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How Are Turbulent Sensible Heat Fluxes and Snow Melt Rates Affected by a Changing Snow Cover Fraction?

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How Are Turbulent Sensible Heat Fluxes and Snow Melt Rates Affected by a Changing Snow Cover Fraction?

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Evaluating snow models with varying process representations for hydrological applications

Buoyant turbulence kinetic energy (TKE) production in katabatic flow despite stable thermal stratification

A two-layer canopy model with thermal inertia for an improved snowpack energy balance below needleleaf forest (model SNOWPACK, version 3.2.1, revision 741)

3D turbulence measurements in inhomogeneous boundary layers with three wind LiDARs

3D turbulence measurements in inhomogeneous boundary layers with three wind LiDARs

Modelling Small-Scale Drifting Snow with a Lagrangian Stochastic Model Based on Large-Eddy Simulations

Boundary layer processes over a patchy mountain snow cover and associated changes in the energy balance

Relative importance of advective heat transport and boundary layer decoupling in the melt dynamics of a patchy snow cover

Atmospheric boundary layers in complex terrain and over ice, snow and vegetated surfaces

Snow cover runoff and stream discharge modelling during snow melt in Alpine terrain

Boundary layer processes over a patchy mountain snow cover and associated changes in the energy balance

Evaluating snow models with varying process representations for hydrological applications

Atmospheric boundary layers in complex terrain and over ice, snow and vegetated surfaces

3D turbulence measurements in inhomogeneous boundary layers with three wind LiDARs

3D turbulence measurements in inhomogeneous boundary layers with three wind LiDARs

Modelling Small-Scale Drifting Snow with a Lagrangian Stochastic Model Based on Large-Eddy Simulations

Relative importance of advective heat transport and boundary layer decoupling in the melt dynamics of a patchy snow cover

Snow cover runoff and stream discharge modelling during snow melt in Alpine terrain

Buoyant turbulence kinetic energy (TKE) production in katabatic flow despite stable thermal stratification

A two-layer canopy model with thermal inertia for an improved snowpack energy balance below needleleaf forest (model SNOWPACK, version 3.2.1, revision 741)