Articles | Volume 19, issue 10
https://doi.org/10.5194/acp-19-7105-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-19-7105-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Impact of light-absorbing particles on snow albedo darkening and associated radiative forcing over high-mountain Asia: high-resolution WRF-Chem modeling and new satellite observations
Chandan Sarangi
Pacific Northwest National Laboratory, Richland, WA, USA
Yun Qian
CORRESPONDING AUTHOR
Pacific Northwest National Laboratory, Richland, WA, USA
Karl Rittger
Institute of Arctic and Alpine Research, Boulder, CO, USA
Kathryn J. Bormann
Jet Propulsion Laboratory, California Institute of Technology,
Pasadena, CA, USA
Ying Liu
Pacific Northwest National Laboratory, Richland, WA, USA
Hailong Wang
Pacific Northwest National Laboratory, Richland, WA, USA
Pacific Northwest National Laboratory, Richland, WA, USA
Guangxing Lin
Pacific Northwest National Laboratory, Richland, WA, USA
Thomas H. Painter
Jet Propulsion Laboratory, California Institute of Technology,
Pasadena, CA, USA
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Latest update: 23 Nov 2024
Short summary
Radiative forcing induced by deposition of light-absorbing particles (LAPs) on snow is an important surface forcing. Here, we have used high-resolution WRF-Chem (coupled with online snow–LAP–radiation model) simulations for 2013–2014 to estimate the spatial variation in LAP-induced snow albedo darkening effect in high-mountain Asia. Significant improvement in simulated LAP–snow properties with use of a higher spatial resolution for the same model configuration is illustrated over this region.
Radiative forcing induced by deposition of light-absorbing particles (LAPs) on snow is an...
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