’s Cold Region

1
College of Landscape Architecture and Art, Northwest A&F University, Yangling, Xianyang 712100, China
2
College of Forestry, Northwest A&F University, Yangling, Xianyang 712100, China
*
Authors to whom correspondence should be addressed.
Buildings 2023, 13(9), 2329; https://doi.org/10.3390/buildings13092329
Submission received: 3 August 2023 / Revised: 28 August 2023 / Accepted: 6 September 2023 / Published: 14 September 2023
(This article belongs to the Topic Bioclimatic Designs to Enhance Urban/Rural Resilience)

Abstract

:
In this study, typical open spaces were selected in the urban area of Lanzhou, China, with varying distances from the Yellow River and different plant configuration spaces. Then, the thermal perception of respondents was investigated through meteorological measurements, thermal comfort questionnaires, and parametric modeling. The findings indicate the following: (1) Wind speed decreases significantly as the distance from the Yellow River increases in the three open green spaces. (2) The cold lake effect of the Yellow River dominates the wind environment. (3) The closest site to the Yellow River exhibits the strongest correlation between wind speed and the respondents’ thermal sensation. (4) There is a strong positive correlation between the model output and different spatial measurement values. (5) There is a certain discrepancy between the UTCI values and the actual measurements, but the fit is high and consistent with an R-squared value of 0.936. This study quantitatively evaluated the thermal comfort and perception in typical spaces and validated the reliability of parameterized modeling for such spaces, providing a reference basis for thermal environment planning in these spaces.

1. Introduction

The global urbanization rate is rapidly increasing, and it is expected that by 2050, nearly 70% of the world’s population will reside in urban areas, according to data from the United Nations (2018). There has been growing concern about the negative environmental impacts of urban areas, with the impact of urban microclimate on public health already being documented; however, people’s attention to microclimate in river basin cities was low [1]. As the capital city of Gansu Province, Lanzhou is located in the upper reaches of the Yellow River and at the geometric center of China’s continental territory, and it is the only city through which the Yellow River flows. In addition, Lanzhou is a river valley city located along a river with a width of nearly 300 m, and it is sandwiched between mountain ranges on the north and south banks. The diurnal temperature difference causes air flow between the variations in elevation, resulting in a significant cold lake effect. This leads to higher wind speeds and lower humidity in the city. In recent years, the intensified winter winds and deteriorating living environment in the Lanzhou basin interact with the cold lake effect, resulting in a more adverse microclimate in the city, which is unpleasant for residents [2]. Vegetation is capable of attenuating the cold lake effect and the ridge heating effect, and thus, vegetation is an effective measure for improving microclimate.
Microclimate refers to a climate characterized by differences in heat and water budgets due to differences in the structure and properties of underlying surfaces, resulting in the formation of a climate with different characteristics from the macroclimate on a small scale. Microclimate conditions include factors such as temperature, precipitation, humidity, wind, and radiation [3]. Numerous studies have reported that vegetation is the primary climate modifier in urban areas [4,5,6,7]. Vegetation can reduce air temperature by providing shading and evapotranspiration, which helps to cool the urban environment [8]. Leaves and branches reduce the amount of solar radiation that reaches the area under the tree canopy or plants. Different locations and variations in tree conditions in terms of air temperature and relative humidity values [9], or the optimization of outdoor comfort conditions for different geometric layout configurations, can have different impacts on microclimate, and a well-organized planting layout can improve microclimate [10,11,12]. Furthermore, a reasonable layout within a green space can significantly decrease wind velocity, improve human comfort, and contribute to the microclimate, ultimately optimizing the living environment [2]. Urban open green spaces play a crucial role in providing thermal comfort and promoting the well-being of urban residents [13]. Therefore, it is necessary to optimize these spaces to improve thermal comfort, especially in cold climate regions, such as high-latitude areas.
Recent studies have demonstrated the potential of parametric optimization in improving thermal comfort in urban green spaces. Factors such as plant selection, layout design, and shading systems can all be optimized to enhance thermal comfort levels. This study contributes to this growing body of knowledge by investigating the effect of different design parameters on thermal comfort in a cold region of China [14]. The recognition of outdoor thermal comfort as a crucial performance indicator for urban-scale environmental assessment has been the focus of several studies that seek to develop effective methods, tools, and indicators to quantify it in various contexts and scales [15]. As part of a global research initiative to standardize the measurement and quantification of outdoor thermal comfort, the Universal Thermal Comfort Index (UTCI) was introduced as a metric [16]. In urban built-up areas, various studies have employed the urban canyon model as the geometrical setting, coupled with one of these thermal comfort indices, to evaluate the impact of various design variables on outdoor thermal comfort.
Software tools play a crucial role in the study of thermal comfort. Recently, the Ladybug Tools suite has emerged as a powerful tool for conducting an extensive parametric analysis of different design choices at a restricted scale [17]. Subsequently, the possibility of modeling outdoor comfort was explored through the integration of a set of tools embedded in the Grasshopper environment, which provides reliable results within reasonable computational time when defining an average urban canopy [10]. This study leverages Ladybug Tools, the plugins of Grasshopper3D, to optimize building height, street width, and orientation to maximize outdoor thermal comfort, which is represented by the diurnal average Universal Thermal Climate Index [18].
Currently, most studies in the field of urban climate focus on investigating the microclimate effects of plants and urban spatial structures under the context of the urban heat island effect during summer. However, a systematic investigation of the microclimate effects of plants with different spatial structures based on the cold lake effect during winter is lacking. In this study, the temperature was aimed to be investigated by the authors alongside humidity and wind speed in various plant configurations during autumn and winter. They analyzed the correlation between plants composition and microclimates under different spatial structures influenced by the cold lake effect. Moreover, the microclimate comfort of three different green open spaces at varying distances from the Yellow River during autumn and winter was assessed by the authors, and the reasons for the observed differences were analyzed. Furthermore, the authors recorded human behavior in different sites and summarized people’s preferences, providing insights into the design strategy of microclimate effects of open green spaces (OGSs) in Lanzhou. Finally, the Ladybug Tool was used by the authors to simulate the microclimate comfort in the study area, and fitting analysis was conducted on the measurement results to validate the accuracy of the model in similar temperate river valley cities like Lanzhou and verify the effectiveness of the transformation. In summary, the objectives of this study are to identify the most suitable green space structure under the cold lake effect from a human perspective and provide a comfortable microclimate environment to improve people’s living conditions.

2. Experimental Design

Lanzhou, as a river valley city in the northwest region of China, is characterized by low temperatures and strong winds. It is influenced by various factors such as terrain, geographical location, and monsoon [19]. These factors contribute to hot and windy summers, cold and dry winters, and a relatively low annual precipitation, resulting in an arid and cold climate in the city. According to meteorological data from Lanzhou for the period of 2001–2020 (CDCW, 2020), as shown in Table 1, the average annual temperature is mainly concentrated between 6 and 8 °C. The average annual relative humidity (RH) ranges from 55.0% to 61.0%. A field survey was conducted in a city park in Lanzhou, which is located at a longitude of 103°40′ E and latitude of 36°03′ N. The measured data for three sampling points are presented in Table 2. Among them, sampling point 1 is closest to the water, exhibiting a temperature difference of 10.7 °C between the maximum and minimum temperatures, with a relative humidity difference of 32.45. Meteorological parameters were measured on site, and the Ladybug Tools tool was utilized to calculate the Universal Thermal Climate Index (UTCI). Questionnaire surveys were conducted among visitors in these spaces to gather personal perception information and spatial perception intentions. The UEG (Urban Energy Game) tool was employed to predict spatial temperature and humidity changes on an hourly basis for one year. The Grasshopper tool was used to construct the spatial models, and the simulation and validation of thermal comfort environments were conducted using meteorological data and UWG (Urban Weather Generator) predictions for the three locations.

2.1. Study Site

Field investigations were conducted during the autumn (7 September and 8 December 2020) and winter (7 November and 7 December 2021) seasons, which corresponded to the coldest and driest periods in Lanzhou. The study areas were located in the Anning District of Lanzhou City, and various green open spaces at different distances from the Yellow River were selected for the investigation (Figure 1).

