SNICAR-ADv4: A physically based radiative transfer model to represent the spectral albedo of glacier ice
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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SNICAR-ADv4: A physically based radiative transfer model to represent the spectral albedo of glacier ice ; day:23 ; month:09 ; year:2021 ; pages:1-36 ; extent:36
The Cryosphere discussions ; (23.09.2021), 1-36 (gesamt 36)
- Creator
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Whicker, Chloe A.
Flanner, Mark G.
Dang, Cheng
Zender, Charles S.
Cook, Joseph M.
Gardner, Alex S.
- DOI
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10.5194/tc-2021-272
- URN
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urn:nbn:de:101:1-2021093005260690762184
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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21.08.2025, 7:36 AM CEST
Data provider
This object is provided by:
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Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Whicker, Chloe A.
- Flanner, Mark G.
- Dang, Cheng
- Zender, Charles S.
- Cook, Joseph M.
- Gardner, Alex S.
Other Objects (12)
SNICAR-ADv4: a physically based radiative transfer model to represent the spectral albedo of glacier ice
Linking glacier annual mass balance and glacier albedo retrieved from MODIS data
Radiative albedo from a linearly fibered half-space
Reconstructing the mass balance of Brewster Glacier, New Zealand, using MODIS-derived glacier-wide albedo
High albedo daytime radiative cooling for enhanced bifacial PV performance
The implications of maintaining Earth's hemispheric albedo symmetry for shortwave radiative feedbacks
Albedo
INTERPRETING CHANGES IN ALBEDO AND MASS BALANCE AT WHITE GLACIER, CANADIAN ARCTIC ARCHIPELAGO
Changes in albedo and its radiative forcing of grasslands in East Asia drylands
Temporal changes in snow albedo, including the possible effects of red algal growth, in northwest Greenland, simulated with a physically based snow albedo model
REPRESENT
-REPRESENT-
SNICAR-ADv4: a physically based radiative transfer model to represent the spectral albedo of glacier ice
Linking glacier annual mass balance and glacier albedo retrieved from MODIS data
Radiative albedo from a linearly fibered half-space
Reconstructing the mass balance of Brewster Glacier, New Zealand, using MODIS-derived glacier-wide albedo
High albedo daytime radiative cooling for enhanced bifacial PV performance
The implications of maintaining Earth's hemispheric albedo symmetry for shortwave radiative feedbacks
Albedo
INTERPRETING CHANGES IN ALBEDO AND MASS BALANCE AT WHITE GLACIER, CANADIAN ARCTIC ARCHIPELAGO
Changes in albedo and its radiative forcing of grasslands in East Asia drylands
Temporal changes in snow albedo, including the possible effects of red algal growth, in northwest Greenland, simulated with a physically based snow albedo model
REPRESENT
-REPRESENT-
SNICAR-ADv4: a physically based radiative transfer model to represent the spectral albedo of glacier ice
Linking glacier annual mass balance and glacier albedo retrieved from MODIS data
Radiative albedo from a linearly fibered half-space
Reconstructing the mass balance of Brewster Glacier, New Zealand, using MODIS-derived glacier-wide albedo
High albedo daytime radiative cooling for enhanced bifacial PV performance
The implications of maintaining Earth's hemispheric albedo symmetry for shortwave radiative feedbacks
Albedo
INTERPRETING CHANGES IN ALBEDO AND MASS BALANCE AT WHITE GLACIER, CANADIAN ARCTIC ARCHIPELAGO
Changes in albedo and its radiative forcing of grasslands in East Asia drylands
Temporal changes in snow albedo, including the possible effects of red algal growth, in northwest Greenland, simulated with a physically based snow albedo model
REPRESENT