Journal topic
Atmos. Meas. Tech., 12, 6049–6058, 2019
https://doi.org/10.5194/amt-12-6049-2019
Atmos. Meas. Tech., 12, 6049–6058, 2019
https://doi.org/10.5194/amt-12-6049-2019

Research article 21 Nov 2019

Research article | 21 Nov 2019

# Full-physics carbon dioxide retrievals from the Orbiting Carbon Observatory-2 (OCO-2) satellite by only using the 2.06 µm band

Full-physics carbon dioxide retrievals from the Orbiting Carbon Observatory-2 (OCO-2) satellite by only using the 2.06 µm band
Lianghai Wu1, Otto Hasekamp1, Haili Hu1, Joost aan de Brugh1, Jochen Landgraf1, Andre Butz2, and Ilse Aben1 Lianghai Wu et al.
• 1SRON Netherlands Institute for Space Research, Utrecht, the Netherlands
• 2Institute of Environmental Physics, University of Heidelberg, Heidelberg, Germany

Correspondence: Lianghai Wu (l.wu@sron.nl)

Abstract

Passive remote sensing of atmospheric carbon dioxide uses spectroscopic measurements of sunlight backscattered by the Earth's surface and atmosphere. The current state-of-the-art retrieval methods use three different spectral bands, the oxygen A band at 0.76µm and the weak and strong CO2 absorption bands at 1.61 and 2.06µm, respectively, to infer information on light scattering and the carbon dioxide column-averaged dry-air mole fraction XCO2. In this study, we propose a one-band XCO2 retrieval technique which uses only the 2.06µm band measurements from the Orbiting Carbon Observatory-2 (OCO-2) satellite. We examine the data quality by comparing the OCO-2 XCO2 with collocated ground-based measurements from the Total Carbon Column Observing Network (TCCON). Over land and ocean the OCO-2 one-band retrieval shows differences from TCCON observations with a standard deviation of ∼1.30 ppm and a station-to-station variability of ∼0.50 ppm. Moreover, we compare one-band and three-band retrievals over Europe, the Middle East, and Africa and see high correlation between the two retrievals with a SD of 0.93 ppm. Compared to the three-band retrievals, XCO2 retrievals using only the 2.06µm band have similar retrieval accuracy, precision, and data yield.

1 Introduction

Over the past decade, space-based measurements of atmospheric carbon dioxide (CO2) have been used, along with ground-based measurements, to characterize CO2 sources and sinks in order to better understand the carbon cycle. The inversion models that calculate the CO2 fluxes are sensitive to biases in the carbon dioxide dry-air column-averaged mole fraction (XCO2) as small as 0.5 ppm (see e.g., ). This poses enormous challenges on the instruments, calibration, and retrieval algorithms used to measure XCO2, and much effort is needed to reduce instrument, calibration, spectroscopy, and other forward model errors. In particular, scattering by aerosol and thin cirrus clouds (thick clouds are screened) can lead to light path modifications causing unacceptable errors in XCO2 if not accounted for in the radiative transfer calculations . The currently operational CO2 satellites, i.e., the Greenhouse Gases Observing Satellite (GOSAT; ) and the Orbiting Carbon Observatory-2 (OCO-2; ), and the corresponding retrieval algorithms (e.g., ) apply a three-band approach using three spectral bands around 0.76 (O2 A band), 1.61 (weak CO2 band), and 2.06µm (strong CO2 band) to simultaneously retrieve XCO2 and other relevant parameters such as surface albedos and aerosol properties.

It has been proposed by , based on simulated OCO measurements, that retrievals using the 2.06µm band alone actually show a performance similar to that when using three bands. The reasons would be that one-band retrievals are less dependent on spectral scattering properties than three-band retrievals. We examine whether this claim holds for real OCO-2 measurements by comparing the XCO2 products for both methods in terms of accuracy and data yield. For the OCO-2 measurements a single-band retrieval is computationally less expensive, which is important considering the huge data amount to be processed. More generally, a single-band retrieval requires a simpler and thus cheaper instrument and may avoid possible complications related to spectral-window-dependent (calibration) errors. For example for OCO-2, there are indications that it is necessary to fit an intensity offset in the weak and strong CO2 absorption bands to account for potential instrumental errors .

