Abstract

The atmosphere has substantial effects on optical remote sensing imagery of the Earth’s surface from space. These effects come through the functioning of atmospheric particles on the radiometric transfer from the Earth’s surface through the atmosphere to the sensor in space. Precipitable water vapor (PWV), CO2, ozone, and aerosol in the atmosphere are very important among the particles through their functioning. This study presented an algorithm to retrieve total PWV from the Chinese second-generation polar-orbiting meteorological satellite FengYun 3D Medium Resolution Spectral Imager 2 (FY-3D MERSI-2) data, which have three near-infrared (NIR) water vapor absorbing channels, i.e., channel 16, 17, and 18. The algorithm was improved from the radiance ratio technique initially developed for Moderate-Resolution Imaging Spectroradiometer (MODIS) data. MODTRAN 5 was used to simulate the process of radiant transfer from the ground surfaces to the sensor at various atmospheric conditions for estimation of the coefficients of ratio technique, which was achieved through statistical regression analysis between the simulated radiance and transmittance values for FY-3D MERSI-2 NIR channels. The algorithm was then constructed as a linear combination of the three-water vapor absorbing channels of FY-3D MERSI-2. Measurements from two ground-based reference datasets were used to validate the algorithm: the sun photometer measurements of Aerosol Robotic Network (AERONET) and the microwave radiometer measurements of Energy’s Atmospheric Radiation Measurement Program (ARMP). The validation results showed that the algorithm performs very well when compared with the ground-based reference datasets. The estimated PWV values come with root mean square error (RMSE) of 0.28 g/cm2 for the ARMP and 0.26 g/cm2 for the AERONET datasets, with bias of 0.072 g/cm2 and 0.096 g/cm2 for the two reference datasets, respectively. The accuracy of the proposed algorithm revealed a better consistency with ground-based reference datasets. Thus, the proposed algorithm could be used as an alternative to retrieve PWV from FY-3D MERSI-2 data for various remote sensing applications such as agricultural monitoring, climate change, hydrologic cycle, and so on at various regional and global scales.

Highlights

  • The total precipitable water vapor (PWV) in the atmosphere is an important variable to determine the dynamics of the atmospheric movements

  • This is because the radiance transferring from the ground to the sensor in space is strongly affected by the atmosphere, in which PWV plays a critical role in the atmosphere even though it only contains a small proportion in comparison to the total atmospheric mass

  • The results showed that the agreement between MERSI-2 and in-situ Atmospheric Radiation Measurement Program (ARMP) and Aerosol Robotic Network (AERONET) measurements was acceptable, with an root mean square error (RMSE) of 0.28 g/cm2 (12.6%) and 0.26 g/cm2 (23.7%), respectively

Read more

Summary

Introduction

The total precipitable water vapor (PWV) in the atmosphere is an important variable to determine the dynamics of the atmospheric movements. PWV is required for quantitative remote sensing, such as land surface temperature (LST) retrieval from thermal infrared data [1,2]. This is because the radiance transferring from the ground to the sensor in space is strongly affected by the atmosphere, in which PWV plays a critical role in the atmosphere even though it only contains a small proportion in comparison to the total atmospheric mass. There are two ways through which PWV affects the satellite remote sensing of the Earth’s ground surface: First, water vapor is an important absorber to the radiance at several spectral ranges for remote sensing. Accurate information of PWV in the atmosphere can help to improve the understanding of weather patterns, climate change, hydrological cycles, atmospheric dynamics and the chemical composition of aerosols [8,9]

Objectives
Results
Discussion
Conclusion
Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call