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Published on: May 29, 2019
A convolutional neural networks method for tropospheric ozone vertical distribution retrieval from Multi-AXis
Zijie Wang1, Xin Tian1, Pinhua Xie2
1Information Materials and Intelligent Sensing Laboratory of Anhui Province, Institutes of Physical Science and Information Technology, Anhui University, Hefei 230601, China.
This study introduces a Convolutional Neural Network (CNN) model to accurately retrieve tropospheric ozone (O3) vertical distribution using Multi-AXis Differential Optical Absorption Spectroscopy (MAX-DOAS) data, improving upon previous methods by reducing error rates.
Area of Science:
- Atmospheric Chemistry and Physics
- Remote Sensing
- Machine Learning Applications in Environmental Science
Background:
- Tropospheric ozone (O3) vertical distribution is critical for atmospheric processes.
- Multi-AXis Differential Optical Absorption Spectroscopy (MAX-DOAS) measurements face challenges with stratospheric O3 interference for tropospheric profiling.
- Accurate O3 profiles are essential for air quality monitoring and climate studies.
Purpose of the Study:
- To develop and validate a Convolutional Neural Network (CNN) model for retrieving tropospheric O3 vertical distribution from MAX-DOAS measurements.
- To address and overcome the interference from stratospheric O3 absorption in MAX-DOAS data.
- To enhance the accuracy and reliability of tropospheric O3 profile retrievals.
Main Methods:
- A hybrid feature selection model (PCA-F_Regression-SVR) was employed to identify sensitive factors for O3 inversion, including meteorological and trace gas profiles.
- A CNN model was constructed using preprocessed MAX-DOAS spectra and selected sensitive factors as input, with reanalysis O3 profiles as output.
- The model's performance was evaluated using Mean Absolute Percentage Error (MAPE) and compared against independent datasets.
Main Results:
- The CNN model successfully reproduced tropospheric O3 profiles, with Mean Absolute Percentage Error (MAPE) decreasing from 26% to approximately 19%.
- The retrieved O3 profiles exhibited a Gaussian-like distribution, peaking around 950 hPa (550 m).
- The model showed a tendency to overestimate surface O3 in summer due to temperature influences, while being insensitive to extreme values in smoothed reanalysis data.
Conclusions:
- The developed CNN model effectively leverages MAX-DOAS spectra for accurate tropospheric O3 vertical distribution retrieval.
- The method successfully mitigates stratospheric O3 interference, offering a more reliable approach to O3 profiling.
- This technique provides valuable data for atmospheric research, air quality management, and climate modeling.
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