Development and Application of Climate Zoning for Asphalt Pavements in China: A Review and Perspective
Abstract
1. Introduction
Review Methodology
2. Asphalt Pavement Climate Zoning Development Characteristics
2.1. Development Stages of Asphalt Pavement Climate Zoning
2.2. Research Keywords in Pavement Climate Zoning
2.3. Provincial Applications of Asphalt Pavement Climate Zoning
3. Asphalt Pavement Climate Zoning Models
3.1. Three-Indicator-Based Climate Zoning Model for Asphalt Pavements
3.2. Climate Zoning Model Based on the Hydrothermal Coefficient
3.3. Climate Zoning Models Based on Clustering Analysis
3.4. Summary of the Performance of Three Climate Zoning Methods
4. Application of Climate Zoning in Performance Grade (PG) Asphalt Binder Classification
- (1)
- High-Temperature Design Models
- (2)
- Low-Temperature Design Models [38]
5. Future Perspectives
6. Conclusions
Author Contributions
Funding
Institutional Review Board Statement
Data Availability Statement
Acknowledgments
Conflicts of Interest
References
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Year | Author | Region | Climate Zoning Results |
---|---|---|---|
1994 | Shen et al. [34] | China | Analyzed 30 years of data from 615 meteorological stations nationwide; identified 26 asphalt pavement climate zones. |
2004 | Deng et al. [29] | Liaoning | Developed a comprehensive climate impact index using high temp, low temp, and precipitation; divided the province into three zones. |
2007 | Sun et al. [38] | Jiangxi | Divided Jiangxi into three regions based on climate influence classification: the 1-3-1, 2-3-1, and 1-4-1 types. |
2008 | Zheng et al. [39] | Xi’an | Used three indicators and varying guarantee levels; divided Xi’an into seven zones. |
2008 | Zhou et al. [40] | Liaoning | Applied a composite climate impact index with three indicators; identified three zones. |
2010 | Feng et al. [41] | Guangxi | Divided Guangxi into a 1-4-1 climate zone classification using the three-indicator model. |
2011 | Wang et al. [42] | Guangdong | Based on 30 years of meteorological data from four typical areas; classified Guangdong into the 1-4-1 zone. |
2011 | Shi et al. [43] | Jiangxi | Redefined high-temperature thresholds using cumulative temperatures ≥30 °C and reclassified rainfall boundaries; identified eight zones. |
2011 | Fu et al. [44] | Hunan | Refined zoning thresholds based on Hunan’s climatic features; identified six zones. |
2012 | Liang et al. [45] | Shaanxi | Analyzed 20 years of climate data from 10 cities; identified three asphalt pavement climate zones. |
2012 | Tang et al. [46] | Hainan | Applied spatial interpolation and province-specific thresholds; identified nine zones. |
2017 | Lv et al. [47] | Tibet | Statistically analyzed 30-year climate data; classified Tibet into six zones. |
2021 | Wu et al. [48] | Qinghai | Integrated sunshine duration into the three-indicator model; divided Qinghai into 10 zones. |
Year | Author | Region | Clustering Method | Climate Zoning Indicators | Climate Zoning Results |
---|---|---|---|---|---|
2007 | Miao et al. [30] | China | Hierarchical Clustering | Accumulated temperature, precipitation–temperature index, combined precipitation–frost index, solar radiation | Divided China into 8 primary zones using multi-indicator clustering and further refined it into 39 secondary zones using single-indicator zoning. |
2012 | Gao et al. [56] | Tibet | Hierarchical Clustering (Ward’s Method) | High temp, low temp, daily temperature range, solar radiation | Applied spline interpolation and GIS; selected the seventh merge result to define five climate zones and indicator ranges. |
2015 | Han et al. [31] | China | Fast, Hierarchical, and Statistical Clustering | Days with stable 5-day sliding average temperature > 10 °C | Classified China into 10, 9, and 13 zones via three methods; finalized 9-zone classification considering temperature variability. |
2017 | Liu et al. [35,36] | China | Q-type Clustering | Temperature, precipitation | Developed a zoning framework; divided Southern China into four zones and Northern China into three, using geographic + thermal + moisture traits. |
2018 | Yang et al. [57] | Liaoning | Ward’s Method | High temp, low temp, precipitation | Used SPSS for clustering; divided Liaoning Province into five climatic zones. |