The paper is organized as follows: we first introduce the data that we used in this work in Sect. 2. The retrieval algorithm and setup for three-band and one-band retrievals are described in Sect. 3. Section 4 evaluates the one-band retrieval performance with the Total Carbon Column Observing Network (TCCON) XCO2 observations and compares the performance to that of three-band retrievals. Finally we conclude and discuss our findings in Sect. 5.

2 Data

In this paper, we use OCO-2 version 8 L1b data between September 2014 and October 2017. To evaluate the retrieval performance, we only use measurements that are collocated with TCCON measurements. Although some limitations exist as discussed by , TCCON measurements are still the most appropriate validation product for space-based XCO2 retrievals. OCO-2 measurements are considered collocated when they are taken within 2 h and a distance of less than 3 in both latitude and longitude of a TCCON measurement. Here, we do not use TCCON stations located within polluted areas, high-latitude regions, or areas with significant topography. The retrieval algorithm also uses the ECMWF (European Centre for Medium-Range Weather Forecasts) high-resolution analysis data to obtain meteorological information including pressure, temperature, humidity, and surface wind speed. For each OCO-2 measurement, the surface elevation data are obtained from the 90 m digital elevation data of NASA's Shuttle Radar Topography Mission (SRTM) . Prior information on the carbon dioxide profile is extracted from the CarbonTracker model for the year 2013 with an added annual increase of 2.25 ppm .

3 Retrieval algorithm and methodology

We use the RemoTeC retrieval algorithm , which has been extensively used for greenhouse gas retrievals from satellite observations like GOSAT, OCO-2, and S5P measurements . The adaptations and first use for OCO-2 measurements are described in . There we employed the three-band XCO2 retrievals, which will be used here as a reference to compare against our XCO2 retrievals from the 2.06µm band.

Table 1State vector elements for the three-band and one-band retrievals.

Table 2Filter variables applied to reject low-quality XCO2 retrievals over land and ocean in three-band and one-band retrievals. For most variables, ocean glint retrievals have the same filtering criteria as those over land. However, due to ocean glint's unique viewing geometry and different surface properties, aerosol- and surface-related filtering variables have different ranges and are listed separately in brackets. Filter variables not used in the relevant retrieval type are marked with a sign. The blended albedo can be derived using surface albedos in the O2 A band (A0.76) and 2.06µm band (A2.06) by 2.4A0.761.13A2.06 . The aerosol ratio parameter is calculated with the three retrieved aerosol parameters by $\mathit{\tau }*z/\mathit{\alpha }$.

The three-band retrieval fits OCO-2 measurements in all three OCO-2 spectral windows. The state vector that is retrieved contains 35 elements as shown in Table 1: a 12-layer vertical profile of CO2 partial columns, the total columns of H2O and CH4, three effective scattering parameters, and, for each channel, three albedo parameters describing the Lambertian albedo up to its 2nd-order spectral dependence, an intensity offset, spectral shifts for the Earth radiance measurement, and the solar reference model. We do not retrieve the dry-air column but compute it using the ECMWF meteorological data. As described in , we use a Lambertian reflection model for land surface reflection properties, and for ocean surfaces we use a wind-speed-driven reflection model of  combined with an additive wavelength-dependent Lambertian term. The retrieved three aerosol parameters are the total column number density N, the parameter α of a power-law size distribution ($n\left(r\right)\propto {r}^{-\mathit{\alpha }}$ with the particle radius r), and the central height parameter z of a Gaussian height distribution. The full width at half maximum of the Gaussian height distribution is fixed at 2 km.

