A potential large and persistent black carbon forcing over Northern Pacific inferred from satellite observations

Black carbon (BC) aerosol strongly absorbs solar radiation, which warms climate. However, accurate estimation of BC’s climate effect is limited by the uncertainties of its spatiotemporal distribution, especially over remote oceanic areas. The HIAPER Pole-to-Pole Observation (HIPPO) program from 2009...

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Detalles Bibliográficos
Autores principales: Li, Zhongshu, Liu, Junfeng, Mauzerall, Denise L., Li, Xiaoyuan, Fan, Songmiao, Horowitz, Larry W., He, Cenlin, Yi, Kan, Tao, Shu
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5339901/
https://www.ncbi.nlm.nih.gov/pubmed/28266532
http://dx.doi.org/10.1038/srep43429

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5339901/
https://www.ncbi.nlm.nih.gov/pubmed/28266532
http://dx.doi.org/10.1038/srep43429

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