2.2. Meteorological Measurement

Meteorological parameters, namely globe temperature (Tg), air temperature (Ta), relative humidity (RH), and wind speed (Va), were recorded every minute (Table 3). Tg was recorded using a WGBT-302, while Ta was measured using an anemometer. RH measurements were obtained using a SIGMA AS837 device [11]. In addition, Vv and Va were measured using a SIGMA AR866A thermal hand-held high-precision digital air volume test and measurement anemometer [14].
The study was conducted during the autumn and winter seasons with experimental observations taking place between 13:30 and 12:00. Measurements of various indicators were taken every 10 min, and the experiment was repeated three times to ensure accuracy. The study encompassed three distinct locations, and specific measurements were obtained from various spaces within each location, including grassland (H), shrub–grass (SH), arbor–grass (AH), and arbor–shrub–grass (ASH) spaces. More detailed information regarding the specific locations and spaces can be found in Appendix A Figure A1, Figure A2 and Figure A3, Tables S1–S4 .
The mean radiant temperature (Tmrt) was calculated on site in terms of the black globe temperature (Tg) and the air temperature (Ta) following the formula:
Tmrt = ( Tg + 273 ) 4 + 1.1   ×   10 8   ×   v 0.6 ε g   ×   D 0.4 × Tg Ta 4 273
where (εg = 0.95) and (D = 0.05 m) are the globe emissivity and diameter, respectively.
The Universal Thermal Climate Index (UTCI) is a widely accepted parameter for measuring the thermal stress people experience when outdoors. The value of UTCI depends only on wind speed, average radiant temperature, relative humidity and actual air temperature. As calculating the UTCI equivalent temperatures by running the thermoregulation model repeatedly, calculations are performed via an extensive polynomial expression with 210 coefficients [16]. Calculations are performed via an extensive polynomial expression with 210 coefficients. The UTCI can also be calculated by the following simplified equation:
UTCI = 3.21 + (0.872 × Ta) + (0.2459 × Tmrt) − (2.5078 × Va) − (0.0176 × RH) (°C)

2.3. Questionnaire Surveys

Questionnaires were conducted simultaneously during the measurement of climatic factors such as wind speed (Appendix A). A total of 600 questionnaires were randomly distributed at 12:00 and 14:00 (±0.5 h) at the selected location with a total of 509 valid data. The survey questions were based on existing research and are set into three categories in this survey: the first was the personal information of each respondent, including age, gender, means of transportation and type of visitors (the thermal comfort questionnaire is an English translation from the original Chinese).
Part II of the questionnaire explored individual perceptions of different types of activities and thermal sensation, comfort and acceptability. Specifically, activity intensity preference was represented by a list of 5-level scales (low (1); lower (2); normal (3); higher (4); high (5)). Coming here for microclimate comfort was recorded on a 2-point scale (yes (0); no (1)). Specifically, thermal sensation was expressed by a list of 5-level scales (cold (1); cool (2); neutral (3); warm (4); hot (5)) (Appendix A).
Part III of the questionnaire surveyed strategies of microclimate and space improvement, including wind, humidity, sunshine, plant, architecture, waterscape and people. And it also explored people’s perceptions of the frequency of special weather (such as sandstorm, rainstorm, hail, extreme drought and extreme low temperature). Frequency was represented by a list of 5-level scales (many (1); more (2); general (3); less (4); few (5)). (Appendix A).

2.4. Presentation of the Simulation Workflow in Grasshopper

The initial step involved in this study was to procure a suitable weather dataset from available sources in “epw” format, which is widely compatible with a variety of simulation tools. And the authors selected the full year data for the study time based on the “.epw” format data. The Urban Weather Generator (UWG) is a tool utilized in this study, which is designed to estimate urban canopy air temperature and relative humidity on an hourly basis. To achieve this, it takes into consideration various factors such as heat exchange and air stratification in different atmospheres [20,21]. The parameters used in the study include Va, RH, Ta, Tg, Sunshine (Ss), and UTCI, which were obtained from a 3D model of the study area, which was constructed using Rhinoceros. These values were considered to be representative of the urban scale, and were easily incorporated into the workflow using the graphical interface provided by the Ladybug tool within the Grasshopper environment. This enabled seamless integration with other components of the proposed workflow.
In the final part, the Ladybug tool was employed to simulate the primary influence of wind elements on the environment. Approaches available in Grasshopper include wind analyses using Butterfly [11] or Eddy3D [14] which produce wind factors, the ratio between the simulated wind speeds and the inlet wind speed generated from a number of directions. In this study, Ladybug in Grasshopper was found to be faster, more accurate, and suitable for wind analysis. The workflow diagram for the development and testing of Ladybug is shown in Figure A1, highlighting the connections between different tools. The first step of the proposed simulation workflow was to create an appropriate geometric representation of the urban area under study.

3. Results

3.1. Deceptive Analysis

3.1.1. Measured Meteorological Parameter

Meteorological variables of 10 species of single arbor (A) and single shrub (S) measured during autumn and winter are listed in Appendix B. Va, Vv of A, S, Ta, Tg and RH all increased significantly. Based on onsite meteorological measurements and field surveys of plant communities, it has been observed that Cornus chinensis and Ligustrum lucidum are dominant tree species in the local area. Their robust branches and dense foliage contribute to their strong wind resistance, enabling them to effectively withstand strong winds [22]. Picea asperata exhibits the strongest thermal insulation due to its needle-like structure. Ilex rotunda, with its thicker wax-coated leaves, helps reduce water loss, resulting in its strong moisturizing ability.
Meteorological variables of the four planting patterns measured during autumn and winter are listed in Appendix A. The order of cooling ability of the four planting patterns was arbor and grass (AH) > arbor–shrub–grass (ASH) > shrub–grass (SH) > grass (H). The order of moisturizing ability of the four planting modes was AH > ASH > SH > H. It shows that the shrub has a certain humidification effect, but it is smaller than that of the arbor. The order of wind resistance of the four planting modes is ASH > AH > SH > H. Because of the wind-blocking ability of shrubs, AS and ASH had the strongest wind-blocking ability. H had the weakest wind-blocking effect, and the grass hardly affected the air flow at the pedestrian level. Through the analysis of dynamic Stream Chart and dynamic Ridgeline plots, the Va and Vv of the three OGSs increased significantly with the seasons, while the Ta, Tg and RH decreased significantly with the seasons. In the three OGS, RH, Va and Vv decreased significantly with the distance from the Yellow River, while Ta, Tg, MRT and UTCI increased significantly (Figure 2). Significant differences in meteorological variables among the three spaces and the four planting patterns were determined through post hoc Tukey tests (Figure 3). The Va near the Yellow River for two OGSs was significantly different in winter and autumn (p > 0.05). The RH of all three OGSs was significantly different in winter.

3.1.2. Respondent Attributes

A total of 509 effective questionnaires were collected, including 166 in OGS1, 148 in OGS2 and 195 in OGS3. Respondents were composed of 50.69% females and 49.31% males, 22.40% seniors (>55 years old), 67.78% adults (18–55 years old) and 9.82% children (<18 years old). In trials, the majority of respondents reported intensity perceptions for different activity types and perceptions of comfort in different spaces (Figure 4 and Figure 5). At the same time, the perception of Lanzhou’s special weather and suggestions for space renovation were also reported for respondents.
1. Effects of physical factors
Among physical factors, the effects of Ta, RH and Va on the thermal perception of the human body were considered [23]. In this study, all meteorological parameters influenced the thermal sensation of respondents. In OGS1, Va had the highest correlation with thermal sensation among respondents, followed by Ta and RH then G in order. In OGS2, Ta and RH had the highest correlation with thermal sensation among respondents, which was followed by Va and then G in order. In OGS3, Ta and RH had the highest correlation with thermal sensation among respondents, which was followed by Va and then G in order.
2. Effects of individual factors
Among individual factors, effects of age, gender, and activity level on the thermal perception of individuals were considered [22]. In this study, there were effects of individual factors on thermal microclimate comfort for respondents. In OGS3, the thermal comfort of microclimate for respondents was influenced by personal activities. The mode of transportation had a negative impact on perceptions of comfort.
3. Landscape elements
In this study, people’s perceptions of the comfort of small environments such as squares, trees, lawns, roads, watersides, buildings, etc. were interviewed by the authors (Figure 6). Discovered by analysis, the comfort of grass space for respondents is affected by the gender in OGS1. The comfort of the waterside is affected by activity. In OGS2, the comfort of grass space for respondents was affected by the Ta and RH. The comfort of architecture was affected by the gender. In OGS3, landscape elements did not have a statistically significant effect on respondents’ comfort level.

3.1.3. Va and RH Simulation in the Model

To validate the reliability of the Ladybug tool in calculating outdoor relative humidity and wind speed, probes were used to apply the same profiles of relative humidity and wind speed within self-built models. The simulated temperature and humidity results for the three spaces were obtained. Wind speed (Figure 7a) and relative humidity (Figure 7c) are simulated through three green space models. It can clearly be seen that although the parameters Va and RH have some discrepancies with the measured values, the fitting degree is high and there is consistency (Figure 7b,e). The results show that there is a strong positive correlation between different spatial measurements and model outputs Va and RH, R2 = 0.986 (Figure 7c), R2 = 0.984 (Figure 7f). It can clearly be seen that although the parameters Va and RH have some discrepancies with the measured values, the fitting degree is high and there is consistency. The results show that there is a strong positive correlation between different spatial measurements and model outputs Va and RH, R2 = 0.986, R2 = 0.984 (Figure 7a–d).

