Articles | Volume 11, issue 6
https://doi.org/10.5194/tc-11-2919-2017
© Author(s) 2017. 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-11-2919-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Effects of snow grain shape on climate simulations: sensitivity tests with the Norwegian Earth System Model
Finnish Meteorological Institute, P.O. Box 503, 00101 Helsinki, Finland
Risto Makkonen
Dept. of Physics, University of Helsinki, P.O. Box 64,
00014 University of Helsinki, Finland
Alf Kirkevåg
Norwegian Meteorological Institute, P.O. Box 43, Blindern, 0313 Oslo, Norway
Jens B. Debernard
Norwegian Meteorological Institute, P.O. Box 43, Blindern, 0313 Oslo, Norway
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19 citations as recorded by crossref.
- Snow-darkening versus direct radiative effects of mineral dust aerosol on the Indian summer monsoon onset: role of temperature change over dust sources Z. Shi et al. 10.5194/acp-19-1605-2019
- Evaluation of E3SM land model snow simulations over the western United States D. Hao et al. 10.5194/tc-17-673-2023
- Remote Sensing-Based Simulation of Snow Grain Size and Spatial–Temporal Variation Characteristics of Northeast China from 2001 to 2019 F. Zhang et al. 10.3390/rs15204970
- Black carbon-induced snow albedo reduction over the Tibetan Plateau: uncertainties from snow grain shape and aerosol–snow mixing state based on an updated SNICAR model C. He et al. 10.5194/acp-18-11507-2018
- Unraveling the optical shape of snow A. Robledano et al. 10.1038/s41467-023-39671-3
- The regional climate model REMO (v2015) coupled with the 1-D freshwater lake model FLake (v1): Fenno-Scandinavian climate and lakes J. Pietikäinen et al. 10.5194/gmd-11-1321-2018
- Evaluation of surface albedo over the Tibetan Plateau simulated by CMIP5 models using in‐situ measurements and MODIS Y. An et al. 10.1002/joc.7281
- Polarization as a Discriminator of Light-Absorbing Impurities in or Above Snow M. Ottaviani 10.3389/frsen.2022.863239
- Impact of aerosols on reservoir inflow: A case study for Big Creek Hydroelectric System in California F. Kabir et al. 10.1002/hyp.13265
- Improving snow albedo modeling in the E3SM land model (version 2.0) and assessing its impacts on snow and surface fluxes over the Tibetan Plateau D. Hao et al. 10.5194/gmd-16-75-2023
- Transmission of ultraviolet, visible and near-infrared solar radiation to plants within a seasonal snow pack T. Robson & P. Aphalo 10.1039/c9pp00197b
- The Spatio-Temporal Variability in the Radiative Forcing of Light-Absorbing Particles in Snow of 2003–2018 over the Northern Hemisphere from MODIS J. Cui et al. 10.3390/rs15030636
- How Asian aerosols impact regional surface temperatures across the globe J. Merikanto et al. 10.5194/acp-21-5865-2021
- The retrieval of snow properties from SLSTR Sentinel-3 – Part 1: Method description and sensitivity study L. Mei et al. 10.5194/tc-15-2757-2021
- Global sensitivity analysis of simulated remote sensing polarimetric observations over snow M. Ottaviani et al. 10.5194/amt-17-4737-2024
- Resolving Size Distribution of Black Carbon Internally Mixed With Snow: Impact on Snow Optical Properties and Albedo C. He et al. 10.1002/2018GL077062
- Enhanced Snow Absorption and Albedo Reduction by Dust‐Snow Internal Mixing: Modeling and Parameterization C. He et al. 10.1029/2019MS001737
- The retrieval of snow properties from SLSTR Sentinel-3 – Part 2: Results and validation L. Mei et al. 10.5194/tc-15-2781-2021
- 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
1 citations as recorded by crossref.
Discussed (final revised paper)
Latest update: 20 Nov 2024
Short summary
While snow grains are non-spherical, spheres are often assumed in radiation calculations. Here, we replace spherical snow grains with non-spherical snow grains in a climate model. This leads to a somewhat higher snow albedo (by 0.02–0.03), increased snow and sea ice cover, and a distinctly colder climate (by over 1 K in the global mean). It also impacts the radiative effects of aerosols in snow. Overall, this work highlights the important role of snow albedo parameterization for climate models.
While snow grains are non-spherical, spheres are often assumed in radiation calculations. Here,...