2020 | Sun et al. [51] | Inner Mongolia | Hierarchical Clustering | High temp, low temp, temperature range, rainfall, solar radiation | Applied kriging for interpolation; used 10th merge to classify eight climate zones. |
2020 | Yang et al. [32] | Liaoning | K-means Clustering | High temp, low temp, precipitation, solar radiation | Applied PCA to extract cluster factors; identified four zones. Accuracy verified via PNN and SVM (>90%). |
2021 | Zhou et al. [58] | Guangdong | Fuzzy C-means Clustering | High temp, low temp, precipitation | Used DEM-based interpolation; identified four climate zones. |
2022 | Fang et al. [33] | China | Fuzzy C-means Clustering | High temp, low temp, mean temp, precipitation | Applied IDW, ordinary kriging, and DEM-based co-kriging; classified China into 10 asphalt pavement climate zones. |
2022 | Zhao et al. [59] | Inner Mongolia | Hierarchical Clustering + Overlay Method | High temp, low temp, precipitation, accumulated temp, temp range, permafrost depth | Used six kriging methods for interpolation; defined 6 surface climate zones and 10 subgrade performance zones. |
High-Temperature Grade | Low-Temperature Grade | ||||||
---|---|---|---|---|---|---|---|
PG46 | −34 | −40 | −46 | — | — | — | — |
PG52 | −10 | −16 | −22 | −28 | −34 | −40 | −46 |
PG58 | −16 | −22 | −28 | −34 | −40 | — | — |
PG64 | −10 | −16 | −22 | −28 | −34 | −40 | — |
PG70 | −10 | −16 | −22 | −28 | −34 | −40 | — |
PG76 | −10 | −16 | −22 | −28 | −34 | — | — |
PG82 | −10 | −16 | −22 | −28 | −34 | — | — |
Author (Year) | Indicator | Temperature Conversion Formula | PG Grading Application Summary |
---|---|---|---|
Zhang et al. (2003) [64] | High Temperature | Tmax = −12.189 + 1.176Tair1 + 0.966Lat | Extreme maximum surface temperature was selected as the high-temperature indicator based on geographic analysis. A regression formula was developed through comparison with the SHRP model and actual meteorological data, and was ultimately adopted for zoning. The collapsible loess region was classified into six PGs according to the established criteria. |
Low Temperature | Tmin = −1.866 + 1.083Tair2 | ||
Deng et al. (2004) [29] | High Temperature | Tmax = 47.519 + 2.805Tair1 − 1.818Lat | The high-temperature indicator was defined as the average extreme maximum surface temperature through statistical analysis. A regression-based conversion formula was selected over the SHRP model for improved regional accuracy. PG classification was applied to divide Liaoning Province into four performance zones. (In the low-temperature formula, F represents the maximum wind speed in January, in m/s.) |
Low Temperature | Tmin = 0.533Tair2 − 1.53Lat − 0.084F + 49.73 | ||
Liang et al. (2012) [45] | High Temperature | Tmax = 11.269 + 1.1Tair1 + 0.996Lat | Three models—linear regression, SHRP, and LTPP—were compared. For high-temperature conversion, SHRP < regression < LTPP; for low-temperature conversion, SHRP < regression < LTPP < C-SHRP. Based on this comparison, the regression model was chosen for temperature index transformation. Shaanxi Province was classified into four PG zones. |
Low Temperature | Tmin = −1.7288 + 1.03506Tair2 | ||
Zhang et al. (2012) [65] | High Temperature | Tmax = (Tair1 − 0.00907Lat2 + 0.2773Lat + 2.1273) × 4.3662 − 57.78 | A high-temperature conversion formula was derived for Heilongjiang Province based on the SHRP model, while a low-temperature formula was derived using the C-SHRP approach. The province’s asphalt pavement performance was ultimately classified into three PG zones. |
Low Temperature | Tmin = 1.91Tair2 + 31.0893 | ||
Liu et al. (2014) [66] | High Temperature | Tmax = Tair1 − 0.0017Lat2 − 0.4936Lat + 48.0 | Similar to the study [49], it is recommended that Heilongjiang Province adopt the SHRP high-temperature design formula and the Canadian C-SHRP low-temperature design formula for temperature conversion and PG determination. The province’s asphalt pavement performance was ultimately classified into three PG zones. |
Low Temperature | Tmin = 0.967Tair2 + 1.0 |
Author (Year) | Indicator | Temperature Conversion Formula | PG Grading Application Summary |
---|---|---|---|