Figure 1XCO2 retrievals by using only the 2.06µm band of OCO-2. We evaluate overpass-averaged results over land and ocean separately. In each panel, we include bias (ba), standard deviation of the difference (σa), station-to-station variability (σs), number of overpasses (N), Pearson correlation coefficient (r), and one-to-one line. For each overpass, variations in XCO2 retrievals and TCCON data are presented with error bars.

Figure 2Bias (a) and standard deviation (b) variation at different TCCON stations for one-band and three-band retrievals over land. To see the bias variation on the same reference level, we directly subtract mean bias ba of one-band and three-band retrievals accordingly as listed in Table 3. The station-to-station variability (σs) is included in the legend of (a). In (b), the number of overpass at each station is listed on the bar. The TCCON stations are ordered by latitude from Southern Hemisphere to Northern Hemisphere. Stations with fewer than five overpasses are excluded.

In the one-band retrieval, we attempt to infer XCO2 by only using OCO-2 measurements in the spectral range 20422081 nm. The state vector is the same as for the three-band retrieval except that the CH4 column is not included and it only contains surface albedo, intensity offset, and spectral shift parameters for the 2.06µm band (see Table 1). In the retrieval, we seek the state vector for which a cost function including the difference between the forward model and measurements and a side constraint is minimized. The same Phillips–Tikhonov regularization scheme as employed in the three-band retrieval is used to solve the minimization problem iteratively . Like for the three-band retrieval, we choose the regularization parameter such that the degree of freedom for signal (DFS) for the CO2 profile is in the range 1.01.5 . Clearly, a one-band retrieval using only the 2.06µm band is only possible if surface pressure information from meteorological reanalysis/forecast is used in the retrieval algorithm. Retrieving this information, as is done by most algorithms, requires the O2 A band .

Figure 3Same as Fig. 2, but for retrievals over ocean.

Table 3Overall performance of three-band and one-band retrievals. Here, overall bias and single sounding precision are estimated for single soundings. All other quantities are obtained using overpass-averaged values.

Table 4Similar to Table 3 but for non-scattering retrievals using the 2.06µm band. Here, we use the same cases as one-band retrievals in Table 3.

It should be noted that the retrieval algorithm is only applicable to clear-sky scenes, so we must define a suitable cloud filter that preselects the scenes to be processed. Before performing full-physics XCO2 retrievals, we retrieve the columns of O2, CO2, and H2O independently in the three spectral bands under the assumption of a non-scattering atmosphere. When neglecting cloud or aerosol scattering, the ratio between the CO2 or H2O column retrieved from the 1.61µm band and that retrieved from the 2.06µm band is a measure of the light path modification because a large deviation can be introduced due to different light path sensitivity. The ratio between the retrieved O2 column and the one computed from the ECMWF surface pressure can also be used to detect clouds. We consider the following scenes as sufficiently cloud-free:

$\begin{array}{}\text{(1)}& \begin{array}{rl}\mathrm{0.90}<& \frac{{\mathrm{O}}_{\mathrm{2}}\left(\mathrm{0.76}\phantom{\rule{0.125em}{0ex}}\mathrm{µ}\mathrm{m}\right)}{{\mathrm{O}}_{\mathrm{2}}\left(\mathrm{ecmwf}\right)}<\mathrm{1.02},\mathrm{0.98}<\frac{{\mathrm{H}}_{\mathrm{2}}\mathrm{O}\left(\mathrm{1.61}\phantom{\rule{0.125em}{0ex}}\mathrm{µ}\mathrm{m}\right)}{{\mathrm{H}}_{\mathrm{2}}\mathrm{O}\left(\mathrm{2.06}\phantom{\rule{0.125em}{0ex}}\mathrm{µ}\mathrm{m}\right)}\\ & <\mathrm{1.05}\mathrm{and}\phantom{\rule{0.25em}{0ex}}\mathrm{0.98}<\frac{{\mathrm{CO}}_{\mathrm{2}}\left(\mathrm{1.61}\phantom{\rule{0.125em}{0ex}}\mathrm{µ}\mathrm{m}\right)}{{\mathrm{CO}}_{\mathrm{2}}\left(\mathrm{2.06}\phantom{\rule{0.125em}{0ex}}\mathrm{µ}\mathrm{m}\right)}<\mathrm{1.03}\end{array}.\end{array}$

This classifies around 26 % of all soundings as cloud-free. However, this cloud screening strategy can not work for the one-band retrieval because here we restrict ourselves to using only measurements from the 2.06µm band.

