Effect of snow grain shape and impurities on snow albedo and its parameterization: China, North America, and the Arctic
Thesis (Ph.D.)--University of Washington, 2017-03 Snow cover is important for Earth’s surface energy budget, primarily because the surface reflectance (albedo) is greatly increased if covered by a layer of snow. A correct estimation of snow albedo is therefore crucial for studying climate and snow h...
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ftunivwashington:oai:digital.lib.washington.edu:1773/38572 2023-05-15T13:10:43+02:00 Effect of snow grain shape and impurities on snow albedo and its parameterization: China, North America, and the Arctic Dang, Cheng Warren, Stephen G Fu, Qiang 2017-03 application/pdf http://hdl.handle.net/1773/38572 en_US eng Dang_washington_0250E_13163.pdf http://hdl.handle.net/1773/38572 CC BY-NC-ND Albedo Light-absorbing particles Parameterization Snow Snow grain shape Atmospheric sciences Thesis 2017 ftunivwashington 2023-03-12T18:57:01Z Thesis (Ph.D.)--University of Washington, 2017-03 Snow cover is important for Earth’s surface energy budget, primarily because the surface reflectance (albedo) is greatly increased if covered by a layer of snow. A correct estimation of snow albedo is therefore crucial for studying climate and snow hydrology. Snow albedo is influenced by many factors including snow depth, snow grain size, solar zenith angle, cloud cover, and light-absorbing particles (LAPs, black carbon, organic carbon, and mineral dust) in snow, and snow albedo is usually obtained from radiative transfer calculations. Therefore, an error in those factors and assumptions used in radiative transfer calculations could introduce errors in the computed snow albedo. This dissertation presents three separate works related to snow albedo, aiming towards a better understanding and quantification on the impact of different factors on snow albedo. First, a new parameterization method for narrowband and broadband albedo of pure snow and snow containing black carbon and mineral dust is introduced. Spectral albedo of snowpacks with different grain radii (5 – 2500 μm), containing a wide range of black carbon or mineral dust amounts (mixing ratio of 0 to 1) were calculated using radiative transfer models (DISORT). For each case, three broadband albedos (visible, near-IR, and all-wave) and twelve narrowband albedos (RRTM bands 2-13) are calculated and parameterized as functions of snow grain radius and LAP concentrations. This method can be incorporated into climate models to calculate snow albedo or study the impact of LAPs on snow albedo. Second, the effect of snow grain shape on snow albedo is studied. Radiative transfer calculations on snow albedo have usually assumed a spherical shape for snow grains, using Mie theory to calculate the single-scattering properties of ice spheres. The scattering by more realistic non-spherical grains is less in the forward direction and more to the sides. Incident sunlight scattered in the forward direction travels a longer ... Thesis albedo Arctic black carbon University of Washington, Seattle: ResearchWorks Arctic |
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Open Polar |
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University of Washington, Seattle: ResearchWorks |
op_collection_id |
ftunivwashington |
language |
English |
topic |
Albedo Light-absorbing particles Parameterization Snow Snow grain shape Atmospheric sciences |
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Albedo Light-absorbing particles Parameterization Snow Snow grain shape Atmospheric sciences Dang, Cheng Effect of snow grain shape and impurities on snow albedo and its parameterization: China, North America, and the Arctic |
topic_facet |
Albedo Light-absorbing particles Parameterization Snow Snow grain shape Atmospheric sciences |
description |
Thesis (Ph.D.)--University of Washington, 2017-03 Snow cover is important for Earth’s surface energy budget, primarily because the surface reflectance (albedo) is greatly increased if covered by a layer of snow. A correct estimation of snow albedo is therefore crucial for studying climate and snow hydrology. Snow albedo is influenced by many factors including snow depth, snow grain size, solar zenith angle, cloud cover, and light-absorbing particles (LAPs, black carbon, organic carbon, and mineral dust) in snow, and snow albedo is usually obtained from radiative transfer calculations. Therefore, an error in those factors and assumptions used in radiative transfer calculations could introduce errors in the computed snow albedo. This dissertation presents three separate works related to snow albedo, aiming towards a better understanding and quantification on the impact of different factors on snow albedo. First, a new parameterization method for narrowband and broadband albedo of pure snow and snow containing black carbon and mineral dust is introduced. Spectral albedo of snowpacks with different grain radii (5 – 2500 μm), containing a wide range of black carbon or mineral dust amounts (mixing ratio of 0 to 1) were calculated using radiative transfer models (DISORT). For each case, three broadband albedos (visible, near-IR, and all-wave) and twelve narrowband albedos (RRTM bands 2-13) are calculated and parameterized as functions of snow grain radius and LAP concentrations. This method can be incorporated into climate models to calculate snow albedo or study the impact of LAPs on snow albedo. Second, the effect of snow grain shape on snow albedo is studied. Radiative transfer calculations on snow albedo have usually assumed a spherical shape for snow grains, using Mie theory to calculate the single-scattering properties of ice spheres. The scattering by more realistic non-spherical grains is less in the forward direction and more to the sides. Incident sunlight scattered in the forward direction travels a longer ... |
author2 |
Warren, Stephen G Fu, Qiang |
format |
Thesis |
author |
Dang, Cheng |
author_facet |
Dang, Cheng |
author_sort |
Dang, Cheng |
title |
Effect of snow grain shape and impurities on snow albedo and its parameterization: China, North America, and the Arctic |
title_short |
Effect of snow grain shape and impurities on snow albedo and its parameterization: China, North America, and the Arctic |
title_full |
Effect of snow grain shape and impurities on snow albedo and its parameterization: China, North America, and the Arctic |
title_fullStr |
Effect of snow grain shape and impurities on snow albedo and its parameterization: China, North America, and the Arctic |
title_full_unstemmed |
Effect of snow grain shape and impurities on snow albedo and its parameterization: China, North America, and the Arctic |
title_sort |
effect of snow grain shape and impurities on snow albedo and its parameterization: china, north america, and the arctic |
publishDate |
2017 |
url |
http://hdl.handle.net/1773/38572 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
albedo Arctic black carbon |
genre_facet |
albedo Arctic black carbon |
op_relation |
Dang_washington_0250E_13163.pdf http://hdl.handle.net/1773/38572 |
op_rights |
CC BY-NC-ND |
_version_ |
1766240347528101888 |