The importance of the representation of air pollution emissions for the modeled distribution and radiative effects of black carbon in the Arctic
Aerosol particles can contribute to the Arctic amplification (AA) by direct and indirect radiative effects. Specifically, black carbon (BC) in the atmosphere, and when deposited on snow and sea ice, has a positive warming effect on the top-of-atmosphere (TOA) radiation balance during the polar day....
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2019
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ftdatacite:10.34657/6021 2023-05-15T13:11:21+02:00 The importance of the representation of air pollution emissions for the modeled distribution and radiative effects of black carbon in the Arctic Schacht, Jacob Heinold, Bernd Quaas, Johannes Backman, John Cherian, Ribu Ehrlich, Andre Herber, Andreas Huang, Wan Ting Katty Kondo, Yutaka Massling, Andreas Sinha, P.R. Weinzierl, Bernadett Zanatta, Marco Tegen, Ina 2019 https://dx.doi.org/10.34657/6021 https://oa.tib.eu/renate/handle/123456789/6974 unknown Katlenburg-Lindau : EGU Creative Commons Attribution 4.0 International CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Global warming Arctic amplification AA black carbon BC top-of-atmosphere TOA aerosol particle 550 CreativeWork article 2019 ftdatacite https://doi.org/10.34657/6021 2022-03-10T12:44:35Z Aerosol particles can contribute to the Arctic amplification (AA) by direct and indirect radiative effects. Specifically, black carbon (BC) in the atmosphere, and when deposited on snow and sea ice, has a positive warming effect on the top-of-atmosphere (TOA) radiation balance during the polar day. Current climate models, however, are still struggling to reproduce Arctic aerosol conditions.We present an evaluation study with the global aerosol-climate model ECHAM6.3-HAM2.3 to examine emission-related uncertainties in the BC distribution and the direct radiative effect of BC. The model results are comprehensively compared against the latest ground and airborne aerosol observations for the period 2005-2017, with a focus on BC. Four different setups of air pollution emissions are tested. The simulations in general match well with the observed amount and temporal variability in near-surface BC in the Arctic. Using actual daily instead of fixed biomass burning emissions is crucial for reproducing individual pollution events but has only a small influence on the seasonal cycle of BC. Compared with commonly used fixed anthropogenic emissions for the year 2000, an up-to-date inventory with transient air pollution emissions results in up to a 30% higher annual BC burden locally. This causes a higher annual mean all-sky net direct radiative effect of BC of over 0.1Wm-2 at the top of the atmosphere over the Arctic region (60-90° N), being locally more than 0.2Wm-2 over the eastern Arctic Ocean. We estimate BC in the Arctic as leading to an annual net gain of 0.5Wm-2 averaged over the Arctic region but to a local gain of up to 0.8Wm-2 by the direct radiative effect of atmospheric BC plus the effect by the BC-in-snow albedo reduction. Long-range transport is identified as one of the main sources of uncertainties for ECHAM6.3-HAM2.3, leading to an overestimation of BC in atmospheric layers above 500 hPa, especially in summer. This is related to a misrepresentation in wet removal in one identified case at least, which was observed during the ARCTAS (Arctic Research of the Composition of the Troposphere from Aircraft and Satellites) summer aircraft campaign. Overall, the current model version has significantly improved since previous intercomparison studies and now performs better than the multi-model average in the Aerosol Comparisons between Observation and Models (AEROCOM) initiative in terms of the spatial and temporal distribution of Arctic BC. © Author(s) 2019. Article in Journal/Newspaper albedo Arctic Arctic Ocean black carbon Global warming Sea ice DataCite Metadata Store (German National Library of Science and Technology) Arctic Arctic Ocean |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Global warming Arctic amplification AA black carbon BC top-of-atmosphere TOA aerosol particle 550 |
spellingShingle |
Global warming Arctic amplification AA black carbon BC top-of-atmosphere TOA aerosol particle 550 Schacht, Jacob Heinold, Bernd Quaas, Johannes Backman, John Cherian, Ribu Ehrlich, Andre Herber, Andreas Huang, Wan Ting Katty Kondo, Yutaka Massling, Andreas Sinha, P.R. Weinzierl, Bernadett Zanatta, Marco Tegen, Ina The importance of the representation of air pollution emissions for the modeled distribution and radiative effects of black carbon in the Arctic |
