Abstract

Abstract. Seasonal CO2 exchange in the boreal forest plays an important role in the global carbon budget and in driving interannual variability in seasonal cycles of atmospheric CO2. Satellite-based observations from polar orbiting satellites like the Orbiting Carbon Observatory-2 (OCO-2) offer an opportunity to characterize boreal forest seasonal cycles across longitudes with a spatially and temporally rich data set, but data quality controls and biases still require vetting at high latitudes. With the objective of improving data availability at northern, terrestrial high latitudes, this study evaluates quality control methods and biases of OCO-2 retrievals of atmospheric column-averaged dry air mole fractions of CO2 (XCO2) in boreal forest regions. In addition to the standard quality control (QC) filters recommended for the Atmospheric Carbon Observations from Space (ACOS) B8 (B8 QC) and ACOS B9 (B9 QC) OCO-2 retrievals, a third set of quality control filters were specifically tailored to boreal forest observations (boreal QC) with the goal of increasing data availability at high latitudes without sacrificing data quality. Ground-based reference measurements of XCO2 include observations from two sites in the Total Carbon Column Observing Network (TCCON) at East Trout Lake, Saskatchewan, Canada, and Sodankylä, Finland. OCO-2 retrievals were also compared to ground-based observations from two Bruker EM27/SUN Fourier transform infrared spectrometers (FTSs) at Fairbanks, Alaska, USA. The EM27/SUN spectrometers that were deployed in Fairbanks were carefully monitored for instrument performance and were bias corrected to TCCON using observations at the Caltech TCCON site. The B9 QC were found to pass approximately twice as many OCO-2 retrievals over land north of 50∘ N than the B8 QC, and the boreal QC were found to pass approximately twice as many retrievals in May, August, and September as the B9 QC. While boreal QC results in a substantial increase in passable retrievals, this is accompanied by increases in the standard deviations in biases at boreal forest sites from ∼1.4 parts per million (ppm) with B9 QC to ∼1.6 ppm with boreal QC. Total average biases for coincident OCO-2 retrievals at the three sites considered did not consistently increase or decrease with different QC methods, and instead, responses to changes in QC varied according to site and satellite viewing geometries. Regardless of the quality control method used, seasonal variability in biases was observed, and this variability was more pronounced at Sodankylä and East Trout Lake than at Fairbanks. Long-term coincident observations from TCCON, EM27/SUN, and satellites from multiple locations would be necessary to determine whether the reduced seasonal variability in bias at Fairbanks is due to geography or instrumentation. Monthly average biases generally varied between −1 and +1 ppm at the three sites considered, with more negative biases in spring (March, April, and May – MAM) and autumn (September and October – SO) but more positive biases in the summer months (June, July, and August – JJA). Monthly standard deviations in biases ranged from approximately 1.0 to 2.0 ppm and did not exhibit strong seasonal dependence, apart from exceptionally high standard deviation observed with all three QC methods at Sodankylä in June. There was no evidence found to suggest that seasonal variability in bias is a direct result of air mass dependence in ground-based retrievals or of proximity bias from coincidence criteria, but there were a number of retrieval parameters used as quality control filters that exhibit seasonality and could contribute to seasonal dependence in OCO-2 bias. Furthermore, it was found that OCO-2 retrievals of XCO2 without the standard OCO-2 bias correction exhibit almost no perceptible seasonal dependence in average monthly bias at these boreal forest sites, suggesting that seasonal variability in bias is introduced by the bias correction. Overall, we found that modified quality controls can allow for significant increases in passable OCO-2 retrievals with only marginal compromises in data quality, but seasonal dependence in biases still warrants further exploration.

Highlights

  • The boreal forest or taiga biome is the largest terrestrial biome on Earth; it includes the sub-Arctic regions of Europe, Asia, and North America between 50 and 70◦ N latitude, it represents an important and influential component of the global carbon cycle, and it is a principle driver of the atmospheric carbon dioxide (CO2) seasonal cycle

  • Two of these three sets of quality control (QC) filters are recommended by the OCO science team for Atmospheric Carbon Observations from Space (ACOS) B8 retrievals (B8 QC) and ACOS B9 retrievals (B9 QC) and are summarized by the binary variables xco2_quality_flag_b8 and xco2_quality_flag in the Orbiting Carbon Observatory-2 (OCO-2) B9 Lite files (Osterman et al, 2018; O’Dell et al, 2018)

  • Through instrument line shape (ILS) testing of EM27/SUN Fourier transform infrared spectrometers (FTSs) used in Alaska, regular comparisons between multiple EM27/SUN FTS, and comparisons of EM27/SUN FTS with Total Carbon Column Observing Network (TCCON), we established the relative equivalence of EM27/SUN and TCCON observations as ground-based references for OCO-2 validation

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Summary

Introduction

The boreal forest or taiga biome is the largest terrestrial biome on Earth; it includes the sub-Arctic regions of Europe, Asia, and North America between 50 and 70◦ N latitude, it represents an important and influential component of the global carbon cycle, and it is a principle driver of the atmospheric carbon dioxide (CO2) seasonal cycle. Studies by Graven et al (2013) and Barlow et al (2015) used a combination of atmospheric modeling, aircraft observations, and a network of ground-based in situ observations to investigate seasonal carbon exchange in the boreal forest. It remains difficult to reconcile conflicting claims about contributions to the global carbon budget without a spatially and temporally rich set of measurements for high-latitude regions, and data availability in the boreal forest remains a major impediment to accurately quantifying uptake in the world’s largest terrestrial biome (Pan et al, 2011; Barlow et al, 2015; Euskirchen et al, 2017). Methods of expanding observational coverage through improved satellite observations at high latitudes are essential for clarifying our understanding of global CO2 exchange

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