3.1.4. UTCI Simulation in the Model

It can be clearly seen that the parameter UTCI is in good agreement with the field measurements. The results show that the Ladybug Tools workflow simulates the thermal performance of the geometric configuration with considerable reliability and a short simulation time. Therefore, it can be used for the environmental simulation of the studied locations in this research. The simulation results represent the temperature variations for each hour of every day throughout the year for the three spaces. Although there is some discrepancy between the UTCI parameter and the measured values, there is a high level of fit and significant consistency with an R-squared value of 0.936 (Figure 8).

3.1.5. Implications for Designers

In Lanzhou, due to the cold lake effect of the Yellow River, the outdoor thermal perception of scenic open spaces was mainly influenced by wind. Therefore, it was a great opportunity to improve outdoor comfort by implementing an optimized design of landscape features. Through the joint verification of actual measurement and simulation, it was concluded that in order to cope with the low temperature and minimum precipitation in the autumn and winter seasons, tree species with strong insulation and moisture retention capabilities should be given priority consideration in the design. At the same time, the analysis revealed a negative correlation between activity levels and respondents’ thermal comfort, emphasizing the importance of providing comfortable activity spaces in design. In addition, our simulation results indicated that there was an important connection between an individual’s thermal adaptation ability and the spatial environment. These results were further elaborated in Table 4 and Figure 9. Research on the thermal comfort of grouped and single plants indicated the following microclimate comfort levels: ASH > AH > A and A > S > H (Figure 9a).

3.1.6. UTCI after Retrofit

In order to investigate the effects of snowstorm, wind volume, wind speed, temperature, relative humidity and solar radiation on the thermal comfort of small environments, three open green spaces models were established using Rhino (Figure 9). The results show that the Ladybug Tools workflow simulates the thermal performance of the geometric configuration with considerable reliability and a short simulation time; therefore, it can be used in this study. Three open green spaces (ASH) were transformed to simulate comfort after modeling. It was found that the UTCI values were higher than before the transformation (Figure 10). By utilizing the Ladybug tool, simulations were conducted for three open green spaces. Six different perspectives were captured within the software to calculate the Universal Thermal Climate Index (UTCI) for the developed models of these three open green spaces. The x-axis represents the months from January to December, while the y-axis represents the UTCI values. From the graph, it is evident that the red areas are predominantly concentrated in July and August, indicating that the optimal thermal comfort is mainly observed during these two months. Furthermore, the comfort levels among the three open green spaces are comparable, indicating that the renovation efforts can alleviate the heat island effect (Figure 11). In addition, the authors simulated the site sunshine through the model. According to Figure 12, the legend indicates the UTCI values, where colors closer to red represent higher UTCI values, while cooler colors indicate lower UTCI values. It was found that the Ss values of the three green spaces were not much different, which was consistent with our conjecture (Figure 12).

4. Discussion

4.1. Factors Affecting Thermal Comfort

Due to the prominent winter microclimate problems in northern China, Lanzhou is cold and long in winter and cools down quickly in autumn. The research is discussing the relationship between different plant configuration patterns and the local microclimate environment in open green spaces at different distances from the Yellow River, which is mainly for the analysis and research of the measured climatic conditions in autumn and winter.

4.1.1. Physical Factors

The present study evaluates the efficacy of different plant configurations in creating environmental comfort. Specifically, it is found by the authors that when a single plant type is employed, trees have the greatest potential to enhance thermal comfort conditions. On the other hand, composite structure types, such as arbor and grass combinations, exhibit the most significant impact on cooling and humidity. Furthermore, the combination of arbor, shrub and grass is found to be most effective in terms of average wind speed and wind-blocking ability in urban green spaces. Notably, our research supports the notion that dense tree coverage is conducive to mitigating heat stress, although vegetation may negatively affect wind ventilation [23,24]. Moreover, our study reveals that changes in relative humidity (RH) are inversely proportional to mean radiant temperature (MRT) and ambient temperature (Ta) during the winter solstice, which is the coldest season in Lanzhou. This finding is consistent with prior research that has shown that the cold lake effect of the Yellow River significantly influences wind conditions in the region during winter [25]. In addition, the authors observed that in OGS1, the thermal sensation of the respondents was most closely related to the air velocity (Va), indicating the significant impact of the UHI (cold lake effect) [26], which is a climatic phenomenon commonly observed in river valley cities at middle to high latitudes. Conversely, on OGS2–3, thermal sensation was most closely correlated with Ta and RH, followed by Va, suggesting that these meteorological factors play a crucial role in influencing thermal perception. Therefore, our results highlight the importance of considering strategies to manipulate Va during the design of outdoor spaces [27].

4.1.2. Individual Factors

The perception of thermal thresholds is influenced by various demographic factors, such as age, gender, and test site [28,29]. However, the present study did not identify any significant effects of individual factors (age and gender) on the thermal microclimate comfort of the respondents. Nevertheless, there were discernible differences in comfort levels across the various test sites. The thermal comfort of respondents in OGS1–2 was not associated with individual factors. However, in OGS3, the thermal microclimate comfort of respondents was found to be influenced by their activity levels. Specifically, the respondents’ mode of transportation to the test site was observed to negatively impact their perception of comfort. This could be attributed to the location of OGS3 on the outskirts of the city, far from the Yellow River, which required respondents to undertake a high level of activity to reach the test site [30].

4.1.3. Environment Factors

The impact of high-rise buildings on microclimate has been well documented in the literature [30]. In the present study, gender was found to influence architectural comfort in OGS1, which is consistent with the fact that this site has the highest number of high-rise buildings among the three test sites. Microclimate perception within the enclosed space of high-rise buildings was found to be inconsistent. A study conducted in Changsha, China, investigated the microclimate of two public squares and explored the effects of buildings, trees, water, and landscape design on improving thermal comfort [31,32]. Within our study, significant differences in respondents’ perception of comfort in grass spaces were observed within OGS2. In OGS1, thermal and humidity factors (Ta and RH) were found to influence comfort in grass spaces. However, the dry and cold climate during autumn and winter may not provide adequate improvement in environmental temperature and humidity within the open grassland spaces [33].

4.2. Microclimate Simulation Parameters

The ladybug tool model was chosen for this study to simulate micro environmental climates for several reasons: it is considerably less time consuming to perform calculations, allowing for the simulation of climatic factors for various plant configurations, including RH, Ta, Tg, Va, Sunshine and UTCI, which are focus on this study, and the ability of parameterization model various spatial shapes, and visualize the results in the Grasshopper environment.
The Ladybug Tools model was selected to simulate micro-environmental climates for several reasons. Firstly, it allows for the simulation of climatic factors for various plant configurations, including relative humidity (RH), air temperature (Ta), globe temperature (Tg), wind velocity (Va), sunshine, and Universal Thermal Climate Index (UTCI), which are the focus of this study. Secondly, the Ladybug Tools model considerably reduces the time required to perform calculations. Thirdly, it enables the parameterization of various spatial shapes and visualization of the results in the Grasshopper environment.
The Ladybug Tools model is a combination of Grasshopper plugins that estimate outdoor thermal comfort through graphical representation. The model connects Grasshopper to proven software engines that individually calculate thermal comfort determinants. For instance, Honeybee links Grasshopper with EnergyPlus [34] to calculate surface temperatures, while Dragonfly uses the Urban Weather Generator (UWG) [19] to calculate urban air temperature and relative humidity. In this study, Lanzhou city’s weather data in “epw” format was used, and the Ladybug component was used to visualize environmental data and output results. The simulations of Tg, Ta, and RH were compared with measured results, which demonstrated strong correlations of R2 = 0.996, R2 = 0.997, and R2 = 0.984, respectively. Although the Butterfly plugin could integrate Open FOAM software (OpenFOAM 9) for computational fluid dynamics (CFD) air-flow analysis, it requires significant computation time. Therefore, the wind speeds in this study were retrieved from weather files, which still demonstrated a strong correlation of R2 = 0.986.
The present study employs a rigorously validated software engine to determine the mean radiant temperature (MRT) and thermal comfort components. In this study, weather data for Lanzhou city in “epw” format was used, and the Ladybug component was employed to visualize the environmental data and output results. The simulation results of Tg, Ta, and RH were compared with the measured values, showing strong correlations with R-squared values of 0.996, 0.997, and 0.984, respectively. The Urban Weather Generator (UWG) has been validated through field measurements in diverse climates [19,20] and is utilized to investigate how different UTCI components are combined and how the MRT equations are applied, both of which require validation. In a Mediterranean climate context, Evola et al. validated the Ladybug Tools workflow through experimental measurements of MRT in Catania, Italy [35]. Their study reported a coefficient of determination R2 = 0.92 in good agreement with measurements. Additionally, the present study rigorously validates the workflow implemented in Ladybug Tools modeling. As shown in Figure 2, the average UTCI results for all three open green spaces exhibit consistent performance with an R2 of 0.936. This indicates that the proposed method exhibits good reliability in scenarios with the cold lake effect in middle to high-latitude regions. In similar environmental settings, this simulation can be applied in the early design process to model and assess alternative schemes, aiming to find space design solutions that offer improved thermal comfort while fulfilling other functional requirements. Subsequently, the design can be further refined and implemented during construction.

