Articles | Volume 10, issue 12
Atmos. Meas. Tech., 10, 5039–5062, 2017
https://doi.org/10.5194/amt-10-5039-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Atmos. Meas. Tech., 10, 5039–5062, 2017
https://doi.org/10.5194/amt-10-5039-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
21 Dec 2017
Research article
| 21 Dec 2017
On Aethalometer measurement uncertainties and an instrument correction factor for the Arctic
John Backman et al.
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- Aerosol carbonaceous, elemental and ionic composition variability and origin at the Siberian High Arctic, Cape Baranova M. Manousakas et al. 10.1080/16000889.2020.1803708
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- A single-beam photothermal interferometer for in situ measurements of aerosol light absorption B. Visser et al. 10.5194/amt-13-7097-2020
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- Influence of Biogenic Organics on the Chemical Composition of Arctic Aerosols J. Choi et al. 10.1029/2019GB006226
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- Effects of mixing state on optical and radiative properties of black carbon in the European Arctic M. Zanatta et al. 10.5194/acp-18-14037-2018
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Latest update: 08 Aug 2022
Short summary
Light absorption by aerosol particles is of climatic importance. A widely used means to measure aerosol light absorption is a filter-based measurement technique. In remote areas, such as the Arctic, filter-based instruments operate close to their detection limit. The study presents how a lower detection limit can be achieved for one such instrument, the Aethalometer. Additionally, the Aethalometer is compared to similar instruments, thus improving measurement inter-comparability in the Arctic.
Light absorption by aerosol particles is of climatic importance. A widely used means to measure...
