Radiative processes are substantially altered by the presence of forest canopies, further affecting snow energetics during wintertime. In situ measurements of subcanopy radiation can help improve process‐scale understanding of these complex interactions, which are needed to further constrain and improve land surface models. In this study, a custom‐made cable car was used to measure incoming and outgoing, shortwave and longwave radiation below an evergreen forest stand. Hemispherical photographs taken concurrently from the cable car measured view fractions of shaded snow, sunlit snow, and bare ground. With this setup it was possible to quantify diurnal and seasonal radiation patterns together with their potential drivers at high spatiotempor...
Small-scale variations in radiative transfer through forest canopies are strongly linked to canopy s...
Sky conditions play an important role in the Earth’s climate system, altering the solar radiation r...
Boreal forests cover about a fifth of seasonally snow‐covered land over the Northern Hemisphere. Enh...
Radiative processes are substantially altered by the presence of forest canopies, further affecting ...
A comprehensive analysis of canopy temperatures was conducted around a small and large gap at a fore...
Forest canopies are complex 3-D structures at the interface between the atmosphere and the land surf...
The overlap of seasonal snow and forests contributes significantly to global snowmelt, largely drive...
Open woodland is a major sub-type of the circum global boreal forest zone. In Canada it dominates th...
Single-layer vegetation schemes in modern land surface models have been found to overestimate diurna...
Utilising extensive field observations and physically-based simulations of forest-snow processes, th...
Snow albedo regulates the surface energy budget of snow-covered regions which governs snowmelt proce...
Boreal forests cover about a fifth of seasonally snow-covered land over the Northern Hemisphere. Ski...
The complex dynamics of snow accumulation and melt processes under forest canopies entail major obse...
Predicting the rate of snowmelt and intercepted snow sublimation in boreal forests requires an under...
Solar radiation beneath a forest canopy can have large spatial variations, but this is frequently ne...
Small-scale variations in radiative transfer through forest canopies are strongly linked to canopy s...
Sky conditions play an important role in the Earth’s climate system, altering the solar radiation r...
Boreal forests cover about a fifth of seasonally snow‐covered land over the Northern Hemisphere. Enh...
Radiative processes are substantially altered by the presence of forest canopies, further affecting ...
A comprehensive analysis of canopy temperatures was conducted around a small and large gap at a fore...
Forest canopies are complex 3-D structures at the interface between the atmosphere and the land surf...
The overlap of seasonal snow and forests contributes significantly to global snowmelt, largely drive...
Open woodland is a major sub-type of the circum global boreal forest zone. In Canada it dominates th...
Single-layer vegetation schemes in modern land surface models have been found to overestimate diurna...
Utilising extensive field observations and physically-based simulations of forest-snow processes, th...
Snow albedo regulates the surface energy budget of snow-covered regions which governs snowmelt proce...
Boreal forests cover about a fifth of seasonally snow-covered land over the Northern Hemisphere. Ski...
The complex dynamics of snow accumulation and melt processes under forest canopies entail major obse...
Predicting the rate of snowmelt and intercepted snow sublimation in boreal forests requires an under...
Solar radiation beneath a forest canopy can have large spatial variations, but this is frequently ne...
Small-scale variations in radiative transfer through forest canopies are strongly linked to canopy s...
Sky conditions play an important role in the Earth’s climate system, altering the solar radiation r...
Boreal forests cover about a fifth of seasonally snow‐covered land over the Northern Hemisphere. Enh...