| Literature DB >> 32699313 |
Saleh Yousefi1, Hamid Reza Pourghasemi2, Sayed Naeim Emami1, Soheila Pouyan3, Saeedeh Eskandari4, John P Tiefenbacher5.
Abstract
This study sought to produce an accurate multi-hazard risk map for a mountainous region of Iran. The study area is in southwestern Iran. The region has experienced numerous extreme natural events in recent decades. This study models the probabilities of snow avalanches, landslides, wildfires, land subsidence, and floods using machine learning models that include support vector machine (SVM), boosted regression tree (BRT), and generalized linear model (GLM). Climatic, topographic, geological, social, and morphological factors were the main input variables used. The data were obtained from several sources. The accuracies of GLM, SVM, and functional discriminant analysis (FDA) models indicate that SVM is the most accurate for predicting landslides, land subsidence, and flood hazards in the study area. GLM is the best algorithm for wildfire mapping, and FDA is the most accurate model for predicting snow avalanche risk. The values of AUC (area under curve) for all five hazards using the best models are greater than 0.8, demonstrating that the model's predictive abilities are acceptable. A machine learning approach can prove to be very useful tool for hazard management and disaster mitigation, particularly for multi-hazard modeling. The predictive maps produce valuable baselines for risk management in the study area, providing evidence to manage future human interaction with hazards.Entities:
Year: 2020 PMID: 32699313 PMCID: PMC7376103 DOI: 10.1038/s41598-020-69233-2
Source DB: PubMed Journal: Sci Rep ISSN: 2045-2322 Impact factor: 4.379
Figure 1Location of the study area of Chaharmahal and Bakhtiari Province, Iran.
Figure 2Flowchart of the study methodology.
Figure 3Distribution of the occurrence of the five hazards between 1977 and 2019 in Chaharmahal and Bakhtiari Province (a), and images of the five natural extreme events in the study area (b) taken by Saleh Yousefi (First author).
The effective factors for susceptibility mapping of five hazards.
| Effective factors | Hazard | |||||
|---|---|---|---|---|---|---|
| Full name | Abbreviation | Flood (F) | Wildfire (WF) | Snow avalanche (SA) | Landslide (L) | Land subsidence (LSu) |
| Rainfall | R | * | * | |||
| Digital elevation model | DEM | * | * | * | * | * |
| Land use | LU | * | * | * | * | |
| Lithology | Lit | * | * | * | ||
| Fault distance | FD | * | * | |||
| Slope | S | * | * | * | * | * |
| River distance | RD | * | * | * | * | |
| Groundwater level | GL | * | ||||
| Normalized difference vegetation index | NDVI | * | * | * | ||
| Road distance | RoD | * | * | * | * | |
| Topographic wetness index | TWI | * | * | * | * | |
| Plan curvature | PC | * | * | * | * | |
| Aspect | A | * | * | * | * | * |
| Drainage density | DD | * | * | |||
| Convergence Index | CI | * | ||||
| Minimum temperature | MinT | * | ||||
| Maximum temperature | MaxT | * | ||||
| Urban area distance | UD | * | ||||
| Wind exposition index | WEI | * | * | |||
| Terrain ruggedness index | TRI | * | ||||
| Snow depth | SD | * | ||||
Figure 4The risk maps of the five hazards created from the three machine learning models for Chahaharmahal and Bakhtiari Province.
Figure 5The multi-hazard risk map based on a combination of the five best hazard risk maps for Chaharmahal and Bakhtiari Province (*L Landslide, LSu Land subsidence, F Flood, WF Wildfire, SA Snow avalanche).
AUC values for three machine learning models in mapping natural hazards.
| Model | Hazard | ||||
|---|---|---|---|---|---|
| Flood (F) | Wildfire (WF) | Snow avalanche (SA) | Landslide (L) | Land subsidence (LSu) | |
| SVM | 0.835 | 0.894 | |||
| FDA | 0.962 | 0.825 | 0.779 | 0.920 | |
| GLM | 0.965 | 0.909 | 0.777 | 0.923 | |
Areas of different classes of various hazards.
| Multi-hazard | Area (ha) | Percent (%) |
|---|---|---|
| No hazard | 269,093.34 | 16.511 |
| SA | 186,049.44 | 11.416 |
| WF | 180,470.97 | 11.074 |
| WF + L | 160,292.88 | 9.835 |
| WF + F + LSu | 136,861.83 | 8.398 |
| L | 133,069.95 | 8.165 |
| WF + F + L | 114,211.8 | 7.008 |
| WF + LSu | 101,536.92 | 6.230 |
| SA + L | 84,893.76 | 5.209 |
| F + L | 65,183.67 | 4.000 |
| WF + F | 55,212.84 | 3.388 |
| F | 45,086.31 | 2.766 |
| WF + F + L + LSu | 22,783.14 | 1.398 |
| LSu | 15,398.73 | 0.945 |
| WF + L + LSu | 12,496.86 | 0.767 |
| SA + F | 12,462.66 | 0.765 |
| F + LSu | 10,308.87 | 0.633 |
| SA + F + L | 7,746.75 | 0.475 |
| SA + WF + L | 6,630.3 | 0.407 |
| SA + WF | 3,918.69 | 0.240 |
| F + L + LSu | 2,751.12 | 0.169 |
| L + LSu | 1,112.31 | 0.068 |
| SA + WF + F + L | 1,084.86 | 0.067 |
| SA + WF + F | 353.25 | 0.022 |
| SA + F + LSu | 273.78 | 0.017 |
| SA + F + L + LSu | 140.67 | 0.009 |
| SA + LSu | 118.53 | 0.007 |
| SA + WF + F + L | 85.77 | 0.005 |
| SA + L + LSu | 48.51 | 0.003 |
| SA + WF + L + LSu | 27.72 | 0.002 |
| SA + WF + LSu | 21.78 | 0.001 |