Black carbon in the Southern Andean snowpack

Research output: Contribution to journalArticleResearchpeer review

Authors

  • Raúl R. Cordero
  • Edgardo Sepúlveda
  • Sarah Feron
  • Chenghao Wang
  • Alessandro Damiani
  • Francisco Fernandoy
  • Steven Neshyba
  • Penny M. Rowe
  • Valentina Asencio
  • Jorge Carrasco
  • Juan A. Alfonso
  • Shelley MacDonell
  • Gunther Seckmeyer
  • Juan M. Carrera
  • Jose Jorquera
  • Pedro Llanillo
  • Jacob Dana
  • Alia L. Khan
  • Gino Casassa

External Research Organisations

  • Universidad de Santiago de Chile
  • University of Groningen
  • Stanford University
  • Chiba University
  • Universidad Andres Bello
  • University of Puget Sound
  • NorthWest Research Associates, Inc.
  • Select Carbon Pty Ltd
  • UNIVERSIDAD DE MAGALLANES
  • Instituto Venezolano de Investigaciones Cientificas
  • Centro de Estudios Avanzados en Zonas Áridas (CEAZA)
  • Alfred Wegener Institute (AWI) Helmholtz Centre for Polar and Marine Research
  • Western Washington University
  • University of Colorado Boulder
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Details

Original languageEnglish
Article number044042
Number of pages10
JournalEnvironmental research letters
Volume17
Issue number4
Early online date25 Mar 2022
Publication statusPublished - Mar 2022

Abstract

The Andean snowpack is an important source of water for many communities. As other snow-covered regions around the world, the Andes are sensitive to black carbon (BC) deposition from fossil fuel and biomass combustion. BC darkens the snow surface, reduces the albedo, and accelerates melting. Here, we report on measurements of the BC content conducted by using the meltwater filtration (MF) technique in snow samples collected across a transect of more than 2500 km from the mid-latitude Andes to the southern tip of South America. Addressing some of the key knowledge gaps regarding the effects of the BC deposition on the Andean snow, we identified BC-impacted areas, assessed the BC-related albedo reduction, and estimated the resulting snow losses. We found that BC concentrations in our samples generally ranged from 2 to 15 ng g-1, except for the nearly BC-free Patagonian Icefields and for the BC-impacted sites nearby Santiago (a metropolis of 6 million inhabitants). We estimate that the seasonal snowpack shrinking attributable to the BC deposition ranges from 4 mm water equivalent (w.e.) at relatively clean sites in Patagonia to 241 mm w.e. at heavily impacted sites close to Santiago.

Cite this

Black carbon in the Southern Andean snowpack. / Cordero, Raúl R.; Sepúlveda, Edgardo; Feron, Sarah et al.
In: Environmental research letters, Vol. 17, No. 4, 044042, 03.2022.

Research output: Contribution to journalArticleResearchpeer review

Cordero, RR, Sepúlveda, E, Feron, S, Wang, C, Damiani, A, Fernandoy, F, Neshyba, S, Rowe, PM, Asencio, V, Carrasco, J, Alfonso, JA, MacDonell, S, Seckmeyer, G, Carrera, JM, Jorquera, J, Llanillo, P, Dana, J, Khan, AL & Casassa, G 2022, 'Black carbon in the Southern Andean snowpack', Environmental research letters, vol. 17, no. 4, 044042. https://doi.org/10.1088/1748-9326/ac5df0
Cordero, R. R., Sepúlveda, E., Feron, S., Wang, C., Damiani, A., Fernandoy, F., Neshyba, S., Rowe, P. M., Asencio, V., Carrasco, J., Alfonso, J. A., MacDonell, S., Seckmeyer, G., Carrera, J. M., Jorquera, J., Llanillo, P., Dana, J., Khan, A. L., & Casassa, G. (2022). Black carbon in the Southern Andean snowpack. Environmental research letters, 17(4), Article 044042. https://doi.org/10.1088/1748-9326/ac5df0
Cordero RR, Sepúlveda E, Feron S, Wang C, Damiani A, Fernandoy F et al. Black carbon in the Southern Andean snowpack. Environmental research letters. 2022 Mar;17(4):044042. Epub 2022 Mar 25. doi: 10.1088/1748-9326/ac5df0
Cordero, Raúl R. ; Sepúlveda, Edgardo ; Feron, Sarah et al. / Black carbon in the Southern Andean snowpack. In: Environmental research letters. 2022 ; Vol. 17, No. 4.
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title = "Black carbon in the Southern Andean snowpack",
abstract = "The Andean snowpack is an important source of water for many communities. As other snow-covered regions around the world, the Andes are sensitive to black carbon (BC) deposition from fossil fuel and biomass combustion. BC darkens the snow surface, reduces the albedo, and accelerates melting. Here, we report on measurements of the BC content conducted by using the meltwater filtration (MF) technique in snow samples collected across a transect of more than 2500 km from the mid-latitude Andes to the southern tip of South America. Addressing some of the key knowledge gaps regarding the effects of the BC deposition on the Andean snow, we identified BC-impacted areas, assessed the BC-related albedo reduction, and estimated the resulting snow losses. We found that BC concentrations in our samples generally ranged from 2 to 15 ng g-1, except for the nearly BC-free Patagonian Icefields and for the BC-impacted sites nearby Santiago (a metropolis of 6 million inhabitants). We estimate that the seasonal snowpack shrinking attributable to the BC deposition ranges from 4 mm water equivalent (w.e.) at relatively clean sites in Patagonia to 241 mm w.e. at heavily impacted sites close to Santiago. ",
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AU - Cordero, Raúl R.

AU - Sepúlveda, Edgardo

AU - Feron, Sarah

AU - Wang, Chenghao

AU - Damiani, Alessandro

AU - Fernandoy, Francisco

AU - Neshyba, Steven

AU - Rowe, Penny M.

AU - Asencio, Valentina

AU - Carrasco, Jorge

AU - Alfonso, Juan A.

AU - MacDonell, Shelley

AU - Seckmeyer, Gunther

AU - Carrera, Juan M.

AU - Jorquera, Jose

AU - Llanillo, Pedro

AU - Dana, Jacob

AU - Khan, Alia L.

AU - Casassa, Gino

N1 - Funding Information: The support of ANID (ANILLO ACT210046, FONDECYT 1191932, DFG190004 and REDES180158), and CORFO (Preis 19BP-117358, 18BPE-93920 and 18BPCR-89100) is gratefully acknowledged. A L K’s contribution was supported by a Fulbright Scholarship to the Chilean Antarctic Program.

PY - 2022/3

Y1 - 2022/3

N2 - The Andean snowpack is an important source of water for many communities. As other snow-covered regions around the world, the Andes are sensitive to black carbon (BC) deposition from fossil fuel and biomass combustion. BC darkens the snow surface, reduces the albedo, and accelerates melting. Here, we report on measurements of the BC content conducted by using the meltwater filtration (MF) technique in snow samples collected across a transect of more than 2500 km from the mid-latitude Andes to the southern tip of South America. Addressing some of the key knowledge gaps regarding the effects of the BC deposition on the Andean snow, we identified BC-impacted areas, assessed the BC-related albedo reduction, and estimated the resulting snow losses. We found that BC concentrations in our samples generally ranged from 2 to 15 ng g-1, except for the nearly BC-free Patagonian Icefields and for the BC-impacted sites nearby Santiago (a metropolis of 6 million inhabitants). We estimate that the seasonal snowpack shrinking attributable to the BC deposition ranges from 4 mm water equivalent (w.e.) at relatively clean sites in Patagonia to 241 mm w.e. at heavily impacted sites close to Santiago.

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