Abstract

Global climate change has noticeable influences on the water vapor redistribution in China, which is embodied by the fact that both wetting and drying tendencies were observed across China. This poses the necessity to monitor and understand the water vapor evolution in China. However, observations of water vapor from different techniques are subjected to systematic biases, different spatiotemporal resolutions and coverages, and different accuracy, which would hamper their joint use, potentially leading to contradictory conclusions when using different techniques. Data fusion is a promising way to address this problem. Some scholars have proposed several methods to fuse multi-source PWV data in China region, such as the enhanced spatial and temporal adaptive reflectance fusion model, the hybrid PWV fusion model, and the linear calibration model. Although these models can produce PWV products with improved accuracy, they still have some shortcomings, such as no consideration for spatial or temporal variations in bias or inevitably impose some biases inaccurate information since assumptions made for interpolations are imperfect. In this study, we use the high-quality Global Navigation Satellite System (GNSS) precipitable water vapor (PWV) to calibrate and optimize the Moderate-resolution Imaging Spectroradiometer (MODIS) and the European Centre for Medium-Range Weather Forecasts ReAnalyses 5 (ERA5) PWV in 2018–2019 through a Generalized Regression Neural Network (GRNN) at annual, quarterly, and monthly timescales. Validation results demonstrate that modifying the MODIS and ERA5 PWV at the monthly timescale results in the best accuracy. In the monthly experiment, the average bias, standard deviation (STD), and root mean square (RMS) error of modified MODIS PWV are 0.0 mm, 2.6 mm, and 2.6 mm, respectively. The percentage improvement is as high as 50% in terms of RMS compared to the original MODIS PWV. It becomes 0.0 mm, 1.7 mm, and 1.7 mm for the modified ERA5 PWV and the percentage improvement is 40%. Since the biases among different products are well-calibrated and the accuracy of MODIS and ERA5 PWV is improved to the same level of GNSS PWV, we can fuse them by simply merging them. Finally, we generate a new product of PWV in China with a temporal resolution of 1 day, a spatial resolution better than 31 km, and an accuracy better than 2.7 mm, which will serve as a high-quality product for investigating the water vapor redistribution under a changing climate.

Highlights

  • Licensee MDPI, Basel, Switzerland.Water vapor plays an important role in climate change and water cycling at various scales

  • Zhao et al [18] proposed a precipitable water vapor (PWV) fusion model in China based on the polynomial fitting and spherical harmonic function, and the results showed that the mean root square (RMS) of the hybrid PWV fusion model was less than 3 mm in any areas of China in all four seasons

  • The bias between the modified Moderate-resolution Imaging Spectroradiometer (MODIS) (ERA5) PWV and the Global Navigation Satellite System (GNSS) PWV is close to 0, indicating that the systemic difference between them has been eliminated after training

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Summary

Introduction

Water vapor plays an important role in climate change and water cycling at various scales. Global climate change has exerted noticeable influences on the water vapor distribution in China, which is evidenced by the fact that some regions in western and southern China are becoming wetter while some regions in eastern China are becoming drier [1,2]. Besides being an indicator of climate change, water vapor affects the propagation of radio signals by causing path bending and time delay, which. 2021, 13, 1720 is known as wet tropospheric delay in radio-based geodetic techniques including Global. Water vapor is an error source in radio-based geodetic techniques, and its effect should be corrected. Monitoring the water vapor is a basic requirement for understanding the change in climate and water cycling, and improving the accuracy of radio-based geodetic techniques

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