Articles | Volume 11, issue 6
https://doi.org/10.5194/tc-11-2727-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/tc-11-2727-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Comparison of different methods to retrieve optical-equivalent snow grain size in central Antarctica
Leipzig Institute for Meteorology, University of Leipzig, Leipzig,
Germany
Gerit Birnbaum
Alfred Wegener Institute, Helmholtz Centre for Polar and
Marine Research, Bremerhaven, Germany
André Ehrlich
Leipzig Institute for Meteorology, University of Leipzig, Leipzig,
Germany
Johannes Freitag
Alfred Wegener Institute, Helmholtz Centre for Polar and
Marine Research, Bremerhaven, Germany
Georg Heygster
Institute of Environmental
Physics, University of Bremen, Bremen, Germany
Larysa Istomina
Institute of Environmental
Physics, University of Bremen, Bremen, Germany
Sepp Kipfstuhl
Alfred Wegener Institute, Helmholtz Centre for Polar and
Marine Research, Bremerhaven, Germany
Anaïs Orsi
Laboratoire des
Sciences du Climat et de l'Environnement, Gif-sur-Yvette, France
Michael Schäfer
Leipzig Institute for Meteorology, University of Leipzig, Leipzig,
Germany
Manfred Wendisch
Leipzig Institute for Meteorology, University of Leipzig, Leipzig,
Germany
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21 citations as recorded by crossref.
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- 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
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- Influence of atmospheric adjacency effect on top-of-atmosphere radiances and its correction in the retrieval of Lambertian surface reflectivity based on three-dimensional radiative transfer B. Sun et al. 10.1016/j.rse.2021.112543
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- The retrieval of snow properties from SLSTR Sentinel-3 – Part 2: Results and validation L. Mei et al. 10.5194/tc-15-2781-2021
- Optimal estimation of snow and ice surface parameters from imaging spectroscopy measurements N. Bohn et al. 10.1016/j.rse.2021.112613
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- Glacier Ice Surface Properties in South‐West Greenland Ice Sheet: First Estimates From PRISMA Imaging Spectroscopy Data N. Bohn et al. 10.1029/2021JG006718
- Microstructure of Snow and Its Link to Trace Elements and Isotopic Composition at Kohnen Station, Dronning Maud Land, Antarctica D. Moser et al. 10.3389/feart.2020.00023
- Spectral albedo measurements over snow-covered slopes: theory and slope effect corrections G. Picard et al. 10.5194/tc-14-1497-2020
- Dynamics of the snow grain size in a windy coastal area of Antarctica from continuous in situ spectral-albedo measurements S. Arioli et al. 10.5194/tc-17-2323-2023
- Characterization of sea ice and its snow cover in the Arctic Pacific sector during the summer of 2016 Q. Ji et al. 10.1007/s13131-021-1716-3
- Snow specific surface area remote sensing retrieval using a microstructure based reflectance model C. Xiong & J. Shi 10.1016/j.rse.2017.09.017
- First Retrievals of Surface and Atmospheric Properties Using EnMAP Measurements over Antarctica A. Kokhanovsky et al. 10.3390/rs15123042
- The determination of snow parameters using SGLI/GCOM-C spaceborne top-of-atmosphere spectral reflectance measurements over Antarctica A. Kokhanovsky et al. 10.1016/j.jqsrt.2022.108226
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Latest update: 24 Dec 2024
Short summary
The optical size of snow grains (ropt) affects the reflectivity of snow surfaces and thus the local surface energy budget in particular in polar regions. The temporal evolution of ropt retrieved from ground-based, airborne, and spaceborne remote sensing could reproduce optical in situ measurements for a 2-month period in central Antarctica (2013/14). The presented validation study provided a unique testbed for retrievals of ropt under Antarctic conditions where in situ data are scarce.
The optical size of snow grains (ropt) affects the reflectivity of snow surfaces and thus the...
Special issue