Impact of water vapor diffusion and latent heat on the effective thermal conductivity of snow
- 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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Impact of water vapor diffusion and latent heat on the effective thermal conductivity of snow ; volume:15 ; number:6 ; year:2021 ; pages:2739-2755 ; extent:17
The Cryosphere ; 15, Heft 6 (2021), 2739-2755 (gesamt 17)
- Creator
- DOI
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10.5194/tc-15-2739-2021
- URN
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urn:nbn:de:101:1-2021082608051214148311
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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14.08.2025, 10:55 AM CEST
Data provider
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Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Fourteau, Kévin
- Domine, Florent
- Hagenmuller, Pascal
Other Objects (12)
Impact of water vapor diffusion and latent heat on the effective thermal conductivity of snow
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Reversible conductivity recovery of highly sensitive flexible devices by water vapor
Impact of water vapor diffusion and latent heat on the effective thermal conductivity of snow
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Macroscopic water vapor diffusion is not enhanced in snow
Macroscopic water vapor diffusion is not enhanced in snow
Using the Sensible Heat Flux Eddy Covariance-Based Exchange Coefficient to Calculate Latent Heat Flux from Moisture Mean Gradients Over Snow
Heat flux in latent thermal energy storage systems: the influence of fins, thermal conductivity and driving temperature difference
Latent heat storage provides process steam.
Temporospatial variability of snow's thermal conductivity on Arctic sea ice
Snow dune growth increases polar heat fluxes
Heat requirement of greenhouses including latent heat flux = Wärmebedarf von Gewächshäusern unter Berücksichtigung des latenten Wärmetransportes
Latent Heat Storage for Heat Pump and Solar Heating Systems
Reversible conductivity recovery of highly sensitive flexible devices by water vapor
Impact of water vapor diffusion and latent heat on the effective thermal conductivity of snow
Snow & Heat Roe
Macroscopic water vapor diffusion is not enhanced in snow
Macroscopic water vapor diffusion is not enhanced in snow
Using the Sensible Heat Flux Eddy Covariance-Based Exchange Coefficient to Calculate Latent Heat Flux from Moisture Mean Gradients Over Snow
Heat flux in latent thermal energy storage systems: the influence of fins, thermal conductivity and driving temperature difference
Latent heat storage provides process steam.
Temporospatial variability of snow's thermal conductivity on Arctic sea ice
Snow dune growth increases polar heat fluxes
Heat requirement of greenhouses including latent heat flux = Wärmebedarf von Gewächshäusern unter Berücksichtigung des latenten Wärmetransportes
Latent Heat Storage for Heat Pump and Solar Heating Systems