Intercomparison of CO measurements from TROPOMI, ACE-FTS, and a high-Arctic ground-based Fourier transform spectrometer
The TROPOspheric Monitoring Instrument (TROPOMI) provides a daily, spatially resolved (initially 7×7 km 2 , upgraded to 7×5.6 km 2 in August 2019) global dataset of CO columns; however, due to the relative sparseness of reliable ground-based data sources, it can be challenging to characterize the va...
| Published in: | Atmospheric Measurement Techniques |
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| Main Authors: | , , , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Copernicus Publications
2021
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| Subjects: | |
| Online Access: | https://doi.org/10.5194/amt-14-7707-2021 https://doaj.org/article/ed53f23655d24b5994043c55dac99b39 |
| Summary: | The TROPOspheric Monitoring Instrument (TROPOMI) provides a daily, spatially resolved (initially 7×7 km 2 , upgraded to 7×5.6 km 2 in August 2019) global dataset of CO columns; however, due to the relative sparseness of reliable ground-based data sources, it can be challenging to characterize the validity and accuracy of satellite data products in remote regions such as the high Arctic. In these regions, satellite intercomparisons can supplement model- and ground-based validation efforts and serve to verify previously observed differences. In this paper, we compare the CO products from TROPOMI, the Atmospheric Chemistry Experiment (ACE) Fourier transform spectrometer (FTS), and a high-Arctic ground-based FTS located at the Polar Environment Atmospheric Research Laboratory (PEARL) in Eureka, Nunavut (80.05 ∘ N, 86.42 ∘ W). A global comparison of TROPOMI reference profiles scaled by the retrieved total column with ACE-FTS CO partial columns for the period from 28 November 2017 to 31 May 2020 displays excellent agreement between the two datasets ( R =0.93 ) and a small relative bias of <math xmlns="http://www.w3.org/1998/Math/MathML" id="M8" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>-</mo><mn mathvariant="normal">0.83</mn><mo>±</mo><mn mathvariant="normal">0.26</mn><mspace linebreak="nobreak" width="0.125em"/><mi mathvariant="italic">%</mi></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="75pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="ec2fc91239eaea953aa270178bffcd62"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-14-7707-2021-ie00001.svg" width="75pt" height="10pt" src="amt-14-7707-2021-ie00001.png"/></svg:svg> (bias ± standard error of the mean). Additional comparisons were performed within five latitude bands: the north polar region (60 to 90 ∘ N), northern mid-latitudes (20 to 60 ∘ N), the equatorial region (20 ∘ S to 20 ∘ ... |
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