Wang et al. (2006) [67] | High Temperature | LTPP | A comparison between the SHRP and LTPP temperature conversion formulas showed that the LTPP model consistently yielded higher temperature values. For safety considerations, the LTPP formula was adopted to classify asphalt pavement performance in Inner Mongolia into seven PGs. |
Low Temperature | LTPP | ||
Ma et al. (2006) [68] | High Temperature | SHRP | The SHRP temperature conversion formula was directly applied to calculate the zoning indicators; asphalt pavement performance in the Liupan Mountains region was classified into two PGs. |
Low Temperature | SHRP | ||
Luo et al. (2008) [69] | High Temperature | LTPP | Two scholars reached similar conclusions: After comparison, it was found that the LTPP formula produced the highest high-temperature values, while the SHRP formula yielded the lowest low-temperature values. Therefore, the LTPP model was used for high-temperature indicator design, and the SHRP model was used for low-temperature indicator design. Based on these results, asphalt pavements in Guangxi were classified into a single grade: PG70-10. |
Low Temperature | SHRP | ||
Feng et al. (2010) [41] | High Temperature | LTPP | |
Low Temperature | SHRP | ||
Fu et al. (2011) [44] | High Temperature | SHRP | The SHRP temperature conversion formula was directly adopted for zoning indicators; Hunan Province was classified into two PGs. |
Low Temperature | SHRP | ||
Chen et al. (2011) [70] | High Temperature | SHRP | For Hainan Province, the comparison revealed that the SHRP formula produced the highest high-temperature conversion values, while the LTPP formula produced the lowest low-temperature values. As a result, the SHRP formula was used for high-temperature indicators and the LTPP formula for low-temperature indicators; the region was classified into two PGs. |
Low Temperature | LTPP | ||
Zhu et al. (2016) [71] | High Temperature | LTPP | A comparative analysis showed that the LTPP model produced the highest high-temperature values, and the SHRP model the lowest low-temperature values. However, the SHRP model was considered overly conservative. Ultimately, the LTPP formula was selected as the temperature conversion model for Jiangxi Province, which was then divided into three PGs. |
Low Temperature | LTPP | ||
Jiao et al. (2016) [72] | High Temperature | SHRP | The SHRP temperature conversion model was directly used to calculate zoning indicators; Hebei Province was classified into five PGs. |
Low Temperature | SHRP | ||
Lv et al. (2017) [47] | High Temperature | LTPP | For Tibet, it was found that the LTPP formula provided the highest high-temperature values, and the SHRP formula the lowest low-temperature values. Consequently, the LTPP model was used for high-temp indicators and the SHRP model for low-temp indicators; the region was classified into nine PGs. |
Low Temperature | SHRP | ||
Tang et al. (2017) [73] | High Temperature | LTPP | For Xinjiang, comparison revealed that the LTPP formula yielded both the highest high-temperature and lowest low-temperature conversion values. Therefore, the LTPP model was used to classify the province into seven PGs. |
Low Temperature | LTPP | ||
Wu et al. (2021) [48] | High Temperature | SHRP | The SHRP formula was directly applied for temperature conversion in Qinghai Province, where asphalt pavement performance was classified into seven PGs. |
Low Temperature | SHRP |
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Chang, H.; Wang, X.; Fang, N. Development and Application of Climate Zoning for Asphalt Pavements in China: A Review and Perspective. Atmosphere 2025, 16, 953. https://doi.org/10.3390/atmos16080953
Chang H, Wang X, Fang N. Development and Application of Climate Zoning for Asphalt Pavements in China: A Review and Perspective. Atmosphere. 2025; 16(8):953. https://doi.org/10.3390/atmos16080953
Chicago/Turabian StyleChang, Huanyu, Xuesen Wang, and Naren Fang. 2025. "Development and Application of Climate Zoning for Asphalt Pavements in China: A Review and Perspective" Atmosphere 16, no. 8: 953. https://doi.org/10.3390/atmos16080953
APA StyleChang, H., Wang, X., & Fang, N. (2025). Development and Application of Climate Zoning for Asphalt Pavements in China: A Review and Perspective. Atmosphere, 16(8), 953. https://doi.org/10.3390/atmos16080953