Opposite Effects of Mineral Dust Nonsphericity and Size on Dust‐Induced Snow Albedo Reduction

Abstract We quantified the combined effects of mineral dust nonsphericity and size on snow albedo reduction using the MOPSMAP (Modeled optical properties of ensembles of aerosol particles) package and SAMDS (Spectral Albedo Model for Dirty Snow) with the consideration of dust from Sahara, Greenland,...

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Main Authors: Tenglong Shi, Cenlin He, Daizhou Zhang, Xuelei Zhang, Xiaoying Niu, Yuxuan Xing, Yang Chen, Jiecan Cui, Wei Pu, Xin Wang
Format: Article
Language:English
Published: Wiley 2022-06-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2022GL099031
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author Tenglong Shi
Cenlin He
Daizhou Zhang
Xuelei Zhang
Xiaoying Niu
Yuxuan Xing
Yang Chen
Jiecan Cui
Wei Pu
Xin Wang
author_facet Tenglong Shi
Cenlin He
Daizhou Zhang
Xuelei Zhang
Xiaoying Niu
Yuxuan Xing
Yang Chen
Jiecan Cui
Wei Pu
Xin Wang
author_sort Tenglong Shi
collection DOAJ
description Abstract We quantified the combined effects of mineral dust nonsphericity and size on snow albedo reduction using the MOPSMAP (Modeled optical properties of ensembles of aerosol particles) package and SAMDS (Spectral Albedo Model for Dirty Snow) with the consideration of dust from Sahara, Greenland, San Juan Mountains, and Tibetan Plateau. Results indicate that the dust‐induced albedo reduction decreases by up to 30% as the effective radii of dust particles increase in 1–5 μm. Nonspherical dust enhances snow albedo reduction relative to spherical dust by up to 20%. Stronger enhancements are obtained for higher dust concentration and larger dust size. Furthermore, the dust nonsphericity‐induced enhancement of snow albedo reduction is more pronounced for more‐absorptive dust. Finally, we develop a new parameterization for quantifying the dependence of snow albedo reduction on dust nonsphericity and size, and provide a convenient way for assessing the climate impacts of dust in snow.
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institution Kabale University
issn 0094-8276
1944-8007
language English
publishDate 2022-06-01
publisher Wiley
record_format Article
series Geophysical Research Letters
spelling doaj-art-a93216b2c756417b8317d884df8bdf002025-01-22T14:38:16ZengWileyGeophysical Research Letters0094-82761944-80072022-06-014912n/an/a10.1029/2022GL099031Opposite Effects of Mineral Dust Nonsphericity and Size on Dust‐Induced Snow Albedo ReductionTenglong Shi0Cenlin He1Daizhou Zhang2Xuelei Zhang3Xiaoying Niu4Yuxuan Xing5Yang Chen6Jiecan Cui7Wei Pu8Xin Wang9Key Laboratory for Semi‐Arid Climate Change of the Ministry of Education College of Atmospheric Sciences Lanzhou University Lanzhou ChinaResearch Applications Laboratory National Center for Atmospheric Research Boulder CO USAFaculty of Environmental and Symbiotic Sciences Prefectural University of Kumamoto Kumamoto JapanKey laboratory of Wetland Ecology and Environment Northeast Institute of Geography and Agroecology Chinese Academy of Sciences Changchun ChinaKey Laboratory for Semi‐Arid Climate Change of the Ministry of Education College of Atmospheric Sciences Lanzhou University Lanzhou ChinaKey Laboratory for Semi‐Arid Climate Change of the Ministry of Education College of Atmospheric Sciences Lanzhou University Lanzhou ChinaKey Laboratory for Semi‐Arid Climate Change of the Ministry of Education College of Atmospheric Sciences Lanzhou University Lanzhou ChinaKey Laboratory for Semi‐Arid Climate Change of the Ministry of Education College of Atmospheric Sciences Lanzhou University Lanzhou ChinaKey Laboratory for Semi‐Arid Climate Change of the Ministry of Education College of Atmospheric Sciences Lanzhou University Lanzhou ChinaKey Laboratory for Semi‐Arid Climate Change of the Ministry of Education College of Atmospheric Sciences Lanzhou University Lanzhou ChinaAbstract We quantified the combined effects of mineral dust nonsphericity and size on snow albedo reduction using the MOPSMAP (Modeled optical properties of ensembles of aerosol particles) package and SAMDS (Spectral Albedo Model for Dirty Snow) with the consideration of dust from Sahara, Greenland, San Juan Mountains, and Tibetan Plateau. Results indicate that the dust‐induced albedo reduction decreases by up to 30% as the effective radii of dust particles increase in 1–5 μm. Nonspherical dust enhances snow albedo reduction relative to spherical dust by up to 20%. Stronger enhancements are obtained for higher dust concentration and larger dust size. Furthermore, the dust nonsphericity‐induced enhancement of snow albedo reduction is more pronounced for more‐absorptive dust. Finally, we develop a new parameterization for quantifying the dependence of snow albedo reduction on dust nonsphericity and size, and provide a convenient way for assessing the climate impacts of dust in snow.https://doi.org/10.1029/2022GL099031dust radiusdust shapedust typesnow albedoparameterization
spellingShingle Tenglong Shi
Cenlin He
Daizhou Zhang
Xuelei Zhang
Xiaoying Niu
Yuxuan Xing
Yang Chen
Jiecan Cui
Wei Pu
Xin Wang
Opposite Effects of Mineral Dust Nonsphericity and Size on Dust‐Induced Snow Albedo Reduction
Geophysical Research Letters
dust radius
dust shape
dust type
snow albedo
parameterization
title Opposite Effects of Mineral Dust Nonsphericity and Size on Dust‐Induced Snow Albedo Reduction
title_full Opposite Effects of Mineral Dust Nonsphericity and Size on Dust‐Induced Snow Albedo Reduction
title_fullStr Opposite Effects of Mineral Dust Nonsphericity and Size on Dust‐Induced Snow Albedo Reduction
title_full_unstemmed Opposite Effects of Mineral Dust Nonsphericity and Size on Dust‐Induced Snow Albedo Reduction
title_short Opposite Effects of Mineral Dust Nonsphericity and Size on Dust‐Induced Snow Albedo Reduction
title_sort opposite effects of mineral dust nonsphericity and size on dust induced snow albedo reduction
topic dust radius
dust shape
dust type
snow albedo
parameterization
url https://doi.org/10.1029/2022GL099031
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