Here, we propose a new cloud filter based only on the 2.06µm band to truly investigate the case where the other bands are not available. We first screen by retrieving XCO2 using the whole 2.06µm band under the assumption of a non-scattering atmosphere and divide this by the a priori value derived from the CarbonTracker. When this ratio is <0.96 or >1.04, the scene is considered too cloudy for XCO2 retrieval. Then, we use two sub-spectral windows in the 2.06µm band: one weak absorption window centered around 2.08µm in the spectral range 20782081 nm and one strong absorption window centered around 2.05µm in the spectral range 20422057 nm. The columns of CO2 and H2O are retrieved independently from these two sub-windows under the assumption of a non-scattering atmosphere, and the ratios between the CO2 and H2O columns retrieved from those two sub-windows are used for cloud screening. The idea is similar to three-band cloud filtering in that a large deviation can be introduced to CO2 and H2O columns retrieved from these two bands due to different light path sensitivity . We only use spectra which meet the following criteria:

$\begin{array}{}\text{(2)}& \begin{array}{rl}\mathrm{0.89}<& \frac{{\mathrm{H}}_{\mathrm{2}}\mathrm{O}\left(\mathrm{2.08}\phantom{\rule{0.125em}{0ex}}\mathrm{µ}\mathrm{m}\right)}{{\mathrm{H}}_{\mathrm{2}}\mathrm{O}\left(\mathrm{2.05}\phantom{\rule{0.125em}{0ex}}\mathrm{µ}\mathrm{m}\right)}<\mathrm{1.05}\phantom{\rule{0.25em}{0ex}}\mathrm{and}\phantom{\rule{0.25em}{0ex}}\mathrm{0.98}\\ & <\frac{{\mathrm{CO}}_{\mathrm{2}}\left(\mathrm{2.08}\phantom{\rule{0.125em}{0ex}}\mathrm{µ}\mathrm{m}\right)}{{\mathrm{CO}}_{\mathrm{2}}\left(\mathrm{2.05}\phantom{\rule{0.125em}{0ex}}\mathrm{µ}\mathrm{m}\right)}<\mathrm{1.03}\end{array}.\end{array}$

After the filtering procedure described above, around 27 % of total soundings are considered cloud-free cases, which is similar to what is found by the three-band cloud filter. The one-band cloud filter and the three-band cloud filter have an overlap of 75 %.

Figure 4Error on XCO2 from one-band and three-band OCO-2 land retrievals as a function of aerosol optical thickness (in O2 A band), size parameter, and layer height as retrieved by three-band retrievals. Shown are the mean bias for each parameter bin along with standard deviation within each bin. Background includes the density map of XCO2 errors from one-band retrievals.

Figure 5Histogram of DFS for aerosols, aerosol size parameter, aerosol optical depth, and aerosol layer height in the one-band retrievals.

For cloud-screened soundings, we first run full-physics retrievals and then apply posterior quality filtering based on the criteria shown in Table 2. Those criteria are related to extreme viewing geometry, difficult scattering scenes, challenging surface properties, spectra with larger uncertainties, and poor fit between forward model and measurements. After the quality filtering, the overall throughputs are 17.0 % and 18.0 % for one-band and three-band retrievals, respectively. The two data sets have an overlap of 75 %.

