Retrieving XCO2from GOSAT FTS over east asia using simultaneous aerosol information from CAI

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Abstract

In East Asia, where aerosol concentrations are persistently high throughout the year, most satellite CO2 retrieval algorithms screen out many measurements during quality control in order to reduce retrieval errors. To reduce the retrieval errors associated with aerosols, we have modified YCAR (Yonsei Carbon Retrieval) algorithm to YCAR-CAI to retrieve XCO2 from GOSAT FTS measurements using aerosol retrievals from simultaneous Cloud and Aerosol Imager (CAI) measurements. The CAI aerosol algorithm provides aerosol type and optical depth information simultaneously for the same geometry and optical path as FTS. The YCAR-CAI XCO2 retrieval algorithm has been developed based on the optimal estimation method. The algorithm uses the VLIDORT V2.6 radiative transfer model to calculate radiances and Jacobian functions. The XCO2 results retrieved using the YCAR-CAI algorithm were evaluated by comparing them with ground-based TCCON measurements and current operational GOSAT XCO2 retrievals. The retrievals show a clear annual cycle, with an increasing trend of 2.02 to 2.39 ppm per year, which is higher than that measured at Mauna Loa, Hawaii. The YCAR-CAI results were validated against the Tsukuba and Saga TCCON sites and show an root mean square error of 2.25, a bias of 0.81 ppm, and a regression line closer to the linear identity function compared with other current algorithms. Even after post-screening, the YCAR-CAI algorithm provides a larger dataset of XCO2 compared with other retrieval algorithms by 21% to 67%, which could be substantially advantageous in validation and data analysis for the area of East Asia. Retrieval uncertainty indicates a 1.39 to 1.48 ppm at the TCCON sites. Using Carbon Tracker-Asia (CT-A) data, the sampling error was analyzed and was found to be between 0.32 and 0.36 ppm for each individual sounding.

Figures

  • Table 1. Specification of state vectors and a priori information.
  • Figure 1. Comparisons of retrieved AOD from MODIS and TANSO-CAI over ocean in: (a) 2010; and (b) 2011. Colors represent the frequency of compared results.
  • Table 2. Summary of the CO2 datasets used in this study.
  • Table 3. Major differences between CO2 retrieval algorithms.
  • Figure 2. The relation between XCO2 difference (XCO2, GOSAT—XCO2, TCCON) and filter variables. Blue dots are mean XCO2 difference of each bin with error bar of standard deviation. Red line represents post screening criteria.
  • Table 4. Post-screening criteria.
  • Figure 3. Time series of retrieved XCO2 from four GOSAT algorithms (YCAR-CAI, NIES, ACOS, and UoL, from top to bottom, respectively) and from two TCCON sites (Tsukuba (left) and Saga (right)). All TCCON retrieved data are shown in small gray dots and daily average TCCON XCO2 values within 1 h of GOSAT passing times (approximately 12:50 UTC at East Asia TCCON sites) are shown in large black dots.
  • Figure 4. Comparison of retrieved XCO2 from four GOSAT algorithms ((a–c) YCAR-CAI; (d–f) NIES; (g–i) ACOS; and (j–l) UoL) with TCCON XCO2 for two TCCON sites: Tsukuba (middle), Saga (right), and both (left). All individual sounding GOSAT data are shown as small faded dots, and daily average values are shown as large distinct colored dots. Black dotted line is the best-fit line calculated from robust fitting and red dotted lines are RMSE range of best-fit line. The solid line is linear identity function.

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CITATION STYLE

APA

Kim, W., Kim, J., Jung, Y., Boesch, H., Lee, H., Lee, S., … Ou, M. L. (2016). Retrieving XCO2from GOSAT FTS over east asia using simultaneous aerosol information from CAI. Remote Sensing, 8(12). https://doi.org/10.3390/rs8120994

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