Articles | Volume 16, issue 4
https://doi.org/10.5194/tc-16-1197-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-16-1197-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
SNICAR-ADv4: a physically based radiative transfer model to represent the spectral albedo of glacier ice
Department of Climate and Space Sciences and Engineering, University
of Michigan, Ann Arbor, MI, USA
Mark G. Flanner
Department of Climate and Space Sciences and Engineering, University
of Michigan, Ann Arbor, MI, USA
Cheng Dang
Joint Center for Satellite Data Assimilation, University Corporation
for Atmospheric Research, Boulder, CO, USA
Charles S. Zender
Department of Earth System Science, University of California, Irvine,
CA, USA
Joseph M. Cook
Department of Environmental Science, Aarhus University,
Frederiksborgvej 339C, 4000, Roskilde, Denmark
Alex S. Gardner
Jet Propulsion Laboratory, California Institute of Technology,
Pasadena, CA 91109, USA
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Cited
15 citations as recorded by crossref.
- Dark brown carbon from wildfires: a potent snow radiative forcing agent? G. Chelluboyina et al. 10.1038/s41612-024-00738-7
- Modelling light-absorbing particle–snow–radiation interactions and impacts on snow albedo: fundamentals, recent advances and future directions C. He & J. Ming 10.1071/EN22013
- Snow Albedo and its Parameterization for the Purposes of Modeling Natural Systems and Climate D. Turkov et al. 10.1134/S0001433824701226
- Light absorption and albedo reduction by pigmented microalgae on snow and ice L. Chevrollier et al. 10.1017/jog.2022.64
- Assessing bare-ice albedo simulated by MAR over the Greenland ice sheet (2000–2021) and implications for meltwater production estimates R. Antwerpen et al. 10.5194/tc-16-4185-2022
- Black carbon concentrations and modeled smoke deposition fluxes to the bare-ice dark zone of the Greenland Ice Sheet A. Khan et al. 10.5194/tc-17-2909-2023
- Snow albedo and its parameterization for natural systems and climate modeling D. Turkov et al. 10.31857/S2076673424030079
- Dark ice in a warming world: advances and challenges in the study of Greenland Ice Sheet's biological darkening L. Halbach et al. 10.1017/aog.2023.17
- Impact of varying solar angles on Arctic iceberg area retrieval from Sentinel-2 near-infrared data H. Fisser et al. 10.1017/aog.2024.39
- Contribution of biomass burning to black carbon deposition on Andean glaciers: consequences for radiative forcing E. Bonilla et al. 10.1088/1748-9326/acb371
- Potential for photosynthesis on Mars within snow and ice A. Khuller et al. 10.1038/s43247-024-01730-y
- Do we still need reflectance? From radiance to snow properties in mountainous terrain: a case study with the EMIT imaging spectrometer N. Bohn et al. 10.5194/tc-19-1279-2025
- Surface and Atmospheric Heating Responses to Spectrally Resolved Albedo of Frozen and Liquid Water Surfaces J. Tolento et al. 10.1029/2023JD039824
- SNICAR-ADv4: a physically based radiative transfer model to represent the spectral albedo of glacier ice C. Whicker et al. 10.5194/tc-16-1197-2022
- SNICAR-ADv3: a community tool for modeling spectral snow albedo M. Flanner et al. 10.5194/gmd-14-7673-2021
12 citations as recorded by crossref.
- Dark brown carbon from wildfires: a potent snow radiative forcing agent? G. Chelluboyina et al. 10.1038/s41612-024-00738-7
- Modelling light-absorbing particle–snow–radiation interactions and impacts on snow albedo: fundamentals, recent advances and future directions C. He & J. Ming 10.1071/EN22013
- Snow Albedo and its Parameterization for the Purposes of Modeling Natural Systems and Climate D. Turkov et al. 10.1134/S0001433824701226
- Light absorption and albedo reduction by pigmented microalgae on snow and ice L. Chevrollier et al. 10.1017/jog.2022.64
- Assessing bare-ice albedo simulated by MAR over the Greenland ice sheet (2000–2021) and implications for meltwater production estimates R. Antwerpen et al. 10.5194/tc-16-4185-2022
- Black carbon concentrations and modeled smoke deposition fluxes to the bare-ice dark zone of the Greenland Ice Sheet A. Khan et al. 10.5194/tc-17-2909-2023
- Snow albedo and its parameterization for natural systems and climate modeling D. Turkov et al. 10.31857/S2076673424030079
- Dark ice in a warming world: advances and challenges in the study of Greenland Ice Sheet's biological darkening L. Halbach et al. 10.1017/aog.2023.17
- Impact of varying solar angles on Arctic iceberg area retrieval from Sentinel-2 near-infrared data H. Fisser et al. 10.1017/aog.2024.39
- Contribution of biomass burning to black carbon deposition on Andean glaciers: consequences for radiative forcing E. Bonilla et al. 10.1088/1748-9326/acb371
- Potential for photosynthesis on Mars within snow and ice A. Khuller et al. 10.1038/s43247-024-01730-y
- Do we still need reflectance? From radiance to snow properties in mountainous terrain: a case study with the EMIT imaging spectrometer N. Bohn et al. 10.5194/tc-19-1279-2025
3 citations as recorded by crossref.
- Surface and Atmospheric Heating Responses to Spectrally Resolved Albedo of Frozen and Liquid Water Surfaces J. Tolento et al. 10.1029/2023JD039824
- SNICAR-ADv4: a physically based radiative transfer model to represent the spectral albedo of glacier ice C. Whicker et al. 10.5194/tc-16-1197-2022
- SNICAR-ADv3: a community tool for modeling spectral snow albedo M. Flanner et al. 10.5194/gmd-14-7673-2021
Latest update: 29 Mar 2025
Short summary
Snow and ice surfaces are important to the global climate. Current climate models use measurements to determine the reflectivity of ice. This model uses physical properties to determine the reflectivity of snow, ice, and darkly pigmented impurities that reside within the snow and ice. Therefore, the modeled reflectivity is more accurate for snow/ice columns under varying climate conditions. This model paves the way for improvements in the portrayal of snow and ice within global climate models.
Snow and ice surfaces are important to the global climate. Current climate models use...