Improved retrieval of gas abundances from near-infrared solar FTIR spectra measured at the Karlsruhe TCCON station

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Abstract

We present a modified retrieval strategy for solar absorption spectra recorded by the Karlsruhe Fourier Transform Infrared (FTIR) spectrometer, which is operational within the Total Carbon Column Observing Network (TCCON). In typical TCCON stations, the 3800–11g€¯000 cm−1 spectral region is measured on a single extended Indium Gallium Arsenide (InGaAs) detector. The Karlsruhe setup instead splits the spectrum across an Indium Antimonide (InSb) and InGaAs detector through the use of a dichroic beam splitter. This permits measurements further into the mid-infrared (MIR) that are of scientific interest, but are not considered TCCON measurements. This optical setup induces, however, larger variations in the continuum level of the solar spectra than the typical TCCON setup. Here we investigate the appropriate treatment of continuum-level variations in the retrieval strategy using the spectra recorded in Karlsruhe. The broad spectral windows used by TCCON require special attention with respect to residual curvature in the spectral fits. To accommodate the unique setup of Karlsruhe, higher-order discrete Legendre polynomial basis functions have been enabled in the TCCON retrieval code to fit the continuum. This improves spectral fits and air-mass dependencies for affected spectral windows. After fitting the continuum curvature, the Karlsruhe greenhouse gas records are in good agreement with other European TCCON data sets.

Figures

  • Figure 1. Upper panel: typical TCCON spectrum recorded by the Park Falls instrument which operates an extended InGaAs detector, marked are the spectral regions of the main gases of interest; lower panel: typical Karlsruhe spectrum recorded by the InSb and InGaAs diode. The coverage of the full spectral range from 3800– 10 000 cm−1 is realized by the simultaneous operation of the two diodes.
  • Figure 3. Same as Fig. 2 but for Karlsruhe cavity spectra. Both residuals follow the same shape as seen for atmospheric measurements.
  • Figure 2. Spectral fits for a particular Karlsruhe spectrum: upper panel, spectral fit and residual for O2 (cw: 7885.0); lower panel, spectral fit and residual for N2O (cw: 4719.5).
  • Figure 5. Air-mass dependence for the O2 (cw: 7885.0) spectral window retrieved by the standard GGG2014 TCCON retrieval strategy and using a higher-order continuum fit. As a reference, cavityratioed atmospheric spectra are used for the standard GGG2014 retrieval setup.
  • Figure 4. Same as Fig. 2 but using the GGG2014 higher-order continuum fit option. For O2 (upper panel) N = 5 was applied while for N2O (lower panel) N = 3 was used.
  • Figure 6. Update of the XCO2 calibration curve which is discussed in detail in, e.g., Wunch et al. (2010), Messerschmidt et al. (2011), and Geibel et al. (2012) using the continuum fit option for the Karlsruhe TCCON data.
  • Figure 7. Same as Fig. 6 but using the standard GGG2014 TCCON retrieval strategy for Karlsruhe spectra.
  • Table 1. Absolute and relative mean differences of retrieved target gases with and without a higher-order continuum fit.

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APA

Kiel, M., Wunch, D., Wennberg, P. O., Toon, G. C., Hase, F., & Blumenstock, T. (2016). Improved retrieval of gas abundances from near-infrared solar FTIR spectra measured at the Karlsruhe TCCON station. Atmospheric Measurement Techniques, 9(2), 669–682. https://doi.org/10.5194/amt-9-669-2016

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