4.3. Retrofit Strategy

In this paper, through the actual measurement and simulation verification of different vegetation configurations in different open green spaces at different distances from the Yellow River, the design strategy with the best environmental comfort is found. The methodology described in this paper can be replicated and used to test other performance criteria, such as energy loads, through its core simulation engine, EnergyPlus [36]. Grasshopper is very friendly to planners, designers and others without proficiency in programming. There is no doubt that the use of open source plugins and environment plugins in Grasshopper has increased its popularity in climate research and has quickly become an indispensable tool in practice [37]. The method described in this article can be replicated and used to test other performance standards, such as energy load, by utilizing its core simulation engine, EnergyPlus [38].
A comprehensive approach was taken to evaluate the impact of different vegetation configurations on environmental comfort in various open green spaces situated at varying distances from the Yellow River. The methodology outlined in this research can be replicated and extended to examine other performance criteria, such as energy loads, through its core simulation engine, EnergyPlus. Grasshopper, with its open source and environmental plugins, has emerged as a popular and user-friendly tool for planners, designers and researchers without expertise in programming [18]. Our study establishes a close correlation between the Tg, Ta, Vv and RH measurements and simulation results. A visual tool, the “UTCI Rose”, was developed by the authors to analyze people’s perceptions of the comfort of small environments and guide urban designers in creating comfortable outdoor environments. The UTCI values reported in our study provide a direct measure of pedestrian thermal comfort in degrees Celsius, thereby facilitating the incorporation of climate indicators into design guidelines at different scales from districts to small urban areas. The methodology outlined in this study has the potential to contribute to the creation of resilient and sustainable urban environments that ensure pedestrian comfort.

4.4. Limitations

The wind and humidity analysis was performed based on the wind speed and relative humidity in the file, as these variables exhibited high reliability in the workflow. While other methods such as wind analysis using Butterfly or Eddy3D [15] are available in Grasshopper and generate wind factors that simulate wind speed in many directions, they are not as accurate as accounting for turbulent heat exchange in the model, which is a feature in the Open FOAM software currently under development and not yet integrated into either of the two plugins. Additionally, the Ladybug Tools model was found to underestimate the UTCI by approximately 3.5 °C compared to the field measurements, which was mainly due to spatial resolution issues in the plant simulation model that may lead to inaccurate sun occlusion angles. Despite these differences, they remain consistent under hypothetical cases and are thus acceptable. However, the model requires further refinement for detailed analysis.

5. Conclusions

In this study, a comparison of respondents’ perceptions of the thermal environment was conducted in three different types of sites in Lanzhou, China, utilizing different plant configuration spaces. Through the use of meteorological measurements and questionnaires, the physical, personal, and environmental factors that influence the thermal perception of residents and tourists were systematically discussed and compared. The study drew some major conclusions:
(1)
The cooling ability of the four planting patterns was ranked in order of arbor and grass (AH) > arbor–shrub–grass (ASH) > shrub–grass (SH) > grass (H), while the moisturizing ability was ranked in order of AH > ASH > SH > H, and the wind resistance was ranked in order of ASH > AH > SH > H. The values of air velocity (Va) and vertical air velocity (Vv) increased significantly with seasons in the three spaces, whereas air temperature (Ta), ground surface temperature (Tg), and relative humidity (RH) changed significantly with seasons in the three spaces. Secondly, the change of RH was found to be inversely proportional to the solar radiation (SR) and mean radiant temperature (MRT), and the RH during winter solstice was the smallest in autumn and winter.
(2)
The cold lake effect of the Yellow River dominates the wind environment in Lanzhou, and the wind speed in winter is high. In OGS1, Va had the highest correlation with respondents’ thermal sensation. The residential area is closest to the Yellow River, indicating that the cold lake effect of the Yellow River does cause strong winds in the environment, which has a certain impact on comfort. In OGS2–3, Ta and RH had the highest correlations with thermal sensation among respondents, which were followed by Va and G.
(3)
The present study highlights the influence of individual factors on respondents’ thermal microclimate comfort with notable variations across different sites. Specifically, in OGS2, respondents exhibit significantly diverse perceptions of the comfort of grassy spaces on the campus. In OGS1, gender affects the comfort of buildings, whereas the comfort of grass space is influenced by Ta and RH. Conversely, individual activities have a significant impact on respondents’ thermal comfort in OGS3.
(4)
Despite certain discrepancies between the measured values and UTCI parameters, the high degree of consistency and good fitting degree, R2 = 0.936, indicate that the parameters Tg, Ta, Va, and RH exhibit good agreement with the field measurements, with R2 values of 0.996, 0.997, 0.986, and 0.984, respectively.
The findings of this study provide insight into the mechanism underlying respondents’ thermal perception of the cold lake effect associated with the Yellow River. Furthermore, the site and actual measurement were simulated by the authors using Ladybug Tools, and the renovation plan was verified to achieve people’s thermal comfort. The implications of our results and methodology are expected to provide theoretical guidance for urban planners to consider climate-responsive design principles such as vegetation, irrigation, and shading to enhance outdoor comfort for visitors. The high level of fit between the simulated and measured data also indicates the reliability of this method in similar environments. It can be used as a reference in the early stages of design to assess and optimize the thermal comfort of spaces.

Supplementary Materials

The following supporting information can be downloaded at: https://www.mdpi.com/article/10.3390/buildings13092329/s1. Table S1. Volunteers’ attributes. Table S2. Open green space 1. Table S3. Open green space 2. Table S4. Open green space 3.

Author Contributions

Conceptualization, J.L. and S.J.; methodology, J.L.; software, S.J.; validation, S.Z. and S.Y.; formal analysis, S.Z.; investigation, W.J.; resources, W.J.; data curation, J.L.; writing—original draft preparation, J.L.; writing—review and editing, J.L. and S.J.; visualization, S.J.; supervision, W.L.; project administration, W.J.; funding acquisition, W.J. and W.L. All authors have read and agreed to the published version of the manuscript.

Funding

This research was funded by the Ministry of Science and Technology of China (2019FY101604).

Data Availability Statement

The data presented in this study are available on request from the corresponding author.

Conflicts of Interest

The authors declare no conflict of interest.

Appendix A

Thermal comfort questionnaire (English translation from the original Chinese).
1.
Location: ______ Time: ______ Length of time living locally: ______ Hometown: ______ Current wind speed: ____________ Current temperature/humidity: ____________
Current sunshine: ____________ (1, 2, 3 and 4, four levels are enhanced in turn)
2.
Gender: _________ Age: _________ Occupation: _________
3.
Means of Transportation: ( ) A. Self-driving B. Bus C. Subway D. Taxi E. Shared bike F. Walking
4.
Activity type and perceived intensity
LowLowerNormalHigherHigh
Sitting
Standing
Slow walking
Fast walking
Ball sports
5.
Did you come to the venue because of the comfortable climate? ○ Yes ○ No
6.
Evaluation of microclimate comfort in different space types
ColdCoolNeutralWarmHot
Square
Woodland
Lawn
Road
Waterside
Architecture
7.
Do you feel that the special weather (such as sandstorm, rainstorm, hail, extreme drought and extreme low temperature) in your place is frequent in the current season?
○ many ○ more ○ general ○ less ○ few
8.
Your preference for microclimate improvement (four groups, one from each group, four in total, and only four)
□ more wind □ less wind □ wet □ dry □ sunshine □ shadow □ more people □ fewer people
9.
Your preference for space improvement
□ increase trees □ reduce trees □ increase flowers □ reduce flowers □ increase pavilions or corridors □ increase waterscape □ reduce waterscape □ increase sprinkler
Figure A1. Open green space 1.
Figure A1. Open green space 1.
Buildings 13 02329 g0a1
Figure A2. Open green space 2.
Figure A2. Open green space 2.
Buildings 13 02329 g0a2
Figure A3. Open green space 3.
Figure A3. Open green space 3.
Buildings 13 02329 g0a3