Figure 6XCO2 distributions over the EMEA regions from one-band (a) and three-band (b) retrievals in the time period between 8 September and 31 December 2014. In (c) corresponding XCO2 retrievals from one-band and three-band retrievals are shown with bias (b), standard deviation (σ), and Pearson correlation coefficient (r). Here, a mean bias of 0.88 ppm was subtracted from three-band retrievals.

4 Performance evaluation

Note that in this work, we do not apply a bias correction as it is common practice for CO2 retrievals from space-based observations , but show the uncorrected results because we want to evaluate the true retrieval capability. Due to the high spatial sampling of OCO-2, we typically obtain several collocations of OCO-2 retrievals with individual TCCON measurements for our collocation criteria in a single overpass. To reduce the impact of random and representation errors in our comparison, we compare overpass averages between OCO-2 and TCCON results and use bias (ba), standard deviation of the difference (σa), and station-to-station variability (σs) for performance evaluation . The station-to-station variability is the standard deviation of all biases between the different TCCON sites and is a measure of regional-scale accuracy, which is crucial for flux inversion.

Figure 1 shows validations of one-band XCO2 retrievals over land and ocean. We neglect cases where fewer than 10 individual data points are available in OCO-2 retrievals during one overpass. Here, both land and ocean retrievals exhibit high correlation (around 0.94) with TCCON data, and both have a standard deviation (SD) of ∼1.30 ppm.

To evaluate the one-band and three-band retrieval performance in more detail, Figs. 2 and 3 show the bias and SD of the retrievals per TCCON station. One-band and three-band retrievals have similar bias and SD among most individual stations. One-band retrievals have slightly higher overall SD, which is increased by 0.01 ppm for land retrievals and 0.14 ppm for ocean retrievals. Over land, one-band and three-band retrievals have comparable station-to-station variability of 0.44 and 0.42 ppm, respectively. Over ocean, the one-band retrieval has a station-to-station variability of 0.55 ppm, which is about 0.1 ppm higher than that of the three-band retrieval; however, as shown in Fig. 3 this is mainly caused by larger biases from the Lauder and Ascension stations. The causes for large biases over the two sites are still unclear. However, they are unlikely due to aerosols because non-scattering retrievals exhibit similar biases, and over ocean aerosols should lead to underestimation instead of overestimation .

Table 3 summarizes the overall validation performance of the one-band and three-band retrievals with TCCON measurements. Compared with three-band retrievals, one-band retrievals have similar throughput and similar high correlation coefficients with TCCON. In one-band retrievals, the single sounding precision is 0.16 ppm larger over both land and ocean. In terms of bias, one-band retrievals have a smaller overall bias but a station-to-station variability similar to that of three-band retrievals.

For the general applicability of the one-band retrieval, it is important to know if the performance of the one-band retrievals is more affected by the amount and properties of aerosols than the three-band retrievals. Figure 4 shows one-band and three-band land retrieval differences with respect to TCCON as a function of aerosol optical thickness (AOT) in the O2 A band, size parameter, and layer height as retrieved by the three-band retrievals. With AOT, one-band retrievals show a positive correlation of 0.17 while three-band retrievals present an anticorrelation of −0.11. In both retrievals, the range of errors between AOT =0.01 and AOT =0.30 is around 1.0 ppm. Scattering errors in both retrievals show similar correlations with aerosol size parameter and layer central height. Thus, compared with three-band retrievals, one-band retrievals exhibit a similar dependence on aerosol properties.

