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Volcanic SO2 retrieved from GF-5 Environmental trace gas Monitoring Instrument

  • role： First author第一作者
  • Affiliation：

    Key Laboratory of Radiometric Calibration and Validation for Environmental Satellites, National Satellite Meteorological Center, China Meteorological Administration, Beijing 100081, China

  • Email：yanhuanhuan136@126.com
  • Introduction：闫欢欢，1986年生，女，副研究员，研究方向为大气成分卫星遥感反演算法、反演产品精度评估、污染气体对大气化学和气候影响分析等。E-mail： yanhuanhuan136@126.com
YAN Huanhuan1,  
  • Affiliation：

    National Space Science Center, Chinese Academy of Sciences, Beijing 100190, China

WANG Houmao2,  
  • Affiliation：

    Key Laboratory of Radiometric Calibration and Validation for Environmental Satellites, National Satellite Meteorological Center, China Meteorological Administration, Beijing 100081, China

WANG Weihe1,  
  • Affiliation：

    Key Laboratory of Radiometric Calibration and Validation for Environmental Satellites, National Satellite Meteorological Center, China Meteorological Administration, Beijing 100081, China

ZHANG Xingying1

resumen

Sulfur dioxide (SO2) from volcanic eruption and its long-distance transportation has a significant impact on global climate change and aviation safety. Satellite remote sensing technology provides an unprecedented advantage for continuous, large spatial and short-revisit monitoring for atmospheric SO2. GF-5 Environmental trace gas Monitoring Instrument (EMI) with high spatial resolution is the China’s first instrument of hyper spectral measurements with wavelength range from 240 nm to 710 nm, and makes daily global observations of key atmospheric constituents, including ozone, nitrogen dioxide, sulfur dioxide.In this paper, based on the atmospheric radiation transfer model SCIATRAN, the clear sky albedo under typical atmospheric conditions is simulated by selecting the ocean area pixels with uniform surface types in the middle and low latitudes to evaluate the accuracy of the EMI Top-of-Atmosphere (TOA) albedo.Secondly, based on the S5P/TROPOMI L1 Radiance data and the DOAS algorithm, after 477nm O4 cloud screening, spectral calibration, slant column to vertical column conversion, the inversion results of total SO2 columns over volcanic eruption areas were obtained and compared with TROPOMI offline L2 SO2 products.Finally, GF-5/EMI SO2 columns were retrieved by using GF-5 EMI UV-2 band observations and DOAS algorithm, and then the retrieved GF-5/EMI SO2 columns were compared with similar S5P/TROPOMI SO2 columns to evaluate the ability of GF-5/EMI on monitoring global SO2 change from volcanic activity.Results show that, in the band range of 300—400 nm, the EMI spectra of the sampling points in the ocean area are lower than the simulated spectra of SCIATRAN, and EMI and TROPOMI spectra show similar systematic biases. SO2 obtained by using TROPOMI L1 Radiance data, three band windows of 315—327 nm, 325—335 nm and 360—390 nm, and DOAS inversion algorithm are compared with the TROPOMI offline L2 SO2 products, which show high correlations (correlation coefficient between 0.97—0.99, relative deviation between 3% and 9%). Therefore, GF-5/EMI can obtain the daily distribution of SO2 from volcanic eruption. The accuracy of GF-5/EMI SO2 columns can meet the needs of application of global volcano monitoring.

palabra clave

remote sensing;GF-5 EMI;volcano;SO2 column;DOAS;TROPOMI

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