Local Climate Zone Classification Using Daytime Zhuhai-1 Hyperspectral Imagery and Nighttime Light Data
Abstract
:1. Introduction
- To incorporate many machine learning techniques and features extracted from satellite observation, including spectral, red-edge, textural, and landform features and NTL, for LCZ mapping;
- To explore the potential of using hyperspectral images and their derived feature indices, DEM data, and nighttime lighting data in LCZ classification;
- To assess the variable importance of multiple features on LCZ classifications.
2. Study Area and Datasets
2.1. Study Area
2.2. Datasets
3. Methodology
3.1. Multi-Feature Extraction
3.2. Sample Collection
3.3. Feature Optimization
3.4. Classifiers
- (1)
- Random forests have been extensively employed for categorization [46,47,48] and regression [49,50,51] in remote sensing. The recursive bifurcation method is used by the RF algorithm, which is based on categorical regression trees, to reach the tree structure’s final node [44]. Different decision trees can be used to train samples and forecast results in the RF classifier, which comprises many decision trees. Every tree generates its own prediction. The RF then integrates its votes to anticipate the result by computing the votes in each decision tree [52]. As a result, as compared to individual decision trees, the RF model can greatly enhance the classification results. Furthermore, the RF does well with outliers and noise, successfully avoiding overfitting [12]. Numerous fields have successfully used this technique with positive outcomes. The RF method is superior to many other methods in that it records full data with high accuracy, minimal grading, and no parameters [53].
- (2)
- The XGBoost (extreme gradient boosting) classifier is a tree-integration-based machine learning algorithm for binary or multiclassification problems. It is a gradient boosting framework that trains multiple weak classifiers and combines them into a single strong classifier to improve prediction accuracy. XGBoost uses an optimization algorithm that continuously adds new weak classifiers during training and optimizes the predictive power of each weak classifier using gradient boosting methods to minimize the loss function [45]. It can carry out multiple weak assessments of data collecting by condensing the modeling outcomes of the weak assessments. In addition, the XGBoost approach effectively handles classification and regression issues to produce more data than individual methods [54,55]. XGBoost also has an adaptive regularization capability to prevent overfitting and improve generalization ability [56]. Due to its efficiency and accuracy, one of the most widely used machine learning algorithms is XGBoost.
3.5. Experimental Design
3.6. Accuracy Evaluation
4. Results
4.1. Results of Feature Optimization
4.2. Results of LCZ Classification
4.3. Classification Results for Multi-Feature Combinations
- (1)
- Exp1, which used only the original bands as an input feature, showed the lowest classification accuracy (Exp1: OA = 82.96%, kappa coefficient = 0.81). Most LCZs had PA values above 80%, except for LCZ-1 (compact high-rise), LCZ-3 (compact low-rise), and LCZ-F (bare soil and sand). The UA of LCZ-2 (compact mid-rise) and LCZ-G (water) exceeded 90%.
- (2)
- With regard to the six scenarios, Exp2’s original bands and spectral properties had the best classification accuracy (Exp2: OA = 85.29%, kappa coefficient = 0.84). Aside from that, LCZ-5 (open mid-rise) had the highest PA compared to the other experiments. The UA of Exp2 reached 100% in LCZ-1, LCZ-2, LCZ-7 (lightweight low-rise), LCZ-B (scattered trees), LCZ-C (bush or scrub), and LCZ-G. Similarly, the accuracy of the original bands combined with the textural features as input features in Exp4 was second only to Exp2 (Exp4: OA = 85.15%, kappa coefficient = 0.83). The GLCM helped to improve the PA of LCZ-A (dense trees) and LCZ-E (bare rock or paved). The UA of Exp4 reached 100% in LCZ-7, LCZ-B, and LCZ-G. In conclusion, the accuracy of the LCZ classification was greatly increased by spectral and textural features.