Appendix B

Table A1. Meteorological variables in each measured space (Open green space 1).
Table A1. Meteorological variables in each measured space (Open green space 1).
Autumn (White Dew, 09,07)Autumn (Cold Dew, 10,08)Winter (Beginning of Winter, 11,07)Winter (Winter Solstice, 12,07)
Va (m/s)Juniperus formosana0.20 ± 0.006 Cd0.29 ± 0.006 Bbc0.34 ± 0.186 Bcd0.46 ± 0.009 Ae
Buxus megistophylla0.21 ± 0.006 Bd0.24 ± 0.23 ABc0.27 ± 0.067 ABd0.32 ± 0.009 Af
Cedrus deodara0.54 ± 0.012 Ca0.60 ± 0.012 BCa0.64 ± 0.012 Ba0.77 ± 0.153 Aa
Firmiana simplex0.39 ± 0.013 Bb0.58 ± 0.006 Aa0.60 ± 0.029 Aa0.68 ± 0.003 Ab
Picea asperata0.18 ± 0.006 Cc0.55 ± 0.006 Ba0.67 ± 0.021 Aa0.73 ± 0.007 Aab
Styphnolobium japonicum ‘Pendula’0.14 ± 0.009 Dde0.29 ± 0.012 Cbc0.44 ± 0.021 Bb0.54 ± 0.003 Ad
Juniperus chinensis0.18 ± 0.003 Ce0.27 ± 0.006 Bc0.31 ± 0.012 Bcd0.43 ± 0.012 Ae
Betula platyphylla0.16 ± 0.012 Dde0.29 ± 0.006 Cbc0.40 ± 0.009 Bbc0.4 ± 0.007 Ae
Pinus bungeana0.18 ± 0.003 Dde0.35 ± 0.006 Cb0.47 ± 0.006 Bb0.60 ± 0.003 Bc
Prunus cerasifera f. atropurpurea0.24 ± 0.022 Ce0.23 ± 0.026 Ccde0.32 ± 0.015 Bcd0.46 ± 0.003 Ae
Tg
(°C)
Juniperus formosana6.68 ± 0.058 Bg9.47 ± 0.035 Ae5.68 ± 0.058 Cc3.03 ± 0.037 Df
Buxus megistophylla7.68 ± 0.115 Af6.97 ± 0.059 Bf6.68 ± 0.115 Bbc3.75 ± 0.100 Ce
Cedrus deodara9.88 ± 0.115 ABe10.37 ± 0.344 Ade8.54 ± 0.240 Bab4.72 ± 0.039 Cbc
Firmiana simplex11.62 ± 0.115 Ad11.57 ± 0.079 Bcd9.29 ± 0.240 Ca4.92 ± 0.039 Dab
Picea asperata14.82 ± 0.231 ABab15.56 ± 0.510 Aa10.59 ± 0.489 Ba5.16 ± 0.023 Ca
Styphnolobium japonicum ‘Pendula’15.68 ± 0.058 Aa15.50 ± 0.137 Aa9.67 ± 0.947 Ba4.55 ± 0.029 Cc
Juniperus chinensis13.51 ± 0.058 Ac13.02 ± 0.203 Ab10.18 ± 0.285 Ba4.14 ± 0.031 Cdc
Betula platyphylla14.09 ± 0.379 Ab12.15 ± 0.082 Abc9.14 ± 0.603 Bab3.55 ± 0.068 Ce
Pinus bungeana11.25 ± 0.058 Ad11.10 ± 0.029 Acd8.57 ± 0.368 Bab4.07 ± 0.033 Cd
Prunus cerasifera f. atropurpurea11.60 ± 0.173 Ad11.86 ± 0.449 Ac10.08 ± 0.139 Ba3.82 ± 0.093 Cde
Ta
(°C)
Juniperus formosana5.29 ± 0.035 Ah4.51 ± 0.067 Bf3.15 ± 0.29 Cde1.00 ± 0.115 Dc
Buxus megistophylla6.41 ± 0.234 Ag5.93 ± 0.077 Af3.44 ± 0.04 Bde1.6 ± 0.305 Cbc
Cedrus deodara9.69 ± 0.058 Af9.44 ± 0.172 Ad4.79 ± 0.105 Bbc2.23 ± 0.120 Cab
Firmiana simplex13.78 ± 0.058 Ac13.22 ± 0.563 Ab5.89 ± 0.064 Ba2.45 ± 0.029 Ca
Picea asperata14.73 ± 0.115 Ab15.09 ± 0.266 Aa5.48 ± 0.290 Bab2.53 ± 0.176 Ca
Styphnolobium japonicum ‘Pendula’17.78 ± 0.115 Aa16.35 ± 0.448 Aa5.11 ± 0.437 Babc2.15 ± 0.755 Cab
Juniperus chinensis14.08 ± 0.310 Abc13.17 ± 0.138 Ab4.81 ± 0.064 Bbc1.93 ± 0.064 aCb
Betula platyphylla12.65 ± 0.006 Ad11.53 ± 0.120 Bc4.33 ± 0.088 Ccd1.83 ± 0.035 Dab
Pinus bungeana10.72 ± 0.115 Ae10.22 ± 0.173 Acd4.19 ± 0.034 Bcd1.45 ± 0.074 Cbc
Prunus cerasifera f. atropurpurea11.23 ± 0.115 Ae10.74 ± 0.278 Acd4.17 ± 0.037 Bcd1.86 ± 0.094 Cbc
RH (%)Juniperus formosana60.84 ± 0.462 Aa59.28 ± 0.577 Aa54.85 ± 0.356 Ba47.33 ± 0.362 Cab
Buxus megistophylla54.28 ± 1.707 ABc57.35 ± 1.468 Aa48.35 ± 0.233 BCc43.57 ± 0.513 Cc
Cedrus deodara49.49 ± 0.450 Ad45.49 ± 0.577 ABb42.49 ± 1.154 Bde35.57 ± 0.384 Ce
Firmiana simplex37.06 ± 0.766 Af36.3 ± 0.058 Ac34.07 ± 0.521 ABf31.83 ± 0.273 Bf
Picea asperata35.81 ± 0.181 Af37.47 ± 0.231 Ac32.90 ± 0.385 Bf31.08 ± 0.586 Bf
Styphnolobium japonicum ‘Pendula’38.53 ± 0.312 Af33.21 ± 0.008 Bc29.88 ± 0.252 Cg27.96 ± 0.281 Dg
Juniperus chinensis45.38 ± 0.347 Ae45.03 ± 0.017 Ab40.36 ± 0.384 Be35.99 ± 0.564 Ce
Betula platyphylla53.28 ± 0.398 Acd50.53 ± 0.058 Ab44.36 ± 0.285 Bd39.15 ± 0.596 Cd
Pinus bungeana69.94 ± 0.436 Aa62.57 ± 0.231 Ba51.19 ± 0.748 Cbc45.70 ± 0.439 Dbc
Prunus cerasifera f. atropurpurea59.57 ± 0.637 Ab62.31 ± 3.535 Ab53.76 ± 0.286 Aab49.76 ± 0.694 Aa
Vv
(cmm)
Juniperus formosana13.47 ± 0.049 Ce21.74 ± 0.577 Bc26.13 ± 0.196 Ac28.04 ± 0.294 Ade
Buxus megistophylla16.45 ± 0.654 Bd17.83 ± 0.058 Be19.16 ± 0.338 ABd20.66 ± 0.172 Af
Cedrus deodara39.93 ± 0.126 Ca42.11 ± 0.577 BCa44.11 ± 0.577 Ba47.72 ± 0.434 Aa
Firmiana simplex26.66 ± 0.234 Cb40.93 ± 0.231 Ba42.11 ± 0.485 ABa44.42 ± 0.354 Ab
Picea asperata21.25 ± 0.598 Cc40.46 ± 0.231 Ba43.41 ± 0.516 ABa45.4 ± 0.468 Aab
Styphnolobium japonicum ‘Pendula’14.32 ± 0.244 Ce21.16 ± 0.577 Bcd25.07 ± 0.093 Ac27.59 ± 0.581 Ade
Juniperus chinensis10.28 ± 0.124 Cfe18.89 ± 0.346 Bde24.22 ± 0.647 Ac26.02 ± 0.690 Ae
Betula platyphylla10.43 ± 0.86 Cf20.67 ± 0.577 Bcd26.67 ± 0.577 Ac30.07 ± 0.636 Ac
Pinus bungeana11.00 ± 0.299 Df24.97 ± 0.520 Cb29.30 ± 0.383 Bb33.25 ± 0.653 Ad
Prunus cerasifera f. atropurpurea13.86 ± 0.200 De16.26 ± 0.115 Bf10.14 ± 0.130 Bd25.29 ± 0.420 Ae
