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A twenty-year deposition record of elemental carbon in Northern Japan retrieved from archived filters
The black carbon or elemental carbon (EC) content in ice and snow has been a concern in climate change studies, but time-series records have mostly been obtained from glacier ice-core samples in limited geographical locations, such as the Arctic or high mountains. This is the first study to present...
Autores principales: | , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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Nature Publishing Group UK
2020
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7080725/ https://www.ncbi.nlm.nih.gov/pubmed/32188870 http://dx.doi.org/10.1038/s41598-020-61067-2 |
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author | Kaneyasu, Naoki Matsumoto, Kiyoshi Yamaguchi, Takashi Noguchi, Izumi Murao, Naoto Yasunari, Teppei J. Ikemori, Fumikazu |
author_facet | Kaneyasu, Naoki Matsumoto, Kiyoshi Yamaguchi, Takashi Noguchi, Izumi Murao, Naoto Yasunari, Teppei J. Ikemori, Fumikazu |
author_sort | Kaneyasu, Naoki |
collection | PubMed |
description | The black carbon or elemental carbon (EC) content in ice and snow has been a concern in climate change studies, but time-series records have mostly been obtained from glacier ice-core samples in limited geographical locations, such as the Arctic or high mountains. This is the first study to present decade-long records of EC deposition measured at urban (Sapporo) and background (Rishiri Island) sites in Japan, in the mid-latitude zone of the eastern edge of the Asian continent. By using archived membrane filters from an acid rain study, we retrieved monthly EC deposition records of 1993–2012 in Sapporo and intermittent deposition data in Rishiri. Annual EC deposition showed large fluctuations, with a maximum in 2000–2001 and a minor increase in 2010–2011. This interannual change was moderately related to the deposition of non-sea salt SO(4)(2−) and the collected water volume but did not reflect the estimated emission history of China. High depositions in 2000–2001 were probably caused by the transport of Asian Dust accompanied by air pollutants, which were characteristically active in these years. The findings of this study have implications for the use of observational data in validating global aerosol transport models. |
format | Online Article Text |
id | pubmed-7080725 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2020 |
publisher | Nature Publishing Group UK |
record_format | MEDLINE/PubMed |
spelling | pubmed-70807252020-03-23 A twenty-year deposition record of elemental carbon in Northern Japan retrieved from archived filters Kaneyasu, Naoki Matsumoto, Kiyoshi Yamaguchi, Takashi Noguchi, Izumi Murao, Naoto Yasunari, Teppei J. Ikemori, Fumikazu Sci Rep Article The black carbon or elemental carbon (EC) content in ice and snow has been a concern in climate change studies, but time-series records have mostly been obtained from glacier ice-core samples in limited geographical locations, such as the Arctic or high mountains. This is the first study to present decade-long records of EC deposition measured at urban (Sapporo) and background (Rishiri Island) sites in Japan, in the mid-latitude zone of the eastern edge of the Asian continent. By using archived membrane filters from an acid rain study, we retrieved monthly EC deposition records of 1993–2012 in Sapporo and intermittent deposition data in Rishiri. Annual EC deposition showed large fluctuations, with a maximum in 2000–2001 and a minor increase in 2010–2011. This interannual change was moderately related to the deposition of non-sea salt SO(4)(2−) and the collected water volume but did not reflect the estimated emission history of China. High depositions in 2000–2001 were probably caused by the transport of Asian Dust accompanied by air pollutants, which were characteristically active in these years. The findings of this study have implications for the use of observational data in validating global aerosol transport models. Nature Publishing Group UK 2020-03-18 /pmc/articles/PMC7080725/ /pubmed/32188870 http://dx.doi.org/10.1038/s41598-020-61067-2 Text en © The Author(s) 2020 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. |
spellingShingle | Article Kaneyasu, Naoki Matsumoto, Kiyoshi Yamaguchi, Takashi Noguchi, Izumi Murao, Naoto Yasunari, Teppei J. Ikemori, Fumikazu A twenty-year deposition record of elemental carbon in Northern Japan retrieved from archived filters |
title | A twenty-year deposition record of elemental carbon in Northern Japan retrieved from archived filters |
title_full | A twenty-year deposition record of elemental carbon in Northern Japan retrieved from archived filters |
title_fullStr | A twenty-year deposition record of elemental carbon in Northern Japan retrieved from archived filters |
title_full_unstemmed | A twenty-year deposition record of elemental carbon in Northern Japan retrieved from archived filters |
title_short | A twenty-year deposition record of elemental carbon in Northern Japan retrieved from archived filters |
title_sort | twenty-year deposition record of elemental carbon in northern japan retrieved from archived filters |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7080725/ https://www.ncbi.nlm.nih.gov/pubmed/32188870 http://dx.doi.org/10.1038/s41598-020-61067-2 |
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