- (3)
- Exp5 used a combination of original bands and landform feature DEMs as input features for classification (Exp5: OA = 84.87%, kappa coefficient = 0.83). The DEM in Exp5 helped to improve the PA of LCZ-1, LCZ-6 (open low-rise), LCZ-A, LCZ-F, and LCZ-G. The UA of Exp5 reached 100% in LCZ-1 and LCZ-B. Similarly, Exp6 used original bands combined with nighttime lights as input features; only Exp5 had the same accuracy. However, the RBV in Exp6 helped to improve the PA of LCZ-4 (open high-rise), LCZ-9 (sparsely built), LCZ-D (low plants), and LCZ-G. The UA of Exp6 reached 100% in LCZ-2, LCZ-B, and LCZ-C.
- (4)
- Exp3 combined the original bands and red-edge features as input features with slightly lower classification accuracy (Exp5: OA = 84.30%, kappa coefficient = 0.83). The UA of Exp3 reached 100% for LCZ-2, LCZ-B, and LCZ-C.
5. Discussion
5.1. Variable Importance Analysis
5.2. Comparison with Existing Methods
6. Conclusions
- (1)
- Our findings demonstrate the method’s superb LCZ mapping accuracy. The RF classifier had a kappa coefficient of 0.86 and the greatest OA (87.34%). The classification accuracy of the XGBoost classifier was marginally lower (OA value of 86.07% and kappa coefficient of 0.85). In a word, the RF classifier outperformed the XGBoost classifier in terms of accuracy and had a clear advantage in recognizing LCZs.
- (2)
- Using only the original bands as input features, the RF and XGBoost algorithms achieved OAs of 82.96% and 80.83%, respectively. The results of the study showed that the accuracies of LCZ classification in terms of spectral and textural features were improved by 2.33% and 2.19% using the RF classifier, respectively.
- (3)
- With a GI value of 0.0212, the variable importance analysis revealed that RBV was the variable that had the greatest impact on LCZ classification. The DEM also yielded a high GI value (0.0159). The feature indices were ranked in order of importance as nighttime lights > original bands > landform features > red-edge features > spectral features > textural features.
Author Contributions
Funding
Data Availability Statement
Acknowledgments
Conflicts of Interest
References
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LCZ Type | Schematic | LCZ Type | Schematic |
---|---|---|---|
LCZ-1 compact high-rise | LCZ-9 sparsely built | ||
LCZ-2 compact mid-rise | LCZ-A dense trees | ||
LCZ-3 compact low-rise | LCZ-B scattered trees | ||
LCZ-4 open high-rise | LCZ-C bush or scrub | ||
LCZ-5 open mid-rise | LCZ-D low plants | ||
LCZ-6 open low-rise | LCZ-E bare rock or paved | ||
LCZ-7 lightweight low-rise | LCZ-F bare soil or sand | ||
LCZ-8 large low-rise | LCZ-G water |
Zhuhai-1 | ALOS | Luojia-1 | |
---|---|---|---|
Spatial resolution (m) | 10 | 12.5 | 130 |
Orbital altitude (km) | 500 | 691.65 | 634 |
Weight (kg) | 67 | 4000 | 20 |
Imaging range (km2) | 150 × 2500 | 35 × 35 | 260 × 260 |
Number of spectral bands | 32 | 4 | 1 |
Spectral range (nm) | 400–1000 | 520–770 | 480–800 |