Notes: Values are performed as mean values ± standard errors. The different normal letters in the same column indicate significant differences among treatments at the 0.001 level, while the different capital letters in the same row indicate significant differences among stages at the 0.001 level. The same is shown below.
Table A2. Meteorological variables in each measured space (Open green space 2).
Table A2. Meteorological variables in each measured space (Open green space 2).
Autumn (White Dew, 09,07)Autumn (Cold Dew, 10,08)Winter (Beginning of Winter, 11,07)Winter (Winter Solstice, 12,07)
Va (m/s)Berberis thunbergii ‘Atropurpurea’0.44 ± 0.009 Cd0.55 ± 0.009 Be0.60 ± 0.009 Be0.78 ± 0.012 Ae
Ligustrum lucidum0.25 ± 0.003 Df0.31 ± 0.003 Cg0.43 ± 0.003 Bf0.53 ± 0.009 Ag
Cornus alba0.29 ± 0.003 Df0.36 ± 0.003 Cfg0.47 ± 0.003 Bf0.67 ± 0.009 Af
Syringa oblata0.92 ± 0.012 Ca1.15 ± 0.070 BCa1.31 ± 0.006 Ba1.58 ± 0.009 Aa
Forsythia suspense0.50 ± 0.009 Dc0.760 ± 0.006 Cd0.87 ± 0.003 Bd0.94 ± 0.009 Ad
Lonicera maackii0.38 ± 0.012 De0.80 ± 0.012 Ccd0.92 ± 0.009 Bc1.20 ± 0.026 Ac
Prunus triloba0.40 ± 0.009 Dde0.96 ± 0.034 Cb1.21 ± 0.009 Bb1.55 ± 0.029 Aa
Lonicera japonica0.38 ± 0.009 Ce0.50 ± 0.009 Bef0.58 ± 0.019 ABe0.6 ± 0.003 Ag
Rosa xanthina0.27 ± 0.009 Df0.34 ± 0.006 Cg0.36 ± 0.011 Bg0.38 ± 0.012 Ah
Buxus sinica var. parvifolia0.60 ± 0.012 Db0.92 ± 0.012 Cbc1.24 ± 0.003 Bb1.44 ± 0.027 Ab
Tg
(°C)
Berberis thunbergii ‘Atropurpurea’11.08 ± 0.319 Ad9.74 ± 0.142 Bf7.93 ± 0.045 Ce4.23 ± 0.105 Df
Ligustrum lucidum14.20 ± 0.220 Ac12.56 ± 0.280 Be10.31 ± 0.048 Cbc7.28 ± 0.085 Dd
Cornus alba14.75 ± 0.313 Abc13.17 ± 0.263 ABde11.70 ± 0.2482 Bab8.19 ± 0.195 Cbcd
Syringa oblata15.81 ± 0.217 Aabc14.72 ± 0.172 Aabc12.37 ± 0.186 Ba9.84 ± 0.199 Ca
Forsythia suspense14.01 ± 0.194 Ac13.28 ± 0.283 Ade11.48 ± 0.260 Bab8.91 ± 0.067 Cb
Lonicera maackii15.50 ± 0.430 Aabc13.80 ± 0.104 Acde10.61 ± 0.207 Bbc8.34 ± 0.175 Cbc
Prunus triloba16.78 ± 0.296 Aab15.14 ± 0.227 Aabc9.97 ± 0.289 Bcd7.92 ± 0.192 Ccd
Lonicera japonica16.15 ± 0.090 Aa15.96 ± 0.166 Aa11.25 ± 0.132 Bab7.38 ± 0.204 Ccd
Rosa xanthina14.11 ± 0.379 Ac14.17 ± 0.361 Abc8.93 ± 0.185 Bde6.09 ± 0.152 Ce
Buxus sinica var. parvifolia16.27 ± 0.506 Aab15.37 ± 0.179 Aab12.41 ± 0.226 Ba8.18 ± 0.193 Cbcd
Ta
(°C)
Berberis thunbergii ‘Atropurpurea’9.32 ± 0.291 Af8.52 ± 0.271 fAB7.10 ± 0.381 Be2.64 ± 0.225 Ce
Ligustrum lucidum12.81 ± 0.208 Ae11.15 ± 0.173 Be9.41 ± 0.031 Cbc4.4 ± 0.144 Dcd
Cornus alba13.16 ± 0.148 Ae12.24 ± 0.242 Ade10.16 ± 0.212 Bab5.14 ± 0.081 Cb
Syringa oblata14.28 ± 0.147 Ade11.96 ± 0.205 Bde11.07 ± 0.204 Ba6.43 ± 0.278 Ca
Forsythia suspense14.72 ± 0.280 Acd13.77 ± 0.283 Abc10.03 ± 0.107 Babc5.65 ± 0.124 Cab
Lonicera maackii13.94 ± 0.327 Ade12.57 ± 0.259 Acd8.16 ± 0.114 Bd4.06 ± 0.035 Ccd
Prunus triloba17.92 ± 0.290 Aa15.34 ± 0.189 Ba9.02 ± 0.194 Ccd3.20 ± 0.190 De
Lonicera japonica16.83 ± 0.334 Aab15.36 ± 0.079 Ba9.87 ± 0.046 Cbc4.66 ± 0.087 Dbcd
Rosa xanthina13.32 ± 0.132 Ade12.47 ± 0.241 Ad6.78 ± 0.156 Be3.07 ± 0.060 Ce
Buxus sinica var. parvifolia15.83 ± 0.311 Abc14.2 ± 0.248 Bab8.28 ± 0.142 Cd4.29 ± 0.032 Dcd
RH (%)Berberis thunbergii ‘Atropurpurea’38.58 ± 0.362 Ad37.11 ± 0.497 Ad33.91 ± 0.233 Bcd30.27 ± 0.402 Ce
Ligustrum lucidum54.69 ± 0.347 Ab50.68 ± 0.320 Bb47.79 ± 0.406 Cb45.38 ± 0.504 Cb
Cornus alba53.87 ± 0.473 Abc49.35 ± 0.621 Bbc47.17 ± 0.315 BCb45.52 ± 0.457 Cb
Syringa oblata80.18 ± 0.434 Aa76.52 ± 0.305 Ba71.00 ± 0.197 Ca62.73 ± 0.095 Da
Forsythia suspense37.97 ± 0.266 Ade35.09 ± 0.199 Bde31.91 ± 0.282 Cef29.93 ± 0.131 De
Lonicera maackii38.74 ± 0.311 Ad36.70 ± 0.345 Bde34.91 ± 0.278 BCc33.04 ± 0.038 Cd
Prunus triloba33.58 ± 0.600 Af29.76 ± 0.187 Bf31.21 ± 0.116 BCf28.03 ± 0.148 Cf
Lonicera japonica38.23 ± 0.257 Ade35.65 ± 0.618 ABde34.27 ± 0.168 Bcd30.72 ± 0.458 Ce
Rosa xanthina51.34 ± 0.587 Ac47.75 ± 0.273 Bc47.99 ± 0.245 Bb42.76 ± 0.123 Cc
Buxus sinica var. parvifolia35.97 ± 0.407 Ae34.63 ± 0.486 ABe32.82 ± 0.289 Bde28.18 ± 0.162 Cf
Vv
(cmm)
Berberis thunbergii ‘Atropurpurea’52.63 ± 0.315 Da57.65 ± 0.415 Cd61.15 ± 0.436 Bd67.22 ± 0.503 Ac
Ligustrum lucidum32.82 ± 0.356 Dde35.73 ± 0.499 Cf38.78 ± 0.411 Bg49.07 ± 0.249 Ae
Cornus alba34.11 ± 0.312 Dd39.23 ± 0.422 Cf42.81 ± 0.217 Bf53.75 ± 0.289 Ad
Syringa oblata22.37 ± 0.606 Dg30.43 ± 0.396 Ch38.60 ± 0.234 Bg45.49 ± 0.557 Af
Forsythia suspense39.12 ± 0.778 Dc55.43 ± 0.674 Cd62.12 ± 0.334 Bd68.08 ± 0.394 Ac
Lonicera maackii27.50 ± 0.471 Df61.50 ± 0.712 Cb64.85 ± 0.331 Bc72.16 ± 0.105 Ab
Prunus triloba26.82 ± 0.301 Cf70.88 ± 1.075 Ba75.01 ± 0.133 ABa77.46 ± 0.291 Aa