topic_facet |
Global warming Arctic amplification AA black carbon BC top-of-atmosphere TOA aerosol particle 550 |
description |
Aerosol particles can contribute to the Arctic amplification (AA) by direct and indirect radiative effects. Specifically, black carbon (BC) in the atmosphere, and when deposited on snow and sea ice, has a positive warming effect on the top-of-atmosphere (TOA) radiation balance during the polar day. Current climate models, however, are still struggling to reproduce Arctic aerosol conditions.We present an evaluation study with the global aerosol-climate model ECHAM6.3-HAM2.3 to examine emission-related uncertainties in the BC distribution and the direct radiative effect of BC. The model results are comprehensively compared against the latest ground and airborne aerosol observations for the period 2005-2017, with a focus on BC. Four different setups of air pollution emissions are tested. The simulations in general match well with the observed amount and temporal variability in near-surface BC in the Arctic. Using actual daily instead of fixed biomass burning emissions is crucial for reproducing individual pollution events but has only a small influence on the seasonal cycle of BC. Compared with commonly used fixed anthropogenic emissions for the year 2000, an up-to-date inventory with transient air pollution emissions results in up to a 30% higher annual BC burden locally. This causes a higher annual mean all-sky net direct radiative effect of BC of over 0.1Wm-2 at the top of the atmosphere over the Arctic region (60-90° N), being locally more than 0.2Wm-2 over the eastern Arctic Ocean. We estimate BC in the Arctic as leading to an annual net gain of 0.5Wm-2 averaged over the Arctic region but to a local gain of up to 0.8Wm-2 by the direct radiative effect of atmospheric BC plus the effect by the BC-in-snow albedo reduction. Long-range transport is identified as one of the main sources of uncertainties for ECHAM6.3-HAM2.3, leading to an overestimation of BC in atmospheric layers above 500 hPa, especially in summer. This is related to a misrepresentation in wet removal in one identified case at least, which was observed during the ARCTAS (Arctic Research of the Composition of the Troposphere from Aircraft and Satellites) summer aircraft campaign. Overall, the current model version has significantly improved since previous intercomparison studies and now performs better than the multi-model average in the Aerosol Comparisons between Observation and Models (AEROCOM) initiative in terms of the spatial and temporal distribution of Arctic BC. © Author(s) 2019. |
format |
Article in Journal/Newspaper |
author |
Schacht, Jacob Heinold, Bernd Quaas, Johannes Backman, John Cherian, Ribu Ehrlich, Andre Herber, Andreas Huang, Wan Ting Katty Kondo, Yutaka Massling, Andreas Sinha, P.R. Weinzierl, Bernadett Zanatta, Marco Tegen, Ina |
author_facet |
Schacht, Jacob Heinold, Bernd Quaas, Johannes Backman, John Cherian, Ribu Ehrlich, Andre Herber, Andreas Huang, Wan Ting Katty Kondo, Yutaka Massling, Andreas Sinha, P.R. Weinzierl, Bernadett Zanatta, Marco Tegen, Ina |
author_sort |
Schacht, Jacob |
title |
The importance of the representation of air pollution emissions for the modeled distribution and radiative effects of black carbon in the Arctic |
title_short |
The importance of the representation of air pollution emissions for the modeled distribution and radiative effects of black carbon in the Arctic |
title_full |
The importance of the representation of air pollution emissions for the modeled distribution and radiative effects of black carbon in the Arctic |
title_fullStr |
The importance of the representation of air pollution emissions for the modeled distribution and radiative effects of black carbon in the Arctic |
title_full_unstemmed |
The importance of the representation of air pollution emissions for the modeled distribution and radiative effects of black carbon in the Arctic |
title_sort |
importance of the representation of air pollution emissions for the modeled distribution and radiative effects of black carbon in the arctic |
publisher |
Katlenburg-Lindau : EGU |
publishDate |
2019 |
url |
https://dx.doi.org/10.34657/6021 https://oa.tib.eu/renate/handle/123456789/6974 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
albedo Arctic Arctic Ocean black carbon Global warming Sea ice |
genre_facet |
albedo Arctic Arctic Ocean black carbon Global warming Sea ice |
op_rights |
Creative Commons Attribution 4.0 International CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.34657/6021 |
_version_ |
1766247015696564224 |