Operational orbit (°) | 98 | 98.16 | / |
Category | Feature | Input Band | Output Number of Features | Reference |
---|---|---|---|---|
Original band | Spectral information | B1, B2……B32 | 32 | [23] |
Spectral features | Normalized Difference Vegetation Index (NDVI) | NIR: B23-B29 R: B11-B14 | 28 | [35] |
Normalized Difference Water Index (NDWI) | NIR: B23-B29 G: B3-B7 | 35 | [36] | |
Ratio Vegetation Index (RVI) | NIR: B23-B29 R: B11-B14 | 28 | [37] | |
Difference Vegetation Index (DVI) | NIR: B23-B29 R: B11-B14 | 28 | [38] | |
Enhanced Vegetation Index (EVI) | NIR: B23-B29 R: B11-B14 B: B1, B2 | 56 | [39] | |
Green Chlorophyll Vegetation Index (GCI) | NIR: B23-B29 G: B3-B7 | 35 | [40] | |
Red-edge features | Red-edge Normalized Difference Vegetation Index (NDVIre) | NIR: B23-B29 RE: B15-B20 | 42 | [41] |
Red-edge Chlorophyll Index (CIre) | NIR: B23-B29 RE: B15-B20 | 42 | ||
Modified Red-edge Simple Ratio Index (MSRre) | NIR: B23-B29 RE: B15-B20 | 42 | ||
Textural features | Gray-level Co-occurrence Matrix (GLCM) | The first principal component of the Zhuhai-1 images | 8 | [23] |
Landform features | Digital Elevation Model (DEM) | ALOS data resampling | 1 | / |
Nighttime lighting | Radiation Brightness Value (RBV) | Luojia-1 Image | 1 | [32] |
Type | Number of Training Samples | Number of Validation Samples |
---|---|---|
LCZ-1 compact high-rise | 104 | 22 |
LCZ-2 compact mid-rise | 172 | 44 |
LCZ-3 compact low-rise | 229 | 63 |
LCZ-4 open high-rise | 760 | 196 |
LCZ-5 open mid-rise | 806 | 196 |
LCZ-6 open low-rise | 474 | 106 |
LCZ-7 lightweight low-rise | 35 | 19 |
LCZ-8 large low-rise | 301 | 63 |
LCZ-9 sparsely built | 370 | 76 |
LCZ-A dense trees | 242 | 58 |
LCZ-B scattered trees | 55 | 11 |
LCZ-C bush or scrub | 48 | 12 |
LCZ-D low plants | 394 | 108 |
LCZ-E bare rock or paved | 852 | 230 |
LCZ-F bare soil or sand | 599 | 159 |
LCZ-G water | 215 | 51 |
Experiment | Original Band | Spectral Features | Red-Edge Features | Textural Features | Landform Features | Nighttime Lighting |
---|---|---|---|---|---|---|
1 | √ | |||||
2 | √ | √ | ||||
3 | √ | √ | ||||
4 | √ | √ | ||||
5 | √ | √ | ||||
6 | √ | √ | ||||
7 | Optimal variables combination |
Feature | Optimal Variable Selection | Number |
---|---|---|
Original band | B2, B16, B30, B31 | 4 |
Spectral features | NDWI23_5, DVI23_13, EVI23_11_1, EVI23_11_2, EVI23_12_1, EVI23_12_2, EVI23_13_1, EVI23_13_2, EVI23_14_2, EVI24_11_1, EVI24_11_2, EVI24_12_1, EVI24_12_2, EVI24_13_1, EVI24_13_2, EVI24_14_1, EVI24_14_2, EVI25_11_1, EVI25_11_2, EVI25_12_1, EVI25_12_2, EVI25_13_1, EVI25_13_2, EVI25_14_1, EVI25_14_2, EVI26_11_1, EVI26_11_2, EVI26_12_2, EVI26_13_1, EVI26_13_2, EVI26_14_1, EVI26_14_2, EVI27_11_1, EVI27_11_2, EVI27_12_1, EVI27_12_2, EVI27_13_1, EVI27_13_2, EVI27_14_1, EVI27_14_2, EVI28_11_1, EVI28_11_2, EVI28_12_1, EVI28_12_2, EVI28_13_1, EVI28_13_2, EVI28_14_2, EVI29_11_2, EVI29_12_2, EVI29_13_1, EVI29_13_2, EVI29_14_1, EVI29_14_2, GCI23_5, GCI23_7, GCI28_4 | 56 |