Lonicera japonica30.36 ± 0.700 De42.88 ± 0.418 Ce46.11 ± 0.105 Be50.56 ± 0.296 Ae
Rosa xanthina20.98 ± 0.267 Db24.41 ± 0.655 Ci27.46 ± 0.275 Bh34.05 ± 0.226 Ag
Buxus sinica var. parvifolia42.07 ± 0.410 Dg66.58 ± 0.754 Cb71.70 ± 0.158 Bbd75.97 ± 0.163 Aa
Notes: Values are performed as mean values ± standard errors. The different normal letters in the same column indicate significant differences among treatments at the 0.001 level, while the different capital letters in the same row indicate significant differences among stages at the 0.001 level.
Table A3. Meteorological variables in each measured space (Open green space 3).
Table A3. Meteorological variables in each measured space (Open green space 3).
Autumn (White Dew, 09,07)Autumn (Cold Dew, 10,08)Winter (Beginning of Winter, 11,07)Winter (Winter Solstice, 11,07)
OGS1OGS2OGS3OGS1OGS2OGS3OGS1OGS2OGS3OGS1OGS2OGS3
Va (m/s)H0.45 ± 0.003 d0.44 ± 0.003 d0.41 ± 0.009 d0.61 ± 0.009 c0.58 ± 0.006 c0.51 ± 0.009 c0.76 ± 0.006 b0.68 ± 0.012 b0.60 ± 0.138 b0.82 ± 0.009 a0.78 ± 0.003 a0.76 ± 0.012 a
SH0.43 ± 0.010 d0.41 ± 0.06 d0.35 ± 0.003 d0.59 ± 0.153 c0.56 ± 0.06 c0.50 ± 0.009 c0.71 ± 0.011 b0.69 ± 0.06 b0.66 ± 0.003 b0.77 ± 0.010 a0.74 ± 0.0.09 a0.71 ± 0.007 a
AH0.40 ± 0.003 d0.37 ± 0.006 d0.31 ± 0.009 d0.50 ± 0.009 c0.47 ± 0.010 c0.45 ± 0.006 c0.62 ± 0.011 b0.61 ± 0.019 b0.58 ± 0.009 b0.70 ± 0.009 a0.68 ± 0.006 a0.66 ± 0.006 a
ASH0.36 ± 0.003 d0.34 ± 0.003 d0.23 ± 0.007 c0.41 ± 0.003 c0.38 ± 0.006 c0.39 ± 0.006 b0.54 ± 0.007 b0.53 ± 0.003 b0.53 ± 0.009 a0.66 ± 0.003 a0.57 ± 0.003 a0.57 ± 0.007 a
Tg
(°C)
H9.24 ± 0.118 a8.39 ± 0.203 a8.08 ± 0.040 a7.43 ± 0.082 b7.36 ± 0.197 a7.23 ± 0.145 b5.37 ± 0.116 b5.20 ± 0.145 c5.13 ± 0.064 c4.03 ± 0.088 d4.03 ± 0.058 c3.70 ± 0.058 d
SH11.40 ± 0.529 a10.50 ± 0.265 a10.13 ± 0.188 a9.83 ± 0.764 a8.77 ± 0.145 b8.45 ± 0.232 b7.43 ± 0.404 b7.43 ± 0.404 b7.15 ± 0.736 c5.73 ± 0.246 c4.93 ± 0.115 c4.80 ± 0.058 d
AH13.97 ± 0.058 a13.33 ± 0.203 a12.40 ± 0.36 a12.40 ± 0.208 a11.43 ± 0.379 b9.69 ± 0.64 b8.97 ± 0.162 c8.57 ± 0.296 b8.15 ± 0.101 c7.41 ± 0.059 c6.35 ± 0.174 c6.08 ± 0.231 d
ASH11.43 ± 0.047 a11.28 ± 0.017 d11.20 ± 0.103 a10.31 ± 0.112 b10.17 ± 0.089 a10.07 ± 0.033 c9.54 ± 0.123 b8.35 ± 0.029 b8.28 ± 0.041 b8.17 ± 0.112 c5.11 ± 0.070 a4.60 ± 0.750 c
Ta
(°C)
H7.45 ± 0.247 a7.32 ± 0.072 a7.06 ± 0.067 a5.94 ± 0.068 b5.74 ± 0.029 b5.11 ± 0.067 b3.35 ± 0.084 c2.15 ± 0.077 c2.03 ± 0.033 c2.06 ± 0.173 d1.76 ± 0.031 c1.55 ± 0.029 d
SH8.4 ± 0.100 a8.38 ± 0.044 a8.10 ± 0.100 a7.03 ± 0.033 b6.45 ± 0.234 b5.93 ± 0.120 b4.39 ± 0.194 c4.03 ± 0.088 c3.97 ± 0.148 c3.18 ± 0.356 c2.10 ± 0.058 d1.90 ± 0.058 d
AH12.10 ± 0.208 a11.60 ± 0.400 a10.50 ± 0.289 a9.73 ± 0.371 b9.19 ± 0.335 b7.60 ± 0.306 b5.23 ± 0.186 c5.07 ± 0.067 c4.90 ± 0.100 c4.47 ± 0.72 c4.17 ± 0.120 c4.07 ± 0.115 c
ASH11.60 ± 0.400 a9.92 ± 0.043 a8.33 ± 0.067 a9.15 ± 0.074 b8.50 ± 0.055 a8.48 ± 0.018 a6.82 ± 0.064 b5.78 ± 0.056 b4.58 ± 0.100 c5.19 ± 0.241 c3.18 ± 0.020 d3.15 ± 0.046 c
RH (%)H36.68 ± 0.387 a35.44 ± 0.281 a34.85 ± 0.147 a34.23 ± 0.448 ab33.60 ± 0.359 a32.71 ± 0.359 a31.27 ± 0.410 b30.82 ± 0.431 b29.47 ± 0.309 b25.19 ± 0.478 c24.52 ± 0.289 c23.27 ± 0.601 c
SH48.56 ± 0.294 a48.27 ± 0.267 a38.7 ± 0.153 a44.90 ± 0.493 b42.47 ± 0.291 b37.04 ± 0.166 ab41.15 ± 0.597 c39.80 ± 0.115 c34.71 ± 0.389 b36.82 ± 0.429 d35.90 ± 0.493 d29.04 ± 0.615 c
AH52.60 ± 0.529 a55.27 ± 0.819 a41.7 ± 0.351 a49.30 ± 0.351 b47.60 ± 0.529 b39.27 ± 0.636 ab44.97 ± 0.35 bc42.85 ± 0.790 c37.17 ± 0.119 bc40.33 ± 0.882 c37.5 ± 0.500 d35.09 ± 0.327 c
ASH49.27 ± 0.357 a49.21 ± 0.116 a38.82 ± 0.133 a47.4 ± 0.200 b45.15 ± 0.076 b38.26 ± 0.173 b42.59 ± 0.049 c41.69 ± 0.164 c36.76 ± 0.148 b37.54 ± 0.356 d37.21 ± 0.107 d35.00 ± 0.234 c
Vv
(cmm)
H41.90 ± 0.466 d41.00 ± 0.577 d40.93 ± 0.468 d52.16 ± 0.443 c51.05 ± 0.621 c48.41 ± 0.747 c67.74 ± 0.378 b66.45 ± 0.294 b57.42 ± 0.550 b73.53 ± 0.290 a70.67 ± 0.333 a67.27 ± 1.124 a
SH40.03 ± 0.260 d39.73 ± 0.187 d39.00 ± 0.500 d49.47 ± 0.502 c48.90 ± 0.587 c47.59 ± 0.549 c64.74 ± 0.378 b64.19 ± 0.424 b56.49 ± 0.866 b70.29 ± 0.618 a69.29 ± 0.633 a61.34 ± 0.393 a
AH38.93 ± 0.515 d37.50 ± 0.500 d34.45 ± 0.292 c50.00 ± 1.155 c49.00 ± 1.000 c46.17 ± 0.647 b60.33 ± 1.155 b59.67 ± 1.528 b55.81 ± 0.226 a68.33 ± 0.333 a66.33 ± 0.577 a57.62 ± 0.314 a
ASH36.60 ± 0.150 d34.96 ± 0.031 d29.18 ± 0.157 d54.78 ± 0.048 b46.21 ± 0.107 c44.56 ± 0.300 c57.14 ± 0.305 b54.78 ± 0.048 b46.45 ± 0.121 b74.78 ± 0.264 a66.14 ± 0.071 a56.75 ± 0.411 a
OGS: Open green space. (a, b, c, d are difference significance analysis, a is significant difference, and so on).

