| Literature DB >> 33260391 |
Liadira Kusuma Widya1,2, Chin-Yu Hsu3, Hsiao-Yun Lee4, Lalu Muhamad Jaelani2, Shih-Chun Candice Lung5,6,7, Huey-Jen Su8, Chih-Da Wu1,9.
Abstract
Because of fast-paced industrialization, urbanization, and population growth in Indonesia, there are serious health issues in the country resulting from air pollution. This study uses geospatial modelling technologies, namely land-use regression (LUR), geographically weighted regression (GWR), and geographic and temporal weighted regression (GTWR) models, to assess variations in particulate matter (PM10) and nitrogen dioxide (NO2) concentrations in Surabaya City, Indonesia. This is the first study to implement spatiotemporal variability of air pollution concentrations in Surabaya City, Indonesia. To develop the prediction models, air pollution data collected from seven monitoring stations from 2010 to 2018 were used as dependent variables, while land-use/land cover allocations within a 250 m to 5000 m circular buffer range surrounding the monitoring stations were collected as independent variables. A supervised stepwise variable selection procedure was applied to identify the important predictor variables for developing the LUR, GWR, and GTWR models. The developed models of LUR, GWR, and GTWR accounted for 49%, 50%, and 51% of PM10 variations and 46%, 47%, and 48% of NO2 variations, respectively. The GTWR model performed better (R2 = 0.51 for PM10 and 0.48 for NO2) than the other two models (R2 = 0.49-0.50 for PM10 and 0.46-0.47 for NO2), LUR and GWR. In the PM10 model four predictor variables, public facility, industry and warehousing, paddy field, and normalized difference vegetation index (NDVI), were selected during the variable selection procedure. Meanwhile, paddy field, residential area, rainfall, and temperature played important roles in explaining NO2 variations. Because of biomass burning issues in South Asia, the paddy field, which has a positive correlation with PM10 and NO2, was selected as a predictor. By using long-term monitoring data to establish prediction models, this model may better depict PM10 and NO2 concentration variations within areas across Asia.Entities:
Keywords: geographic and temporal weighted regression (GTWR); geographically weighted regression (GWR); land-use regression (LUR); nitrogen dioxide (NO2); particulate matter (PM10)
Year: 2020 PMID: 33260391 PMCID: PMC7730102 DOI: 10.3390/ijerph17238883
Source DB: PubMed Journal: Int J Environ Res Public Health ISSN: 1660-4601 Impact factor: 3.390
Figure 1Location of Surabaya City and its land-use allocations.
Figure 2Time-series trend of air pollutants (particulate matter (PM10) and nitrogen dioxide (NO2) concentrations) in Surabaya from 2010 to 2018.
Figure 3Box plots of (a) PM10 concentrations (b) NO2 concentrations of the 7 monitoring stations.
The developed land-use regression (LUR) model for PM10 and NO2.
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| Intercept | 36.28 | <0.01 | - | - |
| a Public Facility5000m | 0.562 | <0.01 | 1.39 | 0.10 |
| b Industry and Warehousing500m | 0.027 | 0.01 | 1.33 | 0.11 |
| c Paddy Field2500m | 0.185 | <0.01 | 2.22 | 0.12 |
| d NDVI250m | −191 | <0.01 | 2.89 | 0.17 |
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| Intercept | −374.13 | 0.08 | - | - |
| e Paddy Field4250m | 0.146 | <0.01 | 2.70 | 0.16 |
| f Residential Area4000m | 0.013 | <0.01 | 1.90 | 0.15 |
| Rainfall | −3.028 | <0.01 | 1.71 | 0.08 |
| Temperature | 13.212 | 0.08 | 2.75 | 0.06 |
a Public facility within a radius of 5000 m; b Industry and Warehousing within a radius of 500 m; c Paddy field within a radius of 2500 m; d Average normalized difference vegetation index (NDVI) within a radius of 250 m; e Paddy field within a radius of 4250 m; f Residential area within a radius of 4000 m.
Comparison of Final Model for PM10 using LUR, geographically weighted regression (GWR) and geographic and temporal weighted regression (GTWR).
| LUR | GWR (Bandwidth: 1.989) | GTWR (Bandwidth: 1.414) | |
|---|---|---|---|
| Intercept | 36.28 a | 36.20–36.50 b | 35.90–37.50 b |
| Public Facility5000m c | 0.562 | 0.559–0.560 | 0.544–0.563 |
| Industry and Warehousing500m d | 0.027 | 0.0271–0.0272 | 0.025–0.029 |
| Paddy Field2500m e | 0.185 | 0.184–0.185 | 0.180–0.186 |
| NDVI250m f | −191 | −191.00~−190.00 | −193~−186 |
| R2 | 0.49 | 0.50 | 0.51 |
| adjusted-R2 | 0.42 | 0.44 | 0.45 |
| AIC | 310.00 | 305.14 | 305.03 |
a coefficient estimates; b minimum and maximum of the coefficient estimates; c Public facility within a radius of 5000 m; d Industry and Warehousing within a radius of 500 m; e Paddy field within a radius of 2500 m; f Average NDVI within a radius of 250 m.
Comparison of final model for NO2 using LUR, GWR and GTWR.
| LUR | GWR (Bandwidth: 1.987) | GTWR (Bandwidth: 1.985) | |
|---|---|---|---|
| Intercept | −374.13 a | −377~−367 b | −377~−366 b |
| Paddy Field4250m c | 0.146 | 0.145~0.146 | 0.144~0.146 |
| Residential Area4000m d | 0.013 | 0.0129~0.0131 | 0.0127~0.0131 |
| Rainfall | −3.028 | −3.07~−2.99 | −3.06~−2.95 |
| Temperature | 13.212 | 12.9~13.3 | 12.90~13.30 |
| R2 | 0.46 | 0.47 | 0.48 |
| adj-R2 | 0.39 | 0.41 | 0.41 |
| AIC | 252.00 | 252.08 | 251.81 |
a coefficient estimates; b minimum and maximum of the coefficient estimates; c Paddy field within a radius of 4250 m; d Residential area within a radius of 4000 m.
Figure 4Prediction maps of PM10 concentration variations using GWR model: (a) 2010 (b) 2011 (c) 2012 (d) 2013 (e) 2014 (f) 2015 (g) 2016 (h) 2017 (i) 2018 (j) average from 2010 to 2018.
Figure 5Prediction maps of NO2 concentration variations using GWR model: (a) 2010 (b) 2011 (c) 2012 (d) 2013 (e) 2014 (f) 2015 (g) 2016 (h) 2017 (i) 2018 (j) average from 2010 to 2018.
Figure 6Prediction maps of PM10 concentration variations using GTWR model: (a) 2010 (b) 2011 (c) 2012 (d) 2013 (e) 2014 (f) 2015 (g) 2016 (h) 2017 (i) 2018 (j) average from 2010 to 2018.
Figure 7Prediction maps of NO2 concentration variations using GTWR model: (a) 2010 (b) 2011 (c) 2012 (d) 2013 (e) 2014 (f) 2015 (g) 2016 (h) 2017 (i) 2018 (j) average from 2010 to 2018.
Figure 8External verification using GWR based on observations regressed against predictions. (a) PM10 (b) NO2.
Figure 9Verification using GTWR based on observations regressed against predictions. (a) PM10 (b) NO2.