Bias Correction of the Ratio of Total Column CH<sub>4</sub> to CO<sub>2</sub> Retrieved from GOSAT Spectra

oleh: Haruki Oshio, Yukio Yoshida, Tsuneo Matsunaga, Nicholas M. Deutscher, Manvendra Dubey, David W. T. Griffith, Frank Hase, Laura T. Iraci, Rigel Kivi, Cheng Liu, Isamu Morino, Justus Notholt, Young-Suk Oh, Hirofumi Ohyama, Christof Petri, David F. Pollard, Coleen Roehl, Kei Shiomi, Ralf Sussmann, Yao Té, Voltaire A. Velazco, Thorsten Warneke, Debra Wunch

Format: Article
Diterbitkan: MDPI AG 2020-09-01

Deskripsi

The proxy method, using the ratio of total column CH<sub>4</sub> to CO<sub>2</sub> to reduce the effects of common biases, has been used to retrieve column-averaged dry-air mole fraction of CH<sub>4</sub> from satellite data. The present study characterizes the remaining scattering effects in the CH<sub>4</sub>/CO<sub>2</sub> ratio component of the Greenhouse gases Observing SATellite (GOSAT) retrieval and uses them for bias correction. The variation of bias between the GOSAT and Total Carbon Column Observing Network (TCCON) ratio component with GOSAT data-derived variables was investigated. Then, it was revealed that the variability of the bias could be reduced by using four variables for the bias correction—namely, airmass, 2 μm band radiance normalized with its noise level, the ratio between the partial column-averaged dry-air mole fraction of CH<sub>4</sub> for the lower atmosphere and that for the upper atmosphere, and the difference in surface albedo between the CH<sub>4</sub> and CO<sub>2</sub> bands. The ratio of partial column CH<sub>4</sub> reduced the dependence of bias on the cloud fraction and the difference between hemispheres. In addition to the reduction of bias (from 0.43% to 0%), the precision (standard deviation of the difference between GOSAT and TCCON) was reduced from 0.61% to 0.55% by the correction. The bias and its temporal variation were reduced for each site: the mean and standard deviation of the mean bias for individual seasons were within 0.2% for most of the sites.