A 2-year intercomparison of three methods for measuring black carbon concentration at a high-altitude research station in Europe

Bibliographic Details
Title: A 2-year intercomparison of three methods for measuring black carbon concentration at a high-altitude research station in Europe
Authors: S. Tinorua, C. Denjean, P. Nabat, V. Pont, M. Arnaud, T. Bourrianne, M. Dias Alves, E. Gardrat
Source: Atmospheric Measurement Techniques, Vol 17, Pp 3897-3915 (2024)
Publisher Information: Copernicus Publications, 2024.
Publication Year: 2024
Collection: LCC:Environmental engineering
LCC:Earthwork. Foundations
Subject Terms: Environmental engineering, TA170-171, Earthwork. Foundations, TA715-787
More Details: Black carbon (BC) is one of the most important climate forcers with severe health effects. Large uncertainties in radiative forcing estimation and health impact assessment arise from the fact that there is no standardized method to measure BC mass concentration. This study presents a 2-year comparison of three state-of-the-art BC measurement techniques at the high-altitude research station Pic du Midi (PDM) located in the French Pyrenees at an altitude of 2877 m above sea level. A recently upgraded Aethalometer AE33, a thermal-optical analyser Sunset and a single-particle soot photometer SP2 were deployed to measure simultaneously the mass concentration of equivalent black carbon (MeBC), elemental carbon (MEC) and refractory black carbon (MrBC), respectively. Significant deviations in the response of the instruments were observed. All techniques responded to seasonal variations in the atmospheric changes in BC levels and exhibited good correlation during the whole study period. This indicates that the different instruments quantified the same particle type despite the fact that they are based on different physical principles. However the slopes and correlation coefficients varied between instrument pairs. The largest biases were observed for the AE33 with MeBC values that were around 2 times greater than MrBC and MEC values. The principal reasons of such large discrepancy were explained by the mass absorption cross section (MAC) that was too low and C values recommended by the AE33 manufacturer and applied to the absorption coefficients measured by the AE33. In addition, the long-range transport of dust particles at PDM in spring caused significant increases in the bias between AE33 and SP2 by up to a factor 8. The Sunset MEC measurements agreed within around 17 % with the SP2 MrBC values. The largest overestimations of MEC were observed when the total carbon concentrations were below 25 µg C cm−2, which is probably linked to the incorrect determination of the organic carbon (OC)–EC split point. Another cause of the discrepancy between instruments was found to be the limited detection range of the SP2, which did not allow for the total detection of fine rBC particles. The procedure used to estimate the missing mass fraction of rBC not covered by the measurement range of the SP2 was found to be critical. We found that a time-dependent correction based on fitting the observed rBC size distribution with a multimodal lognormal distribution is needed to accurately estimate MrBC over a larger size range.
Document Type: article
File Description: electronic resource
Language: English
ISSN: 1867-1381
1867-8548
Relation: https://amt.copernicus.org/articles/17/3897/2024/amt-17-3897-2024.pdf; https://doaj.org/toc/1867-1381; https://doaj.org/toc/1867-8548
DOI: 10.5194/amt-17-3897-2024
Access URL: https://doaj.org/article/128d001559fc4fd6beeb794d63b19439
Accession Number: edsdoj.128d001559fc4fd6beeb794d63b19439
Database: Directory of Open Access Journals
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More Details
ISSN:18671381
18678548
DOI:10.5194/amt-17-3897-2024
Published in:Atmospheric Measurement Techniques
Language:English