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Figure 1. Site locations and measured spaces.
Figure 1. Site locations and measured spaces.
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Figure 2. Dynamic Stream Chart and dynamic Ridgeline plots. The X-axis of the three graphs on the left represents “the sampling point numbers of the Qiaoguan grass”, while the Y-axis represents “Globe Temperature (°C), Air Temperature (°C), Mean Radiant Temperature (°C), Universal Thermal Climate Index, Relative Humidity (%), Velocity of Air Motion (cmm), and Air Velocity (m/s)”. The X-axis of the three graphs on the right represents the four seasons, while the Y-axis represents “the sampling point numbers of the Qiaoguan grass”.
Figure 2. Dynamic Stream Chart and dynamic Ridgeline plots. The X-axis of the three graphs on the left represents “the sampling point numbers of the Qiaoguan grass”, while the Y-axis represents “Globe Temperature (°C), Air Temperature (°C), Mean Radiant Temperature (°C), Universal Thermal Climate Index, Relative Humidity (%), Velocity of Air Motion (cmm), and Air Velocity (m/s)”. The X-axis of the three graphs on the right represents the four seasons, while the Y-axis represents “the sampling point numbers of the Qiaoguan grass”.
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Figure 3. A post hoc Tukey’s test for different pairs of measurement points for the meteorological variables (ASH, AH, SH and S). A–D stand for different times, 09,07, 10,08, 11,07, 12,07; * p < 0.05 ** p < 0.01. (*** is the significance difference analysis, the more * the more significant the difference).
Figure 3. A post hoc Tukey’s test for different pairs of measurement points for the meteorological variables (ASH, AH, SH and S). A–D stand for different times, 09,07, 10,08, 11,07, 12,07; * p < 0.05 ** p < 0.01. (*** is the significance difference analysis, the more * the more significant the difference).
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Figure 4. The comfort level of respondents in different spaces.
Figure 4. The comfort level of respondents in different spaces.
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Figure 5. Respondents’ perception of extreme weather in different spaces.
Figure 5. Respondents’ perception of extreme weather in different spaces.
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Figure 6. Respondents’ opinions on renovation of different spaces.
Figure 6. Respondents’ opinions on renovation of different spaces.
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Figure 7. (a) Wind speed simulation results. (b) Relationships between measured and simulated Va. The X-axis represents the sample point number, while the Y-axis represents air velocity. (c) Simulation results of air velocity. (d) Relationships between measured and simulated RH. (e) Relationships between measured and simulated RH. The X-axis represents the sample point number, while the Y-axis represents relative humidity. (f) Relative humidity simulation results.
Figure 7. (a) Wind speed simulation results. (b) Relationships between measured and simulated Va. The X-axis represents the sample point number, while the Y-axis represents air velocity. (c) Simulation results of air velocity. (d) Relationships between measured and simulated RH. (e) Relationships between measured and simulated RH. The X-axis represents the sample point number, while the Y-axis represents relative humidity. (f) Relative humidity simulation results.
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Figure 8. Relationships between measured and simulated UTCI.
Figure 8. Relationships between measured and simulated UTCI.
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Figure 9. Schematic diagram of bioclimatic transformation.
Figure 9. Schematic diagram of bioclimatic transformation.
Buildings 13 02329 g009aBuildings 13 02329 g009b
Figure 10. Compare original and retrofit UTCI.
Figure 10. Compare original and retrofit UTCI.
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Figure 11. UTCI simulation result.
Figure 11. UTCI simulation result.
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Figure 12. Retrofit sunshine.
Figure 12. Retrofit sunshine.
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Table 1. Average meteorological parameters in Lanzhou city from 2001 to 2020.
Table 1. Average meteorological parameters in Lanzhou city from 2001 to 2020.
Average Humidity (%)Average Wind Speed (m/s)Average Temperature (°C)Cumulative Precipitation (mm)Cumulative Sunshine Duration (h)
200157.213.797.91292.522606.69
200257.473.658.07299.062616.25
200360.573.847.83382.602552.71
200456.256.015.60292.712712.01
200556.745.246.21306.392489.82
200657.505.237.00272.492506.88
200760.025.176.56423.422418.02
200859.305.095.98336.802557.43
200956.995.166.77270.472437.19
201057.775.366.52282.362594.43
201158.805.086.10274.132450.31
201259.124.945.78357.332507.42
201353.355.056.95320.002606.57
201458.335.206.40393.352494.27
201556.255.336.97264.542549.92
201656.665.337.01362.332692.70
201757.175.006.68361.872490.41
201859.725.066.54504.662461.90
201960.355.106.50402.572334.70
202057.225.186.57347.822361.26
Table 2. Measurement of spatial–temporal meteorological variables.
Table 2. Measurement of spatial–temporal meteorological variables.
OGS1OGS2OGS3
Va (m/s)max0.830.790.78
min0.360.330.22
average0.580.550.51
Vv (cmm)max76.2371.0069.12
min35.3034.9029.00
average56.1054.1349.34
Tg (°C)max14.0013.7012.70
min3.903.983.60
average8.918.207.91
Ta (°C)max12.5012.0011.00
min1.801.701.50
average6.585.945.49
RH (%)max56.8053.0042.10
min24.3524.0022.00
average41.5940.2935.11
Table 3. Technical details of meteorological equipment.
Table 3. Technical details of meteorological equipment.
ParameterAbbreviationInstrumentRangeAccuracy
Globe temperatureTgWGBT-3020–45 °C<2%
Wind speedVaAnemometer0~360°/0~60 m/s±3°/±0.3 m/s
Wind volumeVvSIGMA AR866A0–999,900 m3/min±1°
Air temperatureTaSIGMA AS837−10–50°±1.5°
Relative humidityRHSIGMA AS8375%RH–98%RH±5%RH (5–40%RH)
Table 4. Bioclimatic design strategies suitable for scenic open spaces in urban areas.
Table 4. Bioclimatic design strategies suitable for scenic open spaces in urban areas.
SpaceInfluencing FactorsOptimal Design Strategies
OGS1
Take ASH space as an example
Closest to the Yellow River, the cold lake effect is the most obvious.
Windy, high wind speed, large air volume; fewer trees that reduce wind speed in winter.
The spatial distribution of shrubs, arbor and grass is unreasonable.
The entrance of the plot faces the Yellow River, and the entire space lacks plant enclosures and wind shields.
With less precipitation in winter, plants need increased post-maintenance.
Reduce shrubs and improve natural ventilation.
Increase large evergreen trees.
Increase the number of fountain pools.
Install outdoor spraying equipment.
Increase lawn irrigation facilities.
OGS2
Take ASH space as an example
Close to the Yellow River, there is a certain cold lake effect.
Windy, few trees that reduce wind speed.
In winter, the temperature is low and there is a lack of tree species with strong thermal insulation ability.
There is little precipitation in winter.
There are shelters around the space, which is not conducive to natural ventilation.
There is not enough space for activities.
Increase large evergreen trees.
According to the research of single tree and single irrigation, choose Syringa oblata to increase the ambient temperature, and choose Prunus cerasifera f. atropurpurea and Syringa oblata to save water.
Reduce the space between tree pools and increase the area of seating shade and event space.
OGS3
Take ASH space as an example
Far from the Yellow River, the cold lake effect is not obvious.
In winter, there is less precipitation, the lowest humidity and the lowest temperature in the grassy space.
There is a certain wind in winter, there are no trees, and it is impossible to block the wind.
Add large evergreen trees, which can be planted alone, or in 3–5 clusters, to ensure lawn space but also provide a certain wind resistance.
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Lin, J.; Jiang, S.; Zhang, S.; Yang, S.; Ji, W.; Li, W. Thermal Comfort in Urban Open Green Spaces: A Parametric Optimization Study in China’s Cold Region. Buildings 2023, 13, 2329. https://doi.org/10.3390/buildings13092329

AMA Style

Lin J, Jiang S, Zhang S, Yang S, Ji W, Li W. Thermal Comfort in Urban Open Green Spaces: A Parametric Optimization Study in China’s Cold Region. Buildings. 2023; 13(9):2329. https://doi.org/10.3390/buildings13092329

Chicago/Turabian Style

Lin, Jiayi, Songlin Jiang, Shuangyu Zhang, Siyu Yang, Wenli Ji, and Weizhong Li. 2023. "Thermal Comfort in Urban Open Green Spaces: A Parametric Optimization Study in China’s Cold Region" Buildings 13, no. 9: 2329. https://doi.org/10.3390/buildings13092329

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