| Literature DB >> 29138390 |
Lei Ma1,2,3, Yu Gao4,5,6, Tengyu Fu4,5,6, Liang Cheng4,5,6, Zhenjie Chen4,5,6, Manchun Li7,8,9.
Abstract
When estimating national PM2.5 concentrations, the results of traditional interpolation algorithms are unreliable due to a lack of monitoring sites and heterogeneous spatial distributions. PM2.5 spatial distribution is strongly correlated to elevation, and the information diffusion algorithm has been shown to be highly reliable when dealing with sparse data interpolation issues. Therefore, to overcome the disadvantages of traditional algorithms, we proposed a method combining elevation data with the information diffusion algorithm. Firstly, a digital elevation model (DEM) was used to segment the study area into multiple scales. Then, the information diffusion algorithm was applied in each region to estimate the ground PM2.5 concentration, which was compared with estimation results using the Ordinary Kriging and Inverse Distance Weighted algorithms. The results showed that: (1) reliable estimate at local area was obtained using the DEM-assisted information diffusion algorithm; (2) the information diffusion algorithm was more applicable for estimating daily average PM2.5 concentrations due to the advantage in noise data; (3) the information diffusion algorithm required less supplementary data and was suitable for simulating the diffusion of air pollutants. We still expect a new comprehensive model integrating more factors would be developed in the future to optimize the interpretation accuracy of short time observation data.Entities:
Year: 2017 PMID: 29138390 PMCID: PMC5686213 DOI: 10.1038/s41598-017-14197-z
Source DB: PubMed Journal: Sci Rep ISSN: 2045-2322 Impact factor: 4.379
Figure 1Elevation and spatial distribution of PM2.5 monitoring sites in the study area. (Created by ArcMap, version 10.2, http://www.esri.com/).
Seven geographical subareas of the study area divided by segmenting the elevation.
| No. | Geographical Subarea | Provinces and Municipalities | Altitude (m) | |
|---|---|---|---|---|
| Average | Range | |||
| 1 | Northeastern area | Liaoning province, south Jilin province, and north Hebei province | 499 | −203–2322 |
| 2 | Eastern coastal area | Beijing city, Shanghai city, Tianjin city, Hebei province, Shandong province, Anhui province, and east Henan province | 63 | −4–1289 |
| 3 | Southeastern coastal area | Zhejiang province, Fujian province, Jiangxi province, Hunan province, Guangdong province, Guangxi Zhuang Autonomous Region, and east Hubei province | 311 | −8–2122 |
| 4 | Central area | Chongqing city, west Henan province, south Shaanxi province, east Hubei province, and east Sichuan province | 743 | 63–2795 |
| 5 | Inner Mongolia-Loess Plateau area | Inner Mongolia Autonomous Region, Ningxia Hui Autonomous Region, Shanxi province, and north Shaanxi province | 1279 | 376–3069 |
| 6 | Yunnan-Guizhou Plateau area | Yunnan province, Guizhou province, and south Sichuan province | 1712 | 132–4638 |
| 7 | Tibetan Plateau area | Gansu province, northeast Sichuan province, and east Qinghai province | 3300 | 630–6241 |
Figure 2Flowchart of the proposed approach.
Figure 3Multi-scale segmentation results of homogeneous-elevation regions, and PM2.5 estimate correlations for different segmentation scales. (Created by ArcMap, version 10.2, http://www.esri.com/).
Comparison of interpolated results derived from Information Diffusion, Inverse Distance Weighted, Ordinary Kriging respectively.
| Daily Average | Information Diffusion | Inverse Distance Weighted | Ordinary Kriging | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| R2 | MAE (µg/m3) | RMSE (µg/m3) | RAE (µg/m3) | R2 | MAE (µg/m3) | RMSE (µg/m3) | RAE (µg/m3) | R2 | MAE (µg/m3) | RMSE (µg/m3) | RAE (µg/m3) | |
| Mean | 0.80 | 13.81 | 19.05 | 68.05 | 0.78 | 14.40 | 20.22 | 74.31 | 0.79 | 13.56 | 18.90 | 67.71 |
| Var | — | 1.05 | 2.55 | 153.78 | — | 1.99 | 4.66 | 526.54 | — | 1.05 | 2.33 | 265.66 |
|
| ||||||||||||
| Mean | 0.83 | 11.01 | 15.64 | 57.80 | 0.81 | 11.50 | 16.69 | 63.52 | 0.82 | 11.55 | 16.18 | 58.74 |
| Var | — | 1.15 | 2.84 | 247.79 | — | 1.31 | 2.64 | 527.98 | — | 2.03 | 5.59 | 370.70 |
|
| ||||||||||||
| Mean | 0.82 | 8.78 | 11.97 | 39.61 | 0.80 | 9.21 | 12.70 | 44.03 | 0.82 | 8.79 | 11.95 | 39.56 |
| Var | — | 0.82 | 1.31 | 16.82 | — | 1.72 | 4.14 | 89.17 | — | 1.37 | 2.76 | 69.43 |
Variations in different grades of PM2.5 concentrations estimated by different methods.
|
| 0–35 | 35–75 | 75–115 | 115–150 | 150–250 | 250–350 |
|---|---|---|---|---|---|---|
| Ground-measured PM2.5 concentration | 10.00% | 47.00% | 29.00% | 4.00% | 9.00% | 1.00% |
| Information Diffusion | 9.00% | 44.00% | 34.00% | 5.00% | 8.00% | 0.00% |
| Inverse Distance Weighted | 10.00% | 42.00% | 34.00% | 7.00% | 6.00% | 1.00% |
| Ordinary Kriging | 6.00% | 45.00% | 35.00% | 8.00% | 5.00% | 1.00% |
|
| ||||||
| Ground-measured PM2.5 concentration | 13.00% | 36.00% | 42.00% | 6.00% | 3.00% | 0.00% |
| Information Diffusion | 14.00% | 28.00% | 52.00% | 4.00% | 2.00% | 0.00% |
| Inverse Distance Weighted | 15.00% | 34.00% | 42.00% | 6.00% | 3.00% | 0.00% |
| Ordinary Kriging | 14.00% | 30.00% | 47.00% | 6.00% | 3.00% | 0.00% |
|
| ||||||
| Ground-measured PM2.5 concentration | 6.00% | 36.00% | 50.00% | 8.00% | 0.00% | 0.00% |
| Information Diffusion | 1.00% | 37.00% | 56.00% | 6.00% | 0.00% | 0.00% |
| Inverse Distance Weighted | 2.00% | 32.00% | 61.00% | 5.00% | 0.00% | 0.00% |
| Ordinary Kriging | 3.00% | 40.00% | 50.00% | 7.00% | 0.00% | 0.00% |
Figure 4Spatial distribution of PM2.5 concentration in the study area using Ordinary Kriging, Information Diffusion, and Inverse Distance Weighted algorithms for different time scales. (Created by ArcMap, version 10.2, http://www.esri.com/).
Figure 5Map showing (a) the terrain of Qinling, and (b–d) the spatial distribution and correlations of monthly average PM2.5 concentration in Qinling produced by (b) Ordinary Kriging, (c) Inverse Distance Weighted, and (d) Information Diffusion algorithms. (Created by ArcMap, version 10.2, http://www.esri.com/).