Red-edge features | NDVIre24_19, CIre24_20, MSRre24_19 | 3 |
Textural features | Mean, Variance, Homogeneity, Contrast, Dissimilarity, Entropy, Second moment, Correlation | 8 |
Landform features | DEM | 1 |
Nighttime light | RBV | 1 |
Type | RF | XGBoost | ||
---|---|---|---|---|
PA (%) | UA (%) | PA (%) | UA (%) | |
1 | 72.73 | 100.00 | 84.21 | 88.89 |
2 | 81.82 | 100.00 | 74.47 | 100.00 |
3 | 77.78 | 100.00 | 78.46 | 100.00 |
4 | 89.29 | 81.02 | 87.98 | 80.90 |
5 | 83.67 | 83.67 | 89.83 | 85.95 |
6 | 84.91 | 90.91 | 81.82 | 86.09 |
7 | 100.00 | 100.00 | 100.00 | 100.00 |
8 | 88.89 | 93.33 | 83.33 | 87.30 |
9 | 89.47 | 85.00 | 89.80 | 84.62 |
A | 89.66 | 89.66 | 76.79 | 82.69 |
B | 100.00 | 100.00 | 100.00 | 100.00 |
C | 100.00 | 100.00 | 100.00 | 100.00 |
D | 87.96 | 95.96 | 82.80 | 82.80 |
E | 92.17 | 84.13 | 88.99 | 82.55 |
F | 83.65 | 81.10 | 86.67 | 89.14 |
G | 92.16 | 100.00 | 84.31 | 87.76 |
OA (%) | 87.34 | 86.07 | ||
Kappa | 0.86 | 0.85 |
Methodology | Data Source | Study Area | Overall Accuracy | References |
---|---|---|---|---|
Machine learning random forest algorithm | Landsat and ASTER data and their GLCM | Guangzhou and Wuhan, China | 66%, 84% | [23] |
An ensemble classifier | Data products for Sentinel-1 Level-1 Dual-Pol | Global scale, 29 cities | 61.8% | [24] |
Residual convolutional neural network (ResNet) | Sentinel-2 and Landsat-8 images and the VIIRS-based NTL data | Nine cities in Europe | 78% | [26] |
The semi-automatic algorithm | Building information, land use data, and remote sensing images from Landsat 8 | Chenzhou, China | 69.54% | [64] |
Supervised convolutional neural networks (CNNs) | Multi-temporal Sentinel-2 composites | Eight German cities | 86.5% | [65] |
WUDAPT (level 0) method | Landsat 5 satellite images | Hong Kong, China | 58% | [66] |
Our method | Zhuhai-1 images, ALOS_DEM data, Luojia-1 nighttime lighting data | Beijing, China | 87.34% | / |
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© 2023 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).
Share and Cite
Liang, Y.; Song, W.; Cao, S.; Du, M. Local Climate Zone Classification Using Daytime Zhuhai-1 Hyperspectral Imagery and Nighttime Light Data. Remote Sens. 2023, 15, 3351. https://doi.org/10.3390/rs15133351
Liang Y, Song W, Cao S, Du M. Local Climate Zone Classification Using Daytime Zhuhai-1 Hyperspectral Imagery and Nighttime Light Data. Remote Sensing. 2023; 15(13):3351. https://doi.org/10.3390/rs15133351
Chicago/Turabian StyleLiang, Ying, Wen Song, Shisong Cao, and Mingyi Du. 2023. "Local Climate Zone Classification Using Daytime Zhuhai-1 Hyperspectral Imagery and Nighttime Light Data" Remote Sensing 15, no. 13: 3351. https://doi.org/10.3390/rs15133351
APA StyleLiang, Y., Song, W., Cao, S., & Du, M. (2023). Local Climate Zone Classification Using Daytime Zhuhai-1 Hyperspectral Imagery and Nighttime Light Data. Remote Sensing, 15(13), 3351. https://doi.org/10.3390/rs15133351