Enhanced solar energy absorption by internally-mixed black carbon in snow grains
Here we explore light absorption by snowpack containing black carbon (BC) particles residing within ice grains. Basic considerations of particle volumes and BC/snow mass concentrations show that there are generally 0.05–10 9 BC particles for each ice grain. This suggests that internal BC is likely d...
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ftcopernicus:oai:publications.copernicus.org:acp13981 2023-05-15T18:18:25+02:00 Enhanced solar energy absorption by internally-mixed black carbon in snow grains Flanner, M. G. Liu, X. Zhou, C. Penner, J. E. Jiao, C. 2018-01-15 application/pdf https://doi.org/10.5194/acp-12-4699-2012 https://www.atmos-chem-phys.net/12/4699/2012/ eng eng doi:10.5194/acp-12-4699-2012 https://www.atmos-chem-phys.net/12/4699/2012/ eISSN: 1680-7324 Text 2018 ftcopernicus https://doi.org/10.5194/acp-12-4699-2012 2019-12-24T09:56:16Z Here we explore light absorption by snowpack containing black carbon (BC) particles residing within ice grains. Basic considerations of particle volumes and BC/snow mass concentrations show that there are generally 0.05–10 9 BC particles for each ice grain. This suggests that internal BC is likely distributed as multiple inclusions within ice grains, and thus the dynamic effective medium approximation (DEMA) (Chýlek and Srivastava, 1983) is a more appropriate optical representation for BC/ice composites than coated-sphere or standard mixing approximations. DEMA calculations show that the 460 nm absorption cross-section of BC/ice composites, normalized to the mass of BC, is typically enhanced by factors of 1.8–2.1 relative to interstitial BC. BC effective radius is the dominant cause of variation in this enhancement, compared with ice grain size and BC volume fraction. We apply two atmospheric aerosol models that simulate interstitial and within-hydrometeor BC lifecycles. Although only ~2% of the atmospheric BC burden is cloud-borne, 71–83% of the BC deposited to global snow and sea-ice surfaces occurs within hydrometeors. Key processes responsible for within-snow BC deposition are development of hydrophilic coatings on BC, activation of liquid droplets, and subsequent snow formation through riming or ice nucleation by other species and aggregation/accretion of ice particles. Applying deposition fields from these aerosol models in offline snow and sea-ice simulations, we calculate that 32–73% of BC in global surface snow resides within ice grains. This fraction is smaller than the within-hydrometeor deposition fraction because meltwater flux preferentially removes internal BC, while sublimation and freezing within snowpack expose internal BC. Incorporating the DEMA into a global climate model, we simulate increases in BC/snow radiative forcing of 43–86%, relative to scenarios that apply external optical properties to all BC. We show that snow metamorphism driven by diffusive vapor transfer likely proceeds too slowly to alter the mass of internal BC while it is radiatively active, but neglected processes like wind pumping and convection may play much larger roles. These results suggest that a large portion of BC in surface snowpack may reside within ice grains and increase BC/snow radiative forcing, although measurements to evaluate this are lacking. Finally, previous studies of BC/snow forcing that neglected this absorption enhancement are not necessarily biased low, because of application of absorption-enhancing sulfate coatings to hydrophilic BC, neglect of coincident absorption by dust in snow, and implicit treatment of cloud-borne BC resulting in longer-range transport. Text Sea ice Copernicus Publications: E-Journals Atmospheric Chemistry and Physics 12 10 4699 4721 |
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Copernicus Publications: E-Journals |
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ftcopernicus |
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English |
description |
Here we explore light absorption by snowpack containing black carbon (BC) particles residing within ice grains. Basic considerations of particle volumes and BC/snow mass concentrations show that there are generally 0.05–10 9 BC particles for each ice grain. This suggests that internal BC is likely distributed as multiple inclusions within ice grains, and thus the dynamic effective medium approximation (DEMA) (Chýlek and Srivastava, 1983) is a more appropriate optical representation for BC/ice composites than coated-sphere or standard mixing approximations. DEMA calculations show that the 460 nm absorption cross-section of BC/ice composites, normalized to the mass of BC, is typically enhanced by factors of 1.8–2.1 relative to interstitial BC. BC effective radius is the dominant cause of variation in this enhancement, compared with ice grain size and BC volume fraction. We apply two atmospheric aerosol models that simulate interstitial and within-hydrometeor BC lifecycles. Although only ~2% of the atmospheric BC burden is cloud-borne, 71–83% of the BC deposited to global snow and sea-ice surfaces occurs within hydrometeors. Key processes responsible for within-snow BC deposition are development of hydrophilic coatings on BC, activation of liquid droplets, and subsequent snow formation through riming or ice nucleation by other species and aggregation/accretion of ice particles. Applying deposition fields from these aerosol models in offline snow and sea-ice simulations, we calculate that 32–73% of BC in global surface snow resides within ice grains. This fraction is smaller than the within-hydrometeor deposition fraction because meltwater flux preferentially removes internal BC, while sublimation and freezing within snowpack expose internal BC. Incorporating the DEMA into a global climate model, we simulate increases in BC/snow radiative forcing of 43–86%, relative to scenarios that apply external optical properties to all BC. We show that snow metamorphism driven by diffusive vapor transfer likely proceeds too slowly to alter the mass of internal BC while it is radiatively active, but neglected processes like wind pumping and convection may play much larger roles. These results suggest that a large portion of BC in surface snowpack may reside within ice grains and increase BC/snow radiative forcing, although measurements to evaluate this are lacking. Finally, previous studies of BC/snow forcing that neglected this absorption enhancement are not necessarily biased low, because of application of absorption-enhancing sulfate coatings to hydrophilic BC, neglect of coincident absorption by dust in snow, and implicit treatment of cloud-borne BC resulting in longer-range transport. |
format |
Text |
author |
Flanner, M. G. Liu, X. Zhou, C. Penner, J. E. Jiao, C. |
spellingShingle |
Flanner, M. G. Liu, X. Zhou, C. Penner, J. E. Jiao, C. Enhanced solar energy absorption by internally-mixed black carbon in snow grains |
author_facet |
Flanner, M. G. Liu, X. Zhou, C. Penner, J. E. Jiao, C. |
author_sort |
Flanner, M. G. |
title |
Enhanced solar energy absorption by internally-mixed black carbon in snow grains |
title_short |
Enhanced solar energy absorption by internally-mixed black carbon in snow grains |
title_full |
Enhanced solar energy absorption by internally-mixed black carbon in snow grains |
title_fullStr |
Enhanced solar energy absorption by internally-mixed black carbon in snow grains |
title_full_unstemmed |
Enhanced solar energy absorption by internally-mixed black carbon in snow grains |
title_sort |
enhanced solar energy absorption by internally-mixed black carbon in snow grains |
publishDate |
2018 |
url |
https://doi.org/10.5194/acp-12-4699-2012 https://www.atmos-chem-phys.net/12/4699/2012/ |
genre |
Sea ice |
genre_facet |
Sea ice |
op_source |
eISSN: 1680-7324 |
op_relation |
doi:10.5194/acp-12-4699-2012 https://www.atmos-chem-phys.net/12/4699/2012/ |
op_doi |
https://doi.org/10.5194/acp-12-4699-2012 |
container_title |
Atmospheric Chemistry and Physics |
container_volume |
12 |
container_issue |
10 |
container_start_page |
4699 |
op_container_end_page |
4721 |
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1766194982293602304 |