Mass and Number Size Distributions of rBC in Snow and Firn Samples From Pine Island Glacier, West Antarctica
Abstract An extended‐range Single Particle Soot Photometer (SP2) coupled to a Marin‐5 nebulizer was used to measure the refractory black carbon (rBC) mass and number size distributions in 1,004 samples from a West Antarctica snow/firn core. The SP2 was calibrated using Aquadag and a Centrifugal Part...
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ftdoajarticles:oai:doaj.org/article:55fa32524118432f91ad6b016a03e150 2023-05-15T13:59:54+02:00 Mass and Number Size Distributions of rBC in Snow and Firn Samples From Pine Island Glacier, West Antarctica Luciano Marquetto Susan Kaspari Jefferson Cardia Simões 2020-11-01T00:00:00Z https://doi.org/10.1029/2020EA001198 https://doaj.org/article/55fa32524118432f91ad6b016a03e150 EN eng American Geophysical Union (AGU) https://doi.org/10.1029/2020EA001198 https://doaj.org/toc/2333-5084 2333-5084 doi:10.1029/2020EA001198 https://doaj.org/article/55fa32524118432f91ad6b016a03e150 Earth and Space Science, Vol 7, Iss 11, Pp n/a-n/a (2020) rBC SP2 size distribution snow West Antarctica Astronomy QB1-991 Geology QE1-996.5 article 2020 ftdoajarticles https://doi.org/10.1029/2020EA001198 2022-12-31T05:23:31Z Abstract An extended‐range Single Particle Soot Photometer (SP2) coupled to a Marin‐5 nebulizer was used to measure the refractory black carbon (rBC) mass and number size distributions in 1,004 samples from a West Antarctica snow/firn core. The SP2 was calibrated using Aquadag and a Centrifugal Particle Mass Analyzer for BC particles ranging from 0.5 to 800 fg. Our results indicate a significant contribution of rare, large particles of mass‐equivalent diameter (DBC) > 500 nm to the total rBC mass (36%), while small particles (DBC < 100 nm) are abundant but contribute <8% to total rBC mass. We observed a primary mass median diameter of 162 ± 40 nm, smaller than reported for snow in other regions of the globe but similar to East Antarctica rBC size distributions. In addition, we observed other modes at 673, 1,040, and >1,810 nm (uncontained mode). We compared two sets of samples from different seasons (wet vs. dry) and observed that dry season concentrations are 3.4 and 2 times that of the wet season in the ranges of 80 nm < DBC < 500 nm (small particles) and 500 nm < DBC < 2,000 nm (large particles), respectively, while number of particles in the dry season is 3.5 and 2 times that of the wet season for the same size ranges. Millimeter thick melt layers have been observed in some samples, although they did not change the observed median diameter. This study provides the first detailed rBC mass and number size distribution from West Antarctica. Article in Journal/Newspaper Antarc* Antarctica East Antarctica Pine Island Pine Island Glacier West Antarctica Directory of Open Access Journals: DOAJ Articles East Antarctica West Antarctica Pine Island Glacier ENVELOPE(-101.000,-101.000,-75.000,-75.000) Earth and Space Science 7 11 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
rBC SP2 size distribution snow West Antarctica Astronomy QB1-991 Geology QE1-996.5 |
spellingShingle |
rBC SP2 size distribution snow West Antarctica Astronomy QB1-991 Geology QE1-996.5 Luciano Marquetto Susan Kaspari Jefferson Cardia Simões Mass and Number Size Distributions of rBC in Snow and Firn Samples From Pine Island Glacier, West Antarctica |
topic_facet |
rBC SP2 size distribution snow West Antarctica Astronomy QB1-991 Geology QE1-996.5 |
description |
Abstract An extended‐range Single Particle Soot Photometer (SP2) coupled to a Marin‐5 nebulizer was used to measure the refractory black carbon (rBC) mass and number size distributions in 1,004 samples from a West Antarctica snow/firn core. The SP2 was calibrated using Aquadag and a Centrifugal Particle Mass Analyzer for BC particles ranging from 0.5 to 800 fg. Our results indicate a significant contribution of rare, large particles of mass‐equivalent diameter (DBC) > 500 nm to the total rBC mass (36%), while small particles (DBC < 100 nm) are abundant but contribute <8% to total rBC mass. We observed a primary mass median diameter of 162 ± 40 nm, smaller than reported for snow in other regions of the globe but similar to East Antarctica rBC size distributions. In addition, we observed other modes at 673, 1,040, and >1,810 nm (uncontained mode). We compared two sets of samples from different seasons (wet vs. dry) and observed that dry season concentrations are 3.4 and 2 times that of the wet season in the ranges of 80 nm < DBC < 500 nm (small particles) and 500 nm < DBC < 2,000 nm (large particles), respectively, while number of particles in the dry season is 3.5 and 2 times that of the wet season for the same size ranges. Millimeter thick melt layers have been observed in some samples, although they did not change the observed median diameter. This study provides the first detailed rBC mass and number size distribution from West Antarctica. |
format |
Article in Journal/Newspaper |
author |
Luciano Marquetto Susan Kaspari Jefferson Cardia Simões |
author_facet |
Luciano Marquetto Susan Kaspari Jefferson Cardia Simões |
author_sort |
Luciano Marquetto |
title |
Mass and Number Size Distributions of rBC in Snow and Firn Samples From Pine Island Glacier, West Antarctica |
title_short |
Mass and Number Size Distributions of rBC in Snow and Firn Samples From Pine Island Glacier, West Antarctica |
title_full |
Mass and Number Size Distributions of rBC in Snow and Firn Samples From Pine Island Glacier, West Antarctica |
title_fullStr |
Mass and Number Size Distributions of rBC in Snow and Firn Samples From Pine Island Glacier, West Antarctica |
title_full_unstemmed |
Mass and Number Size Distributions of rBC in Snow and Firn Samples From Pine Island Glacier, West Antarctica |
title_sort |
mass and number size distributions of rbc in snow and firn samples from pine island glacier, west antarctica |
publisher |
American Geophysical Union (AGU) |
publishDate |
2020 |
url |
https://doi.org/10.1029/2020EA001198 https://doaj.org/article/55fa32524118432f91ad6b016a03e150 |
long_lat |
ENVELOPE(-101.000,-101.000,-75.000,-75.000) |
geographic |
East Antarctica West Antarctica Pine Island Glacier |
geographic_facet |
East Antarctica West Antarctica Pine Island Glacier |
genre |
Antarc* Antarctica East Antarctica Pine Island Pine Island Glacier West Antarctica |
genre_facet |
Antarc* Antarctica East Antarctica Pine Island Pine Island Glacier West Antarctica |
op_source |
Earth and Space Science, Vol 7, Iss 11, Pp n/a-n/a (2020) |
op_relation |
https://doi.org/10.1029/2020EA001198 https://doaj.org/toc/2333-5084 2333-5084 doi:10.1029/2020EA001198 https://doaj.org/article/55fa32524118432f91ad6b016a03e150 |
op_doi |
https://doi.org/10.1029/2020EA001198 |
container_title |
Earth and Space Science |
container_volume |
7 |
container_issue |
11 |
_version_ |
1766268829944512512 |