On the other hand, as shown in Fig. 5 the DFS for aerosol parameters in the one-band retrieval is mostly well below 1, while for the three-band retrieval it is around 2 in most cases. Aerosol properties as retrieved by the one-band retrievals vary within a small range around the prior values. This triggers the question of whether a non-scattering retrieval would also provide performance similar to that of the one-band “full-physics” retrieval for the cases considered in this study. To investigate this, we also performed a non-scattering retrieval using the 2.06µm band only. The results are summarized in Table 4. It can be seen that the non-scattering retrieval has a much larger bias, and the standard deviation of differences with TCCON and the station-to-station bias are somewhat larger than for the one-band (and three-band) retrieval. The improvement of the one-band retrievals compared to the non-scattering retrievals becomes more clear if we consider the Izana TCCON station close to the Sahara, known as a region with difficult aerosol scenes for XCO2 retrieval. Here, we employ a coarse spatial collocation criteria (16.5< latitude <34.0 and $-\mathrm{16.0}<$ longitude <24.5) for observations made between September 2014 and October 2017, which results in 105 valid retrievals. For this Sahara region, the bias and standard deviation (b, σ) of differences with TCCON for one-band and non-scattering retrievals are (−0.23, 1.49) ppm and (−2.46, 1.93) ppm, respectively.

We conclude that despite the small DFS for aerosol properties in the one-band retrieval, the explicit treatment of aerosols in the one-band retrieval is still important to achieve sufficient accuracy on XCO2, comparable to the three-band retrievals.

To further investigate the validity of the conclusions based on the OCO-2 vs. TCCON comparison, we performed a comparison between one-band and three-band retrievals over a larger region. Here, we perform one-band and three-band XCO2 retrievals over Europe, the Middle East, and Africa (EMEA) for all OCO-2 observations made between 8 September and 31 December 2014. In Fig. 6, one-band and three-band retrievals over the EMEA region show similar data coverage and regional XCO2 variations, for example, low XCO2 values in eastern Europe and enhancement towards the Middle East. Here, one-band and three-band retrievals are highly correlated (r=0.84) with a SD of 0.93 ppm. This indicates that the conclusions drawn above on the similar performance between the one-band and three-band retrievals are not only valid for regions around TCCON stations.

5 Conclusions

The comparison between the performance of one-band XCO2 retrievals from OCO-2 using only the 2.06µm band and the commonly employed three-band retrievals showed that with one band similar accuracy can be achieved as with three bands while the processing time is reduced by 40 %. The most noticeable difference is the slightly increased standard deviation of the differences between OCO-2 and TCCON measurements. We see that leaving out the O2 A band and weak CO2 absorption band has little effect on the station-to-station variability in the XCO2 retrievals. Our results suggest that the O2 A band adds only limited information on aerosols relevant for XCO2 retrievals, confirming earlier results  using simulated OCO measurements. For future missions it may be better to replace the O2 A band with measurements that have larger information content on aerosols, like a multi-angle polarimeter (MAP) .

In order to evaluate the true retrieval capability of the one-band and three-band retrievals, we have not applied any bias corrections in this study. It should be noted though that in general a bias correction is needed and will improve the validation against TCCON. For example, and  have found it necessary to apply, among others, a swath-dependent bias correction.

Data availability
Data availability.

The OCO-2 L1b data (version 8) were provided by the OCO-2 project from the data archive at the NASA Goddard Earth Science Data and Information Services Center (https://doi.org/10.5067/1RJW1YMLW2F0, ). TCCON data were obtained from the TCCON Data Archive (https://tccon-wiki.caltech.edu/, ). The three-band and one-band retrieval results presented in this paper can be found at ftp://ftp.sron.nl/open-access-data/ (last access: 19 November 2019).

Author contributions
Author contributions.

LW, OH, HH, AB, JL, and IA were involved in the research design. LW and OH wrote the paper and carried out the experiments. JB, JL, AB, and IA edited the paper.

Competing interests
Competing interests.

The authors declare that they have no conflict of interest.

Acknowledgements
Acknowledgements.

We wish to thank Robert Roland Nelson and the one anonymous referee for their interest and valuable comments, which have led to several improvements. We also would like to thank the TCCON community for providing measurements used in this study.

Financial support
Financial support.

This research was funded by the Netherlands Space Office as part of the User Support Programme Space Research under project ALW-GO/15-23.

Review statement
Review statement.

This paper was edited by Cheng Liu and reviewed by Robert Roland Nelson